subject:(snow melt)

Colorado State University

1. Duncan, Caroline R. Patterns of dust-enhanced absorbed energy and shifts in melt timing for snow of southwestern Colorado.

Degree: MS(M.S.), Ecosystem Science and Sustainability, 2020, Colorado State University

URL: http://hdl.handle.net/10217/211991

► Deposited dust layers reduce the surface albedo of snow and accelerate melt by this change to the snowpack energy balance. Senator Beck Study Basin in… (more)

Subjects/Keywords: melt; dust; snow

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APA (6^th Edition):

Duncan, C. R. (2020). Patterns of dust-enhanced absorbed energy and shifts in melt timing for snow of southwestern Colorado. (Masters Thesis). Colorado State University. Retrieved from http://hdl.handle.net/10217/211991

Chicago Manual of Style (16^th Edition):

Duncan, Caroline R. “Patterns of dust-enhanced absorbed energy and shifts in melt timing for snow of southwestern Colorado.” 2020. Masters Thesis, Colorado State University. Accessed April 12, 2021. http://hdl.handle.net/10217/211991.

MLA Handbook (7^th Edition):

Duncan, Caroline R. “Patterns of dust-enhanced absorbed energy and shifts in melt timing for snow of southwestern Colorado.” 2020. Web. 12 Apr 2021.

Vancouver:

Duncan CR. Patterns of dust-enhanced absorbed energy and shifts in melt timing for snow of southwestern Colorado. [Internet] [Masters thesis]. Colorado State University; 2020. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/10217/211991.

Council of Science Editors:

Duncan CR. Patterns of dust-enhanced absorbed energy and shifts in melt timing for snow of southwestern Colorado. [Masters Thesis]. Colorado State University; 2020. Available from: http://hdl.handle.net/10217/211991

Colorado State University

2. Bonnell, Randall Ray. Spatiotemporal variations in liquid water content in a seasonal snowpack: implications for radar remote sensing.

Degree: MS(M.S.), Geosciences, 2020, Colorado State University

URL: http://hdl.handle.net/10217/212050

► Mountain snowpacks act as seasonal reservoirs, providing a critical water resource to ~1.2 billion people globally. Regions with persistent snowpacks (e.g., mountain and polar environments)… (more)

▼ Mountain snowpacks act as seasonal reservoirs, providing a critical water resource to ~1.2 billion people globally. Regions with persistent snowpacks (e.g., mountain and polar environments) are responding quickly to climate change and are warming at faster rates than low-elevation temperate and equatorial regions. Since 1915, snow water equivalent (SWE) in the western U.S. snowpack has declined by 21% and snow covered area is contracting in the Rocky Mountains. Despite the clear importance of this resource and the identification of changes affecting it, no current remote sensing approach can accurately measure SWE at high spactiotemporal resolution. L-band (1-2 GHz) Interferometric Synthetic Aperture Radar (InSAR) is a promising approach for detecting changes in SWE at high spatiotemporal resolution in complex topography, but there are uncertainties regarding its performance, particularly when liquid water content (LWC) is present in the snowpack. LWC exhibits high spatial variability, causing spatially varying radar velocity that introduces significant uncertainty in SWE-retrievals. The objectives of this thesis include: (1) examine the importance of slope, aspect, canopy cover, and air temperature in the development of LWC in a continental seasonal snowpack using 1 GHz ground-penetrating radar (GPR), a proxy for L-band InSAR, and (2) quantify the uncertainty in L-band radar SWE-retrievals in wet-snow. This research was performed at Cameron Pass, a high elevation pass (3120 m) located in north-central Colorado, over the course of multiple survey dates during the melt season of 2019. Transects were chosen which represent a range in slope, aspect and canopy cover. Slope and aspect were simplified using the northness index (NI). Canopy cover was quantified using the leaf area index (LAI). Positive degree days (PDD) was used to represent available melt-energy from air temperature. The spatiotemporal development of LWC was studied along the transects using GPR, probed depths, and snowpit measured density. A subset of this project substituted Terrestrial LiDAR Scans (TLS) for probed depths. Surveys (17 in total, up to 3 surveys per date) were performed on seven dates which began on5 April 2019, where LWC values were ~0 vol. %, and ended on 19 June 2019 where LWC values exceeded 10 vol. %. Point measurements of LWC were observed to change (ΔLWC) by +9 vol. % or -8 vol. % over the course of a single day, but median ΔLWC were ~0 vol. % or slightly negative. LAI was negatively correlated with LWC for 13 out of the 17 surveys. NI was negatively correlated with LWC for 10 out of the 17 surveys. Multi-variable linear regressions to estimate ΔLWC identified several statistically significant variables (p-value < 0.10): LAI, NI, ΔPDD, and NI x ΔPDD. Snow-on Terrestrial LiDAR Scans (TLS) were conducted twice during the melt season, and a snow-off scan was conducted in late summer. Snow-on scans were differenced from the snow-off scan to produce distributed snow depth maps. TLS-derived snow depths compared poorly with probe-derived… Advisors/Committee Members: McGrath, Daniel (advisor), Fassnacht, Steven (committee member), Rasmussen, Kristen (committee member).

Subjects/Keywords: L-band radar; snow; snow water equivalent; liquid water content; ground-penetrating radar; snow melt

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APA (6^th Edition):

Bonnell, R. R. (2020). Spatiotemporal variations in liquid water content in a seasonal snowpack: implications for radar remote sensing. (Masters Thesis). Colorado State University. Retrieved from http://hdl.handle.net/10217/212050

Chicago Manual of Style (16^th Edition):

Bonnell, Randall Ray. “Spatiotemporal variations in liquid water content in a seasonal snowpack: implications for radar remote sensing.” 2020. Masters Thesis, Colorado State University. Accessed April 12, 2021. http://hdl.handle.net/10217/212050.

MLA Handbook (7^th Edition):

Bonnell, Randall Ray. “Spatiotemporal variations in liquid water content in a seasonal snowpack: implications for radar remote sensing.” 2020. Web. 12 Apr 2021.

Vancouver:

Bonnell RR. Spatiotemporal variations in liquid water content in a seasonal snowpack: implications for radar remote sensing. [Internet] [Masters thesis]. Colorado State University; 2020. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/10217/212050.

Council of Science Editors:

Bonnell RR. Spatiotemporal variations in liquid water content in a seasonal snowpack: implications for radar remote sensing. [Masters Thesis]. Colorado State University; 2020. Available from: http://hdl.handle.net/10217/212050

3. Gold, Brittany. Observations of diurnal melt-freeze events using time domain reflectometry (TDR) in sesonal snowpack.

Degree: MS, Geography, 2014, University of Utah

URL: http://content.lib.utah.edu/cdm/singleitem/collection/etd3/id/3146/rec/1732

► Understanding seasonal snowpack characteristics is essential for avalanche forecasting and water resource management. As technology advances, instrumentscontinue to be developed to study seasonal snowpack characteristics.… (more)

Subjects/Keywords: Melt-freeze; Snow; TDR

…density, and snow liquid water content interact during diurnal melt-freeze cycles in a snowpack… …study to analyze dry snow dielectric constant and offset calculations; evaluate diurnal melt… …water is present in the snowpack. Time periods in which snow density data was collected are… …15 2.2: This table compares the dielectric constant of snow's constituents—air, ice… …This table includes dielectric constant values measured in dry snow as well as the Mätzler…

11 more images…

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APA (6^th Edition):

Gold, B. (2014). Observations of diurnal melt-freeze events using time domain reflectometry (TDR) in sesonal snowpack. (Masters Thesis). University of Utah. Retrieved from http://content.lib.utah.edu/cdm/singleitem/collection/etd3/id/3146/rec/1732

Chicago Manual of Style (16^th Edition):

Gold, Brittany. “Observations of diurnal melt-freeze events using time domain reflectometry (TDR) in sesonal snowpack.” 2014. Masters Thesis, University of Utah. Accessed April 12, 2021. http://content.lib.utah.edu/cdm/singleitem/collection/etd3/id/3146/rec/1732.

MLA Handbook (7^th Edition):

Gold, Brittany. “Observations of diurnal melt-freeze events using time domain reflectometry (TDR) in sesonal snowpack.” 2014. Web. 12 Apr 2021.

Vancouver:

Gold B. Observations of diurnal melt-freeze events using time domain reflectometry (TDR) in sesonal snowpack. [Internet] [Masters thesis]. University of Utah; 2014. [cited 2021 Apr 12]. Available from: http://content.lib.utah.edu/cdm/singleitem/collection/etd3/id/3146/rec/1732.

Council of Science Editors:

Gold B. Observations of diurnal melt-freeze events using time domain reflectometry (TDR) in sesonal snowpack. [Masters Thesis]. University of Utah; 2014. Available from: http://content.lib.utah.edu/cdm/singleitem/collection/etd3/id/3146/rec/1732

4. Vuyovich, Carrie Micheline. PASSIVE MICROWAVE SATELLITE SNOW OBSERVATIONS FOR HYDROLOGIC APPLICATIONS.

Degree: PhD, 2016, University of New Hampshire

URL: https://scholars.unh.edu/dissertation/1384

► Melting snow provides an essential source of water in many regions of the world and can also contribute to devastating, wide-scale flooding. The objective of… (more)

▼ Melting snow provides an essential source of water in many regions of the world and can also contribute to devastating, wide-scale flooding. The objective of this research was to investigate the potential for passive microwave remotely sensed data to characterize snow water equivalent (SWE) and snowmelt across diverse regions and snow regimes to improve snowmelt runoff estimation. The first step was to evaluate the current, empirically-based passive microwave SWE products compared to NOAA’s operational SWE estimates from SNODAS across 2100 watersheds over eight years. The best agreement was found within basins in which maximum annual SWE is less than 200 mm, and forest fraction is less than 20%. Next, a sensitivity analysis was conducted to evaluate the microwave signal response to spatially distributed wet snow using a loosely-coupled snow-emission model. The results over an area approximately the size of a microwave pixel found a near-linear relationship between the microwave signal response and the percent area with wet snow present. These results were confirmed by evaluating actual wet snow events over a nine year period, and suggest that the microwave response provides the potential basis for disaggregating melting snow within a microwave pixel. Finally, a similar sensitivity analysis conducted in six watersheds with diverse landscapes and snow conditions confirmed the relationship holds at a basin scale. The magnitude of the microwave response to wet snow was compared to the magnitude of subsequent discharge events to determine if an empirical relation exists. While positive increases in brightness temperature (TB) correspond to positive increases in discharge, the magnitude of those changes is poorly correlated in most basins. The exception is in basins where snowmelt runoff typically occurs in one event each spring. In similar basins, the microwave response may provide information on the magnitude of spring runoff. Methods to use these findings to improve current snow and snow melt estimation as well as future research direction are discussed. Advisors/Committee Members: Jennifer M Jacobs, Diane Foster, Thomas Lippman.

Subjects/Keywords: flooding; melt; passive microwave; remote sensing; Snow; water; Remote sensing; Civil engineering

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APA (6^th Edition):

Vuyovich, C. M. (2016). PASSIVE MICROWAVE SATELLITE SNOW OBSERVATIONS FOR HYDROLOGIC APPLICATIONS. (Doctoral Dissertation). University of New Hampshire. Retrieved from https://scholars.unh.edu/dissertation/1384

Chicago Manual of Style (16^th Edition):

Vuyovich, Carrie Micheline. “PASSIVE MICROWAVE SATELLITE SNOW OBSERVATIONS FOR HYDROLOGIC APPLICATIONS.” 2016. Doctoral Dissertation, University of New Hampshire. Accessed April 12, 2021. https://scholars.unh.edu/dissertation/1384.

MLA Handbook (7^th Edition):

Vuyovich, Carrie Micheline. “PASSIVE MICROWAVE SATELLITE SNOW OBSERVATIONS FOR HYDROLOGIC APPLICATIONS.” 2016. Web. 12 Apr 2021.

Vancouver:

Vuyovich CM. PASSIVE MICROWAVE SATELLITE SNOW OBSERVATIONS FOR HYDROLOGIC APPLICATIONS. [Internet] [Doctoral dissertation]. University of New Hampshire; 2016. [cited 2021 Apr 12]. Available from: https://scholars.unh.edu/dissertation/1384.

Council of Science Editors:

Vuyovich CM. PASSIVE MICROWAVE SATELLITE SNOW OBSERVATIONS FOR HYDROLOGIC APPLICATIONS. [Doctoral Dissertation]. University of New Hampshire; 2016. Available from: https://scholars.unh.edu/dissertation/1384

Wilfrid Laurier University

5. Walker, Branden J. High resolution spatial variability in spring snowmelt for an Arctic shrub-tundra watershed.

Degree: 2019, Wilfrid Laurier University

URL: https://scholars.wlu.ca/etd/2116

► Arctic tundra environments are characterized by spatially heterogeneous end-of-winter snow cover because of high winds that erode, transport and deposit snow over the winter. This… (more)

▼ Arctic tundra environments are characterized by spatially heterogeneous end-of-winter snow cover because of high winds that erode, transport and deposit snow over the winter. This spatially variable end-of-winter snow cover subsequently influences the spatial and temporal variability of snowmelt and results in a patchy snowcover over the melt period. Documenting changes in both snow cover area (SCA) and snow water equivalent (SWE) during the spring melt is essential for understanding hydrological systems, but the lack of high-resolution SCA and SWE datasets that accurately capture micro-scale changes are not commonly available, and do not exist for the Canadian Arctic. This study applies high-resolution remote sensing measurements of SCA and SWE using a fixed-wing Unmanned Aerial System (UAS) to document snowcover changes over the snowmelt period for an Arctic tundra headwater catchment. Repeat measurements of SWE and SCA were obtained for four dominant land cover types (tundra, short shrub, tall shrub, and topographic drift) to provide observations of spatially distributed snowmelt patterns and basin-wide declines in SWE. High-resolution analysis of snowcover conditions over the melt reveal a strong relationship between land cover type, snow distribution, and snow ablation rates whereby shallow snowpacks found in tundra and short shrub regions feature rapid declines in SWE and SCA and became snow-free approximately 10 days earlier than deeper snowpacks. In contrast, tall shrub patches and topographic drift regions were characterized by large initial SWE values and featured a slow decline in SCA. Analysis of basin-wide declines in SCA and SWE reveal three distinct melt phases characterized by 1) low melt rates across a large area resulting in a minor change in SCA, but a very large decline in SWE with, 2) high melt rates resulting in drastic declines in both SCA and SWE, and 3) low melt rates over a small portion of the basin, resulting in little change to either SCA or SWE. The ability to capture high-resolution spatio-temporal changes to tundra snow cover furthers our understanding of the relative importance of various land cover types on the snowmelt timing and amount of runoff available to the hydrological system during the spring freshet.

Subjects/Keywords: Arctic tundra; snow; melt; spatial variability; Unmanned Aerial Systems (UAS); hydrology; remote sensing; Hydrology

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APA (6^th Edition):

Walker, B. J. (2019). High resolution spatial variability in spring snowmelt for an Arctic shrub-tundra watershed. (Thesis). Wilfrid Laurier University. Retrieved from https://scholars.wlu.ca/etd/2116

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Walker, Branden J. “High resolution spatial variability in spring snowmelt for an Arctic shrub-tundra watershed.” 2019. Thesis, Wilfrid Laurier University. Accessed April 12, 2021. https://scholars.wlu.ca/etd/2116.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Walker, Branden J. “High resolution spatial variability in spring snowmelt for an Arctic shrub-tundra watershed.” 2019. Web. 12 Apr 2021.

Vancouver:

Walker BJ. High resolution spatial variability in spring snowmelt for an Arctic shrub-tundra watershed. [Internet] [Thesis]. Wilfrid Laurier University; 2019. [cited 2021 Apr 12]. Available from: https://scholars.wlu.ca/etd/2116.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Walker BJ. High resolution spatial variability in spring snowmelt for an Arctic shrub-tundra watershed. [Thesis]. Wilfrid Laurier University; 2019. Available from: https://scholars.wlu.ca/etd/2116

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

University of Washington

6. Webster, Melinda Anne. A Geophysical Investigation of the Arctic Sea Ice Surface.

Degree: PhD, 2016, University of Washington

URL: http://hdl.handle.net/1773/36799

► The oldest records of the Arctic sea ice pack illustrate a frozen, yet dynamic icescape composed of hummocks and weathered ridges draped in thick snow.… (more)

Subjects/Keywords: Arctic; melt ponds; remote sensing; sea ice; snow; Geophysics; Physical oceanography; Remote sensing; oceanography

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APA (6^th Edition):

Webster, M. A. (2016). A Geophysical Investigation of the Arctic Sea Ice Surface. (Doctoral Dissertation). University of Washington. Retrieved from http://hdl.handle.net/1773/36799

Chicago Manual of Style (16^th Edition):

Webster, Melinda Anne. “A Geophysical Investigation of the Arctic Sea Ice Surface.” 2016. Doctoral Dissertation, University of Washington. Accessed April 12, 2021. http://hdl.handle.net/1773/36799.

MLA Handbook (7^th Edition):

Webster, Melinda Anne. “A Geophysical Investigation of the Arctic Sea Ice Surface.” 2016. Web. 12 Apr 2021.

Vancouver:

Webster MA. A Geophysical Investigation of the Arctic Sea Ice Surface. [Internet] [Doctoral dissertation]. University of Washington; 2016. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/1773/36799.

Council of Science Editors:

Webster MA. A Geophysical Investigation of the Arctic Sea Ice Surface. [Doctoral Dissertation]. University of Washington; 2016. Available from: http://hdl.handle.net/1773/36799

Utah State University

7. Sen Gupta, Avirup. Improving the Physical Processes and Model Integration Functionality of an Energy Balance Model for Snow and Glacier Melt.

Degree: PhD, Civil and Environmental Engineering, 2014, Utah State University

URL: https://digitalcommons.usu.edu/etd/3875

► The Hindu-Kush Himalayan region possesses a large resource of snow and ice, which acts as a freshwater reservoir for irrigation, domestic water consumption or… (more)

Subjects/Keywords: Physical Processes; Model Integration Functionality; Energy Balance Model; Snow; Glacier Melt; Civil and Environmental Engineering

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APA (6^th Edition):

Sen Gupta, A. (2014). Improving the Physical Processes and Model Integration Functionality of an Energy Balance Model for Snow and Glacier Melt. (Doctoral Dissertation). Utah State University. Retrieved from https://digitalcommons.usu.edu/etd/3875

Chicago Manual of Style (16^th Edition):

Sen Gupta, Avirup. “Improving the Physical Processes and Model Integration Functionality of an Energy Balance Model for Snow and Glacier Melt.” 2014. Doctoral Dissertation, Utah State University. Accessed April 12, 2021. https://digitalcommons.usu.edu/etd/3875.

MLA Handbook (7^th Edition):

Sen Gupta, Avirup. “Improving the Physical Processes and Model Integration Functionality of an Energy Balance Model for Snow and Glacier Melt.” 2014. Web. 12 Apr 2021.

Vancouver:

Sen Gupta A. Improving the Physical Processes and Model Integration Functionality of an Energy Balance Model for Snow and Glacier Melt. [Internet] [Doctoral dissertation]. Utah State University; 2014. [cited 2021 Apr 12]. Available from: https://digitalcommons.usu.edu/etd/3875.

Council of Science Editors:

Sen Gupta A. Improving the Physical Processes and Model Integration Functionality of an Energy Balance Model for Snow and Glacier Melt. [Doctoral Dissertation]. Utah State University; 2014. Available from: https://digitalcommons.usu.edu/etd/3875

University of Edinburgh

8. Turton, Rachael Heather. The impact of the radiation balance on snowmelt in a sparse deciduous birch forest.

Degree: PhD, 2017, University of Edinburgh

URL: http://hdl.handle.net/1842/29567

► The representation of high-latitude surface processes and quantifying surface-climate feedbacks are some of the most serious shortcomings of present day Arctic land surface modelling. The… (more)

▼ The representation of high-latitude surface processes and quantifying surface-climate feedbacks are some of the most serious shortcomings of present day Arctic land surface modelling. The energy balance of seasonally snow-covered sparse deciduous forests at high latitudes is poorly understood and inaccurately represented within hydrological and climate models. Snow cover plays an important role in wintertime fluxes of energy, water and carbon, controlling the length of the active growing season and hence the overall carbon balance of Arctic ecosystems. Snow cover is non-uniform and spatially variable, as wind redistributes snow from areas of exposed open tundra to sheltered areas within the forest, where a deeper snowpack develops. Low solar zenith angles, coupled with sparse deciduous leafless trees, cast shadows across the snow surface. The spatial distribution of canopy gaps determines the timing of direct radiation which penetrates down through the canopy to the snow surface. The forest canopy also excludes incoming longwave radiation and yet also emits longwave radiation to the snow surface. Consequently the forest canopy plays a key role in the radiation balance of sparse forests. To improve our knowledge of these complex processes, meteorological and field observations were taken in an area of highly heterogeneous birch Betula pubescens ssp. czerepanovii forest in Abisko, Sweden during the spring of 2008 and 2009. Detailed measurements of short and longwave radiation above and below the canopy, hemispherical photographs, tree temperatures and snow surveys were conducted to quantify the radiation balance of the sparse deciduous forest. An array of below canopy pyranometers found the mean canopy transmissivity to be 74 % in 2008 and 76 % in 2009. Hemispherical photographs taken at the pyranometer locations analysed with Gap Light Analyzer (GLA) showed reasonable agreement with a mean canopy transmissivity of 75 % in 2008 and 74 % in 2009. The canopy transmissivity was found to be independent of the diffuse fraction of radiation as the canopy is very sparse. A series of survey grids and transects were established to scale up from the below canopy pyranometers to the landscape scale. Hemispherical photographs analysed with GLA showed the sparse forest canopy had a mean transmissivity of 78 % and a mean LAI of 0.25, whereas the open tundra had a mean transmissivity of 97 % and a mean LAI of < 0.01. Snow surveys showed the sparse forest snow depth to vary between 0.34 and 0.55 m, whereas the snow depth in the open tundra varied between 0.12 and 0.18 m. Observations of canopy temperatures showed a strong influence of incident shortwave radiation warming the tree branches to temperatures up to 15 °C warmer than ambient air temperature on the south facing sides of the trees, and up to 6 °C on the north facing sides of the trees. To reproduce the observed radiation balance, two canopy models (Homogenous and Clumped) were developed. The Homogeneous canopy model assumes a single tree tile with a uniform sparse canopy. The…

Subjects/Keywords: 551.4; radiation; sparse; forest; land surface model; snow; modelling; JULES; shaded gap; shortwave; longwave; snow melt; transmissivity; hemispherical photography; snow surveys; Arctic; surface processes; high latitude; canopy; birch

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Turton, R. H. (2017). The impact of the radiation balance on snowmelt in a sparse deciduous birch forest. (Doctoral Dissertation). University of Edinburgh. Retrieved from http://hdl.handle.net/1842/29567

Chicago Manual of Style (16^th Edition):

Turton, Rachael Heather. “The impact of the radiation balance on snowmelt in a sparse deciduous birch forest.” 2017. Doctoral Dissertation, University of Edinburgh. Accessed April 12, 2021. http://hdl.handle.net/1842/29567.

MLA Handbook (7^th Edition):

Turton, Rachael Heather. “The impact of the radiation balance on snowmelt in a sparse deciduous birch forest.” 2017. Web. 12 Apr 2021.

Vancouver:

Turton RH. The impact of the radiation balance on snowmelt in a sparse deciduous birch forest. [Internet] [Doctoral dissertation]. University of Edinburgh; 2017. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/1842/29567.

Council of Science Editors:

Turton RH. The impact of the radiation balance on snowmelt in a sparse deciduous birch forest. [Doctoral Dissertation]. University of Edinburgh; 2017. Available from: http://hdl.handle.net/1842/29567

9. U.F. Minora. Applicazione di tecniche remote sensing per lo studio dell'evoluzione e della dinamica criosferica in aree remote e di alta quota.

Degree: 2016, Università degli Studi di Milano

URL: http://hdl.handle.net/2434/363344

► I ghiacciai sono efficaci indicatori climatici poichè si modificano in risposta ai cambi del clima (es. temperatura e precipitazioni). L'attenzione sui ghiacciai di montagna sta… (more)

▼ I ghiacciai sono efficaci indicatori climatici poichè si modificano in risposta ai cambi del clima (es. temperatura e precipitazioni). L'attenzione sui ghiacciai di montagna sta aumentando tra la comunità scientifica per via del loro sempre più evidente arretramento a scala globale negli ultimi cinquant'anni. Ciò è conseguenza del riscaldamento globale. Comprendere il comportamento dei ghiacciai in risposta al cambio climatico è di enorme importanza non solo per arricchire la conoscenza scientifica, ma anche per poter meglio gestire in futuro le situazioni di rischio naturale che possono colpire le popolazioni che vivono nelle zone montuose, sia nel breve termine (es. GLOF), sia nel lungo (es. Siccità). Questa tesi di dottorato analizza differenti aspetti della criosfera (ghiacciai e neve) per descriverne la variabilità recente e le relazioni con la dinamica climatica. Inizialmente ci si è concentrati sul Karakorum. Questa è un’area particolare per gli studi criosferici, che non segue i trend globali di regresso; infatti, in questa zona il bilancio di massa netto dei ghiacciai nei primi anni del ventunesimo secolo è stato leggermente positivo, con anche taluni casi di espansione. Questa eccezionale situazione è riconosciuta con il nome di Anomalia del Karakorum (Karakoram Anomaly). Più precisamente il presente elaborato si focalizza sulla zona del Central Karakoram National Park (CKNP), un'area protetta nel nord del Pakistan, rappresentativa della glaciazione dell'intera catena del Karakorum. In questa regione, i venti occidentali rappresentano il sistema di venti dominante e sono presenti nella stagione invernale, mentre la confinante regione Himalayana è sotto l'influenza predominante dei monsoni, che sono venti estivi. Il presente lavoro descrive in maniera completa lo stato dei ghiacciai del CKNP e la loro recente evoluzione. Ciò è stato possibile a seguito della compilazione del catasto glaciale del parco per gli anni 2001 e 2010, a sua volta descritto nel dettaglio nel presente elaborato. Inoltre è discussa l'analisi dei cambiamenti climatici poi messa in relazione con quelli glaciali, per poter comprendere le cause dietro l'Anomalia del Karakorum. Il cambiamento areale dei 711 ghiacciai mappati nell'area di studio è stato -0.4 ± 202.9 km2 (su 4605.9 ± 86.1 km2 nel 2001), il che evidenzia una generale situazione di stabilità. Anche l'analisi climatica supporta tale condizione di stabilità. Durante il periodo 2001–2010 si è osservato grazie ai dati del sensore MODIS un leggero aumento delle aree coperte da neve a fine estate. Allo stesso tempo, dati meteo dalle stazioni disponibili hanno rivelato un aumento delle nevicate e una diminuzione della temperatura media dell'aria in estate fin dal 1980, il che si tradurrebbe in coperture nivali più persistenti durante la stagione ablativa. Questi risultati vanno a favore della preservazione glaciale nelle zone di ablazione dovuta a una copertura di neve più duratura, e un maggiore accumulo a quote più alte, presupponendo bilanci di massa netti tendenti al segno… Advisors/Committee Members: co-tutor: M. Guglielmin, C. Smiraglia, G. Diolaiuti, D. Bocchiola, coordinator: N. Saino, SMIRAGLIA, CLAUDIO, SAINO, NICOLA MICHELE FRANCESCO.

Subjects/Keywords: remote sensing; glaciers; cryosphere; snow cover; debris-covered glacier; ice melt; climate change; Settore GEO/04 - Geografia Fisica e Geomorfologia

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APA (6^th Edition):

Minora, U. (2016). Applicazione di tecniche remote sensing per lo studio dell'evoluzione e della dinamica criosferica in aree remote e di alta quota. (Thesis). Università degli Studi di Milano. Retrieved from http://hdl.handle.net/2434/363344

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Minora, U.F.. “Applicazione di tecniche remote sensing per lo studio dell'evoluzione e della dinamica criosferica in aree remote e di alta quota.” 2016. Thesis, Università degli Studi di Milano. Accessed April 12, 2021. http://hdl.handle.net/2434/363344.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Minora, U.F.. “Applicazione di tecniche remote sensing per lo studio dell'evoluzione e della dinamica criosferica in aree remote e di alta quota.” 2016. Web. 12 Apr 2021.

Vancouver:

Minora U. Applicazione di tecniche remote sensing per lo studio dell'evoluzione e della dinamica criosferica in aree remote e di alta quota. [Internet] [Thesis]. Università degli Studi di Milano; 2016. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/2434/363344.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Minora U. Applicazione di tecniche remote sensing per lo studio dell'evoluzione e della dinamica criosferica in aree remote e di alta quota. [Thesis]. Università degli Studi di Milano; 2016. Available from: http://hdl.handle.net/2434/363344

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

University of Colorado

10. Khan, Alia Lauren. Quantifying Sources, Distribution, and Processing of Light Absorbing Aerosols in the Cryosphere: a Comparison of Dissolved and Refractory Black Carbon in Polar and High Mountain Regions.

Degree: PhD, 2016, University of Colorado

URL: https://scholar.colorado.edu/cven_gradetds/47

► Light absorbing aerosols (LAAs), such as black carbon (BC), in snow and ice are one of the least understood parameters in global climate models.… (more)

▼ Light absorbing aerosols (LAAs), such as black carbon (BC), in snow and ice are one of the least understood parameters in global climate models. This is due to complicated physical processes within the cryosphere and too few in situ observations. BC is derived from the incomplete combustion of biomass and fossil fuels and can enhance melt water generation and glacial recession when deposited on snow and ice surfaces. Measurements are limited due to the difficulty of collecting and preserving samples for analysis from remote environments. In order to help build a larger repository of ground observations, this dissertation explores the concentration and composition of black carbon (BC) in snow and glacial melt-water across the polar regions in the Arctic and Antarctic, as well as major mountain regions such as the Himalayas, Rockies, and Andes Mountains. Three state-of-the-art methods for BC detection are applied. The first chapter identifies chemical signatures of past and present sources of dissolved black carbon (DBC) in Antarctic lakes, utilizing a DBC molecular marker method. Here we find that DBC with a woody signature is preserved in the deep, ancient brines of Antarctic lake bottom waters. In contrast, the surface waters are enriched in BC from fossil fuels. The second chapter, which also utilizes the DBC molecular marker technique, explores DBC concentration and composition across a global sample set from the cryosphere. Here we show the bottom waters of Antarctic lakes are surprisingly much more enriched in DBC compared to other regions of the cryosphere. The third and fourth chapters utilize the Single Particle Soot Photometer to measure refractory black carbon (rBC). The third chapter also applies spectral albedo measurements and the light absorption heating method to show that coal dust from an active mine in Svalbard, Norway significantly reduces the spectral reflectance of the surrounding Arctic surface snow. The fourth chapter reports aerosol rBC concentrations in the boundary layer of the McMurdo Dry Valleys, as well as in snow from the accumulation area of the Commonwealth Glacier. Here we determine that aerosol concentrations increase during katabatic wind events, but there is no significant trend in deposition in the snow pit. These findings support the importance of real in-situ observations in order to fully understand the role of BC in the global carbon cycle. Also, these ground-based measurements will likely serve as validation for future remote sensing of snow/ice impurities and LAAs deposition models. Advisors/Committee Members: Diane M. McKnight, Paul Chinowsky, Lupita Montoya, Tad Pfeffer, Mark Williams.

Subjects/Keywords: black carbon; cryosphere; glacial melt; light absorbing aerosols; polar regions; snow; Environmental Engineering; Environmental Sciences; Geochemistry

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APA (6^th Edition):

Khan, A. L. (2016). Quantifying Sources, Distribution, and Processing of Light Absorbing Aerosols in the Cryosphere: a Comparison of Dissolved and Refractory Black Carbon in Polar and High Mountain Regions. (Doctoral Dissertation). University of Colorado. Retrieved from https://scholar.colorado.edu/cven_gradetds/47

Chicago Manual of Style (16^th Edition):

Khan, Alia Lauren. “Quantifying Sources, Distribution, and Processing of Light Absorbing Aerosols in the Cryosphere: a Comparison of Dissolved and Refractory Black Carbon in Polar and High Mountain Regions.” 2016. Doctoral Dissertation, University of Colorado. Accessed April 12, 2021. https://scholar.colorado.edu/cven_gradetds/47.

MLA Handbook (7^th Edition):

Khan, Alia Lauren. “Quantifying Sources, Distribution, and Processing of Light Absorbing Aerosols in the Cryosphere: a Comparison of Dissolved and Refractory Black Carbon in Polar and High Mountain Regions.” 2016. Web. 12 Apr 2021.

Vancouver:

Khan AL. Quantifying Sources, Distribution, and Processing of Light Absorbing Aerosols in the Cryosphere: a Comparison of Dissolved and Refractory Black Carbon in Polar and High Mountain Regions. [Internet] [Doctoral dissertation]. University of Colorado; 2016. [cited 2021 Apr 12]. Available from: https://scholar.colorado.edu/cven_gradetds/47.

Council of Science Editors:

Khan AL. Quantifying Sources, Distribution, and Processing of Light Absorbing Aerosols in the Cryosphere: a Comparison of Dissolved and Refractory Black Carbon in Polar and High Mountain Regions. [Doctoral Dissertation]. University of Colorado; 2016. Available from: https://scholar.colorado.edu/cven_gradetds/47

University of Arizona

11. Dressler, Kevin Andrew. Estimating the Spatial Distribution of Snow Water Equivalent and Simulated Snowmelt Runoff Modeling in Headwater Basins of the Semi-arid Southwest .

Degree: 2005, University of Arizona

URL: http://hdl.handle.net/10150/190929

► The spatial distribution of snowpack in relation to snow water equivalent (SWE) and covered extent is highly variable in time both seasonally and interannually. In… (more)

▼ The spatial distribution of snowpack in relation to snow water equivalent (SWE) and covered extent is highly variable in time both seasonally and interannually. In order to assess basin water resources, SWE must be distributed to areal estimates. This spatially distributed SWE connects the point scale to the larger scale of the basin (i.e. macro-scale), requiring a combination approach of statistical interpolation techniques and snowpack extent constraint from remote sensing. This research connects those multiple spatial scales and applies the combined remote sensing and ground-based SWE products in a hydrologic model setting to aid in improving streamflow forecasting in the mountainous terrain of snowmelt-dominated basins, a current modeling gap. Four specific advancements were achieved: 1) a comprehensive assessment of spatial distribution techniques in interpolating point snow water equivalent (SWE) measurements at snow telemetry (SNOTEL) stations to the macro-scale was made and an optimal technique for distributing SWE on this scale was obtained; 2) differences between two major data sources of SWE (SNOTEL and snowcourse) were quantified for both point-scale variability and interpolated macro-scale variability to determine spatial and temporal differences in data sources for dry, average and wet years to better inform water resources management applications; 3) basin-scale estimates of ground-based SWE and snow covered area (SCA) from remote sensing were evaluated relative to equivalent fields calculated by a hydrologic model and the effect of assimilating the remote sensing products into the model were investigated; and 4) in the context of (3), improvements were made in macro-scale SCA estimates through both a canopy correction and a low pass statistical filter in an effort to correct for the relatively low resolution of remotely sensed estimates. Advisors/Committee Members: Shtutleworth, W. James (committeemember), Nijssen, Bart M. (committeemember), Fassnacht, Steven R. (committeemember).

Subjects/Keywords: Hydrology.; Runoff – Southwestern States – Mathematical models.; Snow melt.; Meltwater.

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Dressler, K. A. (2005). Estimating the Spatial Distribution of Snow Water Equivalent and Simulated Snowmelt Runoff Modeling in Headwater Basins of the Semi-arid Southwest . (Doctoral Dissertation). University of Arizona. Retrieved from http://hdl.handle.net/10150/190929

Chicago Manual of Style (16^th Edition):

Dressler, Kevin Andrew. “Estimating the Spatial Distribution of Snow Water Equivalent and Simulated Snowmelt Runoff Modeling in Headwater Basins of the Semi-arid Southwest .” 2005. Doctoral Dissertation, University of Arizona. Accessed April 12, 2021. http://hdl.handle.net/10150/190929.

MLA Handbook (7^th Edition):

Dressler, Kevin Andrew. “Estimating the Spatial Distribution of Snow Water Equivalent and Simulated Snowmelt Runoff Modeling in Headwater Basins of the Semi-arid Southwest .” 2005. Web. 12 Apr 2021.

Vancouver:

Dressler KA. Estimating the Spatial Distribution of Snow Water Equivalent and Simulated Snowmelt Runoff Modeling in Headwater Basins of the Semi-arid Southwest . [Internet] [Doctoral dissertation]. University of Arizona; 2005. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/10150/190929.

Council of Science Editors:

Dressler KA. Estimating the Spatial Distribution of Snow Water Equivalent and Simulated Snowmelt Runoff Modeling in Headwater Basins of the Semi-arid Southwest . [Doctoral Dissertation]. University of Arizona; 2005. Available from: http://hdl.handle.net/10150/190929

12. Kormos, Patrick Richard. Estimating Deep Percolation in the Mountain Rain-Snow Transition Zone.

Degree: 2013, Boise State University

URL: https://scholarworks.boisestate.edu/td/786

► Deep percolation (DP) is estimated from a small study catchment in the semi arid rain-snow transition zone in the foothills north of Boise, ID. A… (more)

▼ Deep percolation (DP) is estimated from a small study catchment in the semi arid rain-snow transition zone in the foothills north of Boise, ID. A water balance is performed at the catchment soil bedrock interface, where soil drainage is assumed to be partitioned into DP and streamflow. While stream flow is measured, soil drainage must be estimated. We model the snow dynamics and surface water inputs (SWI) to the soil (Chapter 3), and the soil dynamics and soil drainage to the soil-bedrock interface (Chapter 4). The high spatiotemporal dataset used in this modeling effort is presented for the 2011 water year, which includes weather, topographic, vegetation, and soils data (Chapter 1). The image SNOw and mass BALance model is used to predict the distributed surface water inputs at a 2.5 m2 resolution. Southwest facing slopes receive smaller and more frequent SWI from mid winter snowmelt, while the northeast slope receives more SWI during the spring. Rain on snow events produce similar SWI between slopes. Turbulent fluxes dominated the snowpack energetics in four of the five rain-on-snow events. Advective fluxes are greater than 17% during the 2 rain-on-snow events in December and January. Net radiation fluxes dominate spring melt events. Variations in the method used to distribute precipitation may result in large differences in total precipitation to the basin. The Soil Ecohydraulic Model is used to predict soil drainage at 57 points across the catchment. Soils on the southwest facing slope drain more often throughout the water year, but the northeast facing slope contributes a greater total magnitude of soil drainage. Peaks in catchment soil drainage and deep percolation coincide with rain on snow events. Deep percolation is estimated to be 272 mm ± 34 mm for the 2011 water year, which is 29% ±4% of the precipitation. In summary, we provide a high temporal and spatial data set from a catchment in the rain snow transition zone in Chapter 2. This dataset provides a) soil, vegetation, and weather data to parameterize and drive hydrologic models, and b) snow and hydrologic response data to validate hydrologic models. The data is used to run a physically based snow accumulation and melt model, from which we obtain a high spatial and temporal resolution data set of surface water inputs to the catchment in Chapter 3. Chapter 4 estimates deep percolation from the catchment using the surface water input time series from Chapter 3.

Subjects/Keywords: deep percolation; rain snow transition zone; snow distribution; snow melt; rain on snow; soil; Water Resource Management

…27 CHAPTER THREE: SNOW DISTRIBUTION, MELT AND SURFACE WATER INPUTS TO THE SOIL IN THE… …of a fully distributed physically-based snow accumulation and melt model to obtain… …distribution of the snow accumulation and melt at fine spatial and temporal resolutions. These models… …5 CHAPTER TWO: SOIL, SNOW, WEATHER, AND SUB-SURFACE STORAGE DATA FROM A MOUNTAIN… …CATCHMENT IN THE RAIN-SNOW TRANSITION ZONE…

10 more images…

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APA (6^th Edition):

Kormos, P. R. (2013). Estimating Deep Percolation in the Mountain Rain-Snow Transition Zone. (Thesis). Boise State University. Retrieved from https://scholarworks.boisestate.edu/td/786

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Kormos, Patrick Richard. “Estimating Deep Percolation in the Mountain Rain-Snow Transition Zone.” 2013. Thesis, Boise State University. Accessed April 12, 2021. https://scholarworks.boisestate.edu/td/786.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Kormos, Patrick Richard. “Estimating Deep Percolation in the Mountain Rain-Snow Transition Zone.” 2013. Web. 12 Apr 2021.

Vancouver:

Kormos PR. Estimating Deep Percolation in the Mountain Rain-Snow Transition Zone. [Internet] [Thesis]. Boise State University; 2013. [cited 2021 Apr 12]. Available from: https://scholarworks.boisestate.edu/td/786.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Kormos PR. Estimating Deep Percolation in the Mountain Rain-Snow Transition Zone. [Thesis]. Boise State University; 2013. Available from: https://scholarworks.boisestate.edu/td/786

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Jawaharlal Nehru University

13. Chauhan, Devendra Singh. Chemical characteristics of snow, ice and meltwater from Satopanth and Bhagirath Kharak Glacier basins, Alaknanda Valley, India; -.

Degree: International Studies, 1993, Jawaharlal Nehru University

URL: http://shodhganga.inflibnet.ac.in/handle/10603/14249

None

-

Advisors/Committee Members: Subramanian, V, Hasnain, S I.

Subjects/Keywords: International Studies; Alaknanda Valley; Snow; ice; melt water; Satopant; Bhagirath Kharak glacier basins

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APA (6^th Edition):

Chauhan, D. S. (1993). Chemical characteristics of snow, ice and meltwater from Satopanth and Bhagirath Kharak Glacier basins, Alaknanda Valley, India; -. (Thesis). Jawaharlal Nehru University. Retrieved from http://shodhganga.inflibnet.ac.in/handle/10603/14249

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Chauhan, Devendra Singh. “Chemical characteristics of snow, ice and meltwater from Satopanth and Bhagirath Kharak Glacier basins, Alaknanda Valley, India; -.” 1993. Thesis, Jawaharlal Nehru University. Accessed April 12, 2021. http://shodhganga.inflibnet.ac.in/handle/10603/14249.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Chauhan, Devendra Singh. “Chemical characteristics of snow, ice and meltwater from Satopanth and Bhagirath Kharak Glacier basins, Alaknanda Valley, India; -.” 1993. Web. 12 Apr 2021.

Vancouver:

Chauhan DS. Chemical characteristics of snow, ice and meltwater from Satopanth and Bhagirath Kharak Glacier basins, Alaknanda Valley, India; -. [Internet] [Thesis]. Jawaharlal Nehru University; 1993. [cited 2021 Apr 12]. Available from: http://shodhganga.inflibnet.ac.in/handle/10603/14249.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Chauhan DS. Chemical characteristics of snow, ice and meltwater from Satopanth and Bhagirath Kharak Glacier basins, Alaknanda Valley, India; -. [Thesis]. Jawaharlal Nehru University; 1993. Available from: http://shodhganga.inflibnet.ac.in/handle/10603/14249

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Université Catholique de Louvain

14. Fettweis, Xavier. Reconstruction of the 1979-2005 Greenland ice sheet surface mass balance using satellite data and the regional climate model MAR.

Degree: 2006, Université Catholique de Louvain

URL: http://hdl.handle.net/2078.1/5384

►

In order to improve our knowledge on the current state and variability of the Greenland ice sheet surface mass balance (SMB), a 27-year simulation (1979-2005)… (more)

▼

In order to improve our knowledge on the current state and variability of the Greenland ice sheet surface mass balance (SMB), a 27-year simulation (1979-2005) has been performed with the coupled atmosphere-snow regional model MAR. This simulation reveals an increase in the main factors of the SMB which are, on the one hand, the snowfall (+ 1.6 ± 1.8 km3 yr-1) in winter and on the other hand, the run-off (+ 4.2 ± 1.9 km3 yr-1) in summer. The net effect of these two competing factors leads to a SMB loss rate of - 2.7 ± 3.0 km3 yr-1, which has a significance of 87%. The melt extent derived from the passive microwave satellite data since 1979 also shows this trend. The melt water supply has increased because the Greenland ice sheet has been warming up by + 0.09 ± 0.04 °C yr-1 since 1979. This warming comes from a uniform increase of downward infra-red radiation which can not be explained by the natural variability. These changes result very likely from the global warming induced by human activities. As a result, it seems that: i) increased melting dominates over increased accumulation in a warming scenario, ii) the Greenland ice sheet has been significantly losing mass since the beginning of the 1980's by an increasing melt water run-off as well as by a probable increase of iceberg discharge into the ocean due to the "Zwally effect" (the melt water-induced ice sheet flow acceleration) and iii) the Greenland ice sheet is projected to continue to lose mass in the future. The Greenland ice sheet melting could have an effect on the stability of the thermohaline circulation (THC) and the global sea level rise. On the one hand, increases in the freshwater flux from the Greenland ice sheet (glacier discharge and run-off) could perturb the THC by reducing the density contrast driving it. On the other hand, the melting of the whole Greenland ice sheet would account for a global mean sea level rise of 7.4 m.

(PHYS 3) – UCL, 2006

Advisors/Committee Members: UCL - SC/PHYS - Département de physique, Nauts, André, Fichefet, Thierry, Lefebre, Filip, Schayes, Guy, van Lipzig, Nicole, Prieels, René, Gallée, Hubert, van Ypersele, Jean-Pascal.

Subjects/Keywords: Microwave; Climate; Model; Snow; Satellite; Melt; Ice sheet; Mass balance; Greenland

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APA (6^th Edition):

Fettweis, X. (2006). Reconstruction of the 1979-2005 Greenland ice sheet surface mass balance using satellite data and the regional climate model MAR. (Thesis). Université Catholique de Louvain. Retrieved from http://hdl.handle.net/2078.1/5384

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Fettweis, Xavier. “Reconstruction of the 1979-2005 Greenland ice sheet surface mass balance using satellite data and the regional climate model MAR.” 2006. Thesis, Université Catholique de Louvain. Accessed April 12, 2021. http://hdl.handle.net/2078.1/5384.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Fettweis, Xavier. “Reconstruction of the 1979-2005 Greenland ice sheet surface mass balance using satellite data and the regional climate model MAR.” 2006. Web. 12 Apr 2021.

Vancouver:

Fettweis X. Reconstruction of the 1979-2005 Greenland ice sheet surface mass balance using satellite data and the regional climate model MAR. [Internet] [Thesis]. Université Catholique de Louvain; 2006. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/2078.1/5384.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Fettweis X. Reconstruction of the 1979-2005 Greenland ice sheet surface mass balance using satellite data and the regional climate model MAR. [Thesis]. Université Catholique de Louvain; 2006. Available from: http://hdl.handle.net/2078.1/5384

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

15. Litt, Maxime. Etude de la couche de surface atmosphérique et des flux turbulents sur deux glaciers de montagne dans les Andes tropicales et les alpes Françaises : A study of the atmospheric surface layer and turbulent fluxes on two mountain glaciers in the Tropical Andes and in the French Alps.

Degree: Docteur es, Sciences de l'univers, 2015, Université Grenoble Alpes (ComUE)

URL: http://www.theses.fr/2015GREAU005

► Nous étudions les flux turbulents de chaleur sensible et de chaleur latente, qui sont mal compris et mal mesurés sur les glaciers, à l'aide de… (more)

▼ Nous étudions les flux turbulents de chaleur sensible et de chaleur latente, qui sont mal compris et mal mesurés sur les glaciers, à l'aide de campagnes de terrain déployées dans la zone d'ablation du glacier tropical du Zongo (16°S, Bolivie, 4900-6000 m) durant la saison sèche de l'hiver austral et sur le glacier alpin de Saint-Sorlin (Alpes Françaises, 45°N, 2600-3400 m) durant l'été boréal. Un mât de 6 m permettait la mesure des profils verticaux de vitesse de vent et de température de l'air et des mâts de 2 m comportaient des systèmes de covariances turbulentes (CT). Nous étudions l'évolution temporelle des flux turbulents et l'applicabilité de la méthode aérodynamique des profils en terrain complexe de montagne. Les hypothèses sont discutées via la caractérisation des régimes de vent et de la turbulence. Nous calculons ensuite les flux et les erreurs associées. Sur le Zongo, sous forçage synoptique faible, un écoulement catabatique s'installe de la fin d'après-midi jusqu'au matin, avec un maximum de vitesse de vent à environ 2 m de hauteur. Les forçages synoptiques forts s'alignent approximativement avec le glacier, provoquant un intense écoulement descendant, et dans ce cas nous n'observons pas de maximum de vitesse de vent. Souvent, autour de midi, des vents ascendants sont observés. Sur le glacier de Saint-Sorlin les forçages associés à des épisodes de Foehn ou à des dépressions se déplaçant depuis l'ouest, s'alignent approximativement avec le glacier, générant des vents forts descendants. Quand le forçage synoptique est modéré, un maximum de vitesse de vent est observé nuit et jour 50% du temps. Des vents ascendants sont observés 15% du temps, quand le forçage synoptique est faible. La couche de surface est perturbée par des tourbillons de couches externes sous vent fort, ou de lentes oscillations en écoulement catabatique. Ces perturbations influencent les flux turbulents. Les erreurs aléatoires sur la méthode des profils sont dues principalement à des incertitudes sur la température. L'erreur reste faible sur les flux moyens. La couche de surface est rarement plus épaisse que 2 m et la méthode des profils appliquée à l'aide des mesures plus obtenus plus haut sous-estime les flux de surface de 20% à 70% . Quand un maximum de vitesse de vent est observé, les flux sont sous-estimés même à 2 m. L'influence des perturbations de la couche de surface n'est pas capturée par la méthode des profils, et les flux sont environ 40% inférieurs à ceux mesurés par CT. Ces derniers sont affectés par d'importantes erreurs aléatoires, en raison d'un échantillonnage statistique insuffisant des grands tourbillons. La méthode sous-estime probablement les flux à cause d'une sous-estimation de la vitesse verticale (~15%) et de la divergence verticale des flux. Sur le glacier du Zongo, l'air de haute altitude est très sec et la sublimation (quelques mm d'eau par jour) est un important puits d'énergie à la surface. Le flux de chaleur sensible est un important gain d'énergie la nuit sous l'influence de vents forts (de 30 à 50 W m-2),… Advisors/Committee Members: Sicart, Jean-Emmanuel (thesis director), Wagnon, Patrick (thesis director).

Subjects/Keywords: Bilan d'énergie; Fusion de la neige et de la glace; Flux turbulents; Couche limite; Energy balance; Snow and ice melt; Turbulent fluxes; Boundary layer; 550

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Litt, M. (2015). Etude de la couche de surface atmosphérique et des flux turbulents sur deux glaciers de montagne dans les Andes tropicales et les alpes Françaises : A study of the atmospheric surface layer and turbulent fluxes on two mountain glaciers in the Tropical Andes and in the French Alps. (Doctoral Dissertation). Université Grenoble Alpes (ComUE). Retrieved from http://www.theses.fr/2015GREAU005

Chicago Manual of Style (16^th Edition):

Litt, Maxime. “Etude de la couche de surface atmosphérique et des flux turbulents sur deux glaciers de montagne dans les Andes tropicales et les alpes Françaises : A study of the atmospheric surface layer and turbulent fluxes on two mountain glaciers in the Tropical Andes and in the French Alps.” 2015. Doctoral Dissertation, Université Grenoble Alpes (ComUE). Accessed April 12, 2021. http://www.theses.fr/2015GREAU005.

MLA Handbook (7^th Edition):

Litt, Maxime. “Etude de la couche de surface atmosphérique et des flux turbulents sur deux glaciers de montagne dans les Andes tropicales et les alpes Françaises : A study of the atmospheric surface layer and turbulent fluxes on two mountain glaciers in the Tropical Andes and in the French Alps.” 2015. Web. 12 Apr 2021.

Vancouver:

Litt M. Etude de la couche de surface atmosphérique et des flux turbulents sur deux glaciers de montagne dans les Andes tropicales et les alpes Françaises : A study of the atmospheric surface layer and turbulent fluxes on two mountain glaciers in the Tropical Andes and in the French Alps. [Internet] [Doctoral dissertation]. Université Grenoble Alpes (ComUE); 2015. [cited 2021 Apr 12]. Available from: http://www.theses.fr/2015GREAU005.

Council of Science Editors:

Litt M. Etude de la couche de surface atmosphérique et des flux turbulents sur deux glaciers de montagne dans les Andes tropicales et les alpes Françaises : A study of the atmospheric surface layer and turbulent fluxes on two mountain glaciers in the Tropical Andes and in the French Alps. [Doctoral Dissertation]. Université Grenoble Alpes (ComUE); 2015. Available from: http://www.theses.fr/2015GREAU005

University of Minnesota

16. Novotny, Eric Vladimir. Road deicing salt impacts on urban water quality.

Degree: PhD, Civil Engineering, 2009, University of Minnesota

URL: http://purl.umn.edu/56780

► Salt is widely used for ice and snow control on roads in the US, Canada and other parts of the world affected by adverse winter… (more)

▼ Salt is widely used for ice and snow control on roads in the US, Canada and other parts of the world affected by adverse winter driving conditions. The primary product applied in North America for deicing of roads is sodium chloride (NaCl), a readily available and inexpensive material. The use of sodium chloride as a road deicing chemical has increased dramatically in the northern areas of the United States over the last 50 years with about 23 million tons used in 2005. The primary objective of my research was to determine how road salt applications influenced the water quality in a major metropolitan area (Twin Cities metropolitan area (TCMA) of Minneapolis/St Paul, Minnesota, USA). This objective was met by collecting and analyzing data from area lakes, streams and rivers and through the development 0 Dimensional (0D) and 1 Dimensional (1D) models. It was determined that on average over 70% of the chloride applied annually in the TCMA was retained in the watershed instead of entering the Mississippi River and eventually exported to the Gulf of Mexico. Salinity cycles were observed in area lakes with high concentration in the winter followed by lower concentrations in the spring and summer. Mean annual concentrations in 38 lakes in the TCMA rose on average 1.4 mg/L per year over 22-years matching a similar trend in the amount of rock salt the state of Minnesota purchased over the same time period. Salt water inflows changed the natural mixing behavior of area lakes. In some lakes monomictic behavior developed with mixing events only occuring in the fall. The presence of a saline layer at the bottom of the lake prohibited dissolved oxygen from reaching the benthic water layer in the spring extending the anoxic period of this water layer by 6 months. Simulations conducted without the presence of a saline layer showed complete mixing and oxygenation of the benthic layers in the spring and fall. Rising Cl concentrations in lakes are expected to continue. If the annual inputs of salt to the lakes were stopped it would take 10 to 30 years to reach chloride concentrations equal to predevelopment concentration. Chloride retention in urban areas where road salt is applied should cause much concern. Mitigation measures, best management practices (BMPs) for road salt application and alternatives to NaCl need to be examined.

Subjects/Keywords: Chloride; Minnesota; Road Salt; Snow melt; Urban runoff; Civil Engineering

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APA (6^th Edition):

Novotny, E. V. (2009). Road deicing salt impacts on urban water quality. (Doctoral Dissertation). University of Minnesota. Retrieved from http://purl.umn.edu/56780

Chicago Manual of Style (16^th Edition):

Novotny, Eric Vladimir. “Road deicing salt impacts on urban water quality.” 2009. Doctoral Dissertation, University of Minnesota. Accessed April 12, 2021. http://purl.umn.edu/56780.

MLA Handbook (7^th Edition):

Novotny, Eric Vladimir. “Road deicing salt impacts on urban water quality.” 2009. Web. 12 Apr 2021.

Vancouver:

Novotny EV. Road deicing salt impacts on urban water quality. [Internet] [Doctoral dissertation]. University of Minnesota; 2009. [cited 2021 Apr 12]. Available from: http://purl.umn.edu/56780.

Council of Science Editors:

Novotny EV. Road deicing salt impacts on urban water quality. [Doctoral Dissertation]. University of Minnesota; 2009. Available from: http://purl.umn.edu/56780

Utah State University

17. Thies, Paul R. The Effects of Elevation and Vegetation Type on Snow Accumulation and Melt in Logan Canyon, Utah.

Degree: MS, Watershed Sciences, 1973, Utah State University

URL: https://digitalcommons.usu.edu/etd/2194

► Snow accumulation and melt characteristics were studied in Logan Canyon, Utah. Three replications of aspen, conifer, and open field types at 6300, 7100,and 8000… (more)

Subjects/Keywords: Elevation; Vegetation; Snow; Accumulation; Melt; Logan; Canyon; Utah; Life Sciences; Other Life Sciences

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APA (6^th Edition):

Thies, P. R. (1973). The Effects of Elevation and Vegetation Type on Snow Accumulation and Melt in Logan Canyon, Utah. (Masters Thesis). Utah State University. Retrieved from https://digitalcommons.usu.edu/etd/2194

Chicago Manual of Style (16^th Edition):

Thies, Paul R. “The Effects of Elevation and Vegetation Type on Snow Accumulation and Melt in Logan Canyon, Utah.” 1973. Masters Thesis, Utah State University. Accessed April 12, 2021. https://digitalcommons.usu.edu/etd/2194.

MLA Handbook (7^th Edition):

Thies, Paul R. “The Effects of Elevation and Vegetation Type on Snow Accumulation and Melt in Logan Canyon, Utah.” 1973. Web. 12 Apr 2021.

Vancouver:

Thies PR. The Effects of Elevation and Vegetation Type on Snow Accumulation and Melt in Logan Canyon, Utah. [Internet] [Masters thesis]. Utah State University; 1973. [cited 2021 Apr 12]. Available from: https://digitalcommons.usu.edu/etd/2194.

Council of Science Editors:

Thies PR. The Effects of Elevation and Vegetation Type on Snow Accumulation and Melt in Logan Canyon, Utah. [Masters Thesis]. Utah State University; 1973. Available from: https://digitalcommons.usu.edu/etd/2194

The Ohio State University

18. Fortner, Sarah K. The Geochemistry Of Glacier Snow And Melt: The Oregon Cascades And The Taylor Valley, Antarctica.

Degree: PhD, Geological Sciences, 2008, The Ohio State University

URL: http://rave.ohiolink.edu/etdc/view?acc_num=osu1228255773

► Snow and glacial melt were investigated for their dissolved (<0.4µm) and environmentally available (unfiltered and acidified 2% HNO3 v/v) elemental concentrations and relation with… (more)

▼ Snow and glacial melt were investigated for their dissolved (<0.4µm) and environmentally available (unfiltered and acidified 2% HNO3 v/v) elemental concentrations and relation with melt. These studies are presented as three manuscripts. The first manuscript examines geochemical differences between fresh and ablation snow at Eliot Glacier, Mount Hood in the Oregon Cascades. Unlike major ions, environmentally available elements are retained during snowmelt and or added via dry deposition throughout the melt season. Proglacial stream dissolved, or solution chemistry reflects the large degree of processing, primarily weathering and adsorption that occur as water is routed in, through, and beneath the glacier and trace elements bear little relation to their snow concentrations. The second paper details the importance of aeolian deposition to environmentally available elemental concentrations and distributions in the Taylor Valley, Antarctica. Unlike the Oregon Cascades, there is little precipitation in the Taylor Valley and dry deposition is the dominant source of environmentally available elements. Therefore, proximity to valley floor sediment, wind intensity, wind direction, and glacier surface aspect explain the large degree of chemical heterogeneity between three nearby (<10 km) glacier accumulation zones. Finally the third manuscript explores the controls on dissolved and environmentally available elemental concentrations in supraglacial and proglacial streams in Taylor Valley, Antarctica. This includes identifying the influences of aeolian deposition, hyporheic exchange, and biological uptake on stream geochemistry. Elemental behaviors are examined along with their daily, seasonal, and interannual stream hydrologic conditions. Taylor Valley stream geochemistry is sensitive to landscape aspect as well as to changes in climate including shifts in wind speed and direction, austral summer temperatures, and cloud cover conditions. Decadal ‘flood events’ are extremely important to Taylor Valley ecosystems as they replenish water and are a source of important trace and minor elements. Advisors/Committee Members: Lyons, W. Berry (Advisor).

Subjects/Keywords: Environmental Science; Geochemistry; trace elements; snow; glacier; melt; eolian; diel; metals; streams

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APA (6^th Edition):

Fortner, S. K. (2008). The Geochemistry Of Glacier Snow And Melt: The Oregon Cascades And The Taylor Valley, Antarctica. (Doctoral Dissertation). The Ohio State University. Retrieved from http://rave.ohiolink.edu/etdc/view?acc_num=osu1228255773

Chicago Manual of Style (16^th Edition):

Fortner, Sarah K. “The Geochemistry Of Glacier Snow And Melt: The Oregon Cascades And The Taylor Valley, Antarctica.” 2008. Doctoral Dissertation, The Ohio State University. Accessed April 12, 2021. http://rave.ohiolink.edu/etdc/view?acc_num=osu1228255773.

MLA Handbook (7^th Edition):

Fortner, Sarah K. “The Geochemistry Of Glacier Snow And Melt: The Oregon Cascades And The Taylor Valley, Antarctica.” 2008. Web. 12 Apr 2021.

Vancouver:

Fortner SK. The Geochemistry Of Glacier Snow And Melt: The Oregon Cascades And The Taylor Valley, Antarctica. [Internet] [Doctoral dissertation]. The Ohio State University; 2008. [cited 2021 Apr 12]. Available from: http://rave.ohiolink.edu/etdc/view?acc_num=osu1228255773.

Council of Science Editors:

Fortner SK. The Geochemistry Of Glacier Snow And Melt: The Oregon Cascades And The Taylor Valley, Antarctica. [Doctoral Dissertation]. The Ohio State University; 2008. Available from: http://rave.ohiolink.edu/etdc/view?acc_num=osu1228255773

University of Montana

19. Gillan, Bonnie Jean. Snow Accumulation and Melt Timing at High Elevations in Northwest Montana.

Degree: MS, 2008, University of Montana

URL: https://scholarworks.umt.edu/etd/892

► The sensitivity of snowmelt driven water supply to climate variability and change is difficult to assess in the mountain west, where strong climatic gradients coupled… (more)

Subjects/Keywords: melt model; melt timing; Middle Fork of the Flathead Basin; snow accumulation; temperature variability

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APA (6^th Edition):

Gillan, B. J. (2008). Snow Accumulation and Melt Timing at High Elevations in Northwest Montana. (Masters Thesis). University of Montana. Retrieved from https://scholarworks.umt.edu/etd/892

Chicago Manual of Style (16^th Edition):

Gillan, Bonnie Jean. “Snow Accumulation and Melt Timing at High Elevations in Northwest Montana.” 2008. Masters Thesis, University of Montana. Accessed April 12, 2021. https://scholarworks.umt.edu/etd/892.

MLA Handbook (7^th Edition):

Gillan, Bonnie Jean. “Snow Accumulation and Melt Timing at High Elevations in Northwest Montana.” 2008. Web. 12 Apr 2021.

Vancouver:

Gillan BJ. Snow Accumulation and Melt Timing at High Elevations in Northwest Montana. [Internet] [Masters thesis]. University of Montana; 2008. [cited 2021 Apr 12]. Available from: https://scholarworks.umt.edu/etd/892.

Council of Science Editors:

Gillan BJ. Snow Accumulation and Melt Timing at High Elevations in Northwest Montana. [Masters Thesis]. University of Montana; 2008. Available from: https://scholarworks.umt.edu/etd/892

University of British Columbia

20. Mitchell, Kevin A. Chaotic pattern dynamics on sun-melted snow.

Degree: MS- MSc, Physics, 2008, University of British Columbia

URL: http://hdl.handle.net/2429/2611

► This thesis describes the comparison of time-lapse field observations of suncups on alpine snow with numerical simulations. The simulations consist of solutions to a nonlinear… (more)

Subjects/Keywords: Snow melt; Pattern formation; Dynamical systems; Surface morphology; Chaotic fluctuations; PDEs; Suncups; Nonlinear dynamics

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APA (6^th Edition):

Mitchell, K. A. (2008). Chaotic pattern dynamics on sun-melted snow. (Masters Thesis). University of British Columbia. Retrieved from http://hdl.handle.net/2429/2611

Chicago Manual of Style (16^th Edition):

Mitchell, Kevin A. “Chaotic pattern dynamics on sun-melted snow.” 2008. Masters Thesis, University of British Columbia. Accessed April 12, 2021. http://hdl.handle.net/2429/2611.

MLA Handbook (7^th Edition):

Mitchell, Kevin A. “Chaotic pattern dynamics on sun-melted snow.” 2008. Web. 12 Apr 2021.

Vancouver:

Mitchell KA. Chaotic pattern dynamics on sun-melted snow. [Internet] [Masters thesis]. University of British Columbia; 2008. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/2429/2611.

Council of Science Editors:

Mitchell KA. Chaotic pattern dynamics on sun-melted snow. [Masters Thesis]. University of British Columbia; 2008. Available from: http://hdl.handle.net/2429/2611

ETH Zürich

21. Bründl, Michael. Snow interception and meltwater transport in subalpine forests.

Degree: 1997, ETH Zürich

URL: http://hdl.handle.net/20.500.11850/143349

Subjects/Keywords: SCHNEEVERTEILUNG + SCHNEEVORKOMMEN (METEOROLOGIE); NIEDERSCHLAG/EINFLUSS DER VEGETATION (METEOROLOGIE); WASSERVORRAT AUS SCHNEESCHMELZE (METEOROLOGIE); GEBIRGSWÄLDER (FORSTWIRTSCHAFT); SNOW SURVEY + SNOW DISTRIBUTION + SNOW ABUNDANCE (METEOROLOGY); PRECIPITATION/INFLUENCE OF VEGETATION (METEOROLOGY); WATER SUPPLY FROM SNOW COVER, SNOW MELT (METEOROLOGY); MOUNTAIN FORESTS (FORESTRY); info:eu-repo/classification/ddc/550; Earth sciences

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APA (6^th Edition):

Bründl, M. (1997). Snow interception and meltwater transport in subalpine forests. (Doctoral Dissertation). ETH Zürich. Retrieved from http://hdl.handle.net/20.500.11850/143349

Chicago Manual of Style (16^th Edition):

Bründl, Michael. “Snow interception and meltwater transport in subalpine forests.” 1997. Doctoral Dissertation, ETH Zürich. Accessed April 12, 2021. http://hdl.handle.net/20.500.11850/143349.

MLA Handbook (7^th Edition):

Bründl, Michael. “Snow interception and meltwater transport in subalpine forests.” 1997. Web. 12 Apr 2021.

Vancouver:

Bründl M. Snow interception and meltwater transport in subalpine forests. [Internet] [Doctoral dissertation]. ETH Zürich; 1997. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/20.500.11850/143349.

Council of Science Editors:

Bründl M. Snow interception and meltwater transport in subalpine forests. [Doctoral Dissertation]. ETH Zürich; 1997. Available from: http://hdl.handle.net/20.500.11850/143349

22. Compagnoni, Aldo. Climate change and plant demography in the sagebrush steppe.

Degree: PhD, Wildland Resources, 2013, Utah State University

URL: https://digitalcommons.usu.edu/etd/1748

► We used demographic methods to address one of the main challenges facing ecological science: forecasting the effect of climate change on plant communities. Ecological… (more)

Subjects/Keywords: Bromus tectorum; coexistence theory; Infra-red heters; niche differences; open top chambers; snow melt; Ecology and Evolutionary Biology

…29 3. LOSS OF SNOW CONTRIBUTES TO THE POSITIVE EFFECT OF WARMING ON BROMUS TECTORUM'S… …warming could indirectly favor cheatgrass by decreasing snow cover. Previous research has shown… …snow cover decreases cheatgrass population growth (Griffith and Loik 2010, Concilio et… …al. 2013). Because a few degrees of warming can cause large decreases in snow cover… …x28;2) Does decreased snow cover contribute to the increase of cheatgrass population…

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APA (6^th Edition):

Compagnoni, A. (2013). Climate change and plant demography in the sagebrush steppe. (Doctoral Dissertation). Utah State University. Retrieved from https://digitalcommons.usu.edu/etd/1748

Chicago Manual of Style (16^th Edition):

Compagnoni, Aldo. “Climate change and plant demography in the sagebrush steppe.” 2013. Doctoral Dissertation, Utah State University. Accessed April 12, 2021. https://digitalcommons.usu.edu/etd/1748.

MLA Handbook (7^th Edition):

Compagnoni, Aldo. “Climate change and plant demography in the sagebrush steppe.” 2013. Web. 12 Apr 2021.

Vancouver:

Compagnoni A. Climate change and plant demography in the sagebrush steppe. [Internet] [Doctoral dissertation]. Utah State University; 2013. [cited 2021 Apr 12]. Available from: https://digitalcommons.usu.edu/etd/1748.

Council of Science Editors:

Compagnoni A. Climate change and plant demography in the sagebrush steppe. [Doctoral Dissertation]. Utah State University; 2013. Available from: https://digitalcommons.usu.edu/etd/1748

ETH Zürich

23. Egli, Luca Edoardo. Spatial variability of seasonal snow cover at different scales in the Swiss Alps.

Degree: 2011, ETH Zürich

URL: http://hdl.handle.net/20.500.11850/152954

Subjects/Keywords: FIRNIFICATION + SNOW COVER CHANGES (METEOROLOGY); SNOW COVER MEASUREMENTS (GLACIOLOGY); ABLATION + THERMAL BALANCE OF SNOW COVER (METEOROLOGY); HYDROLOGICAL MODELS + MATHEMATICAL MODELLING IN HYDROLOGY; WATER SUPPLY FROM PRECIPITATION, SNOW COVER AND GLACIERS (HYDROMETEOROLOGY); SNOW MELT (HYDROLOGY); SWISS ALPS; FIRNBILDUNG + SCHNEEDECKENVERÄNDERUNGEN (METEOROLOGIE); SCHNEEDECKENEIGENSCHAFTEN (GLAZIOLOGIE); ABLATION + WÄRMEGLEICHGEWICHT VON SCHNEEDECKEN (METEOROLOGIE); HYDROLOGISCHE MODELLE + HYDROLOGISCHE MODELLRECHNUNG; WASSERVORRAT AUS NIEDERSCHLÄGEN, SCHNEEDECKE UND GLETSCHER (HYDROMETEOROLOGIE); SCHNEESCHMELZE (HYDROLOGIE); SCHWEIZER ALPEN; info:eu-repo/classification/ddc/550; info:eu-repo/classification/ddc/550; Earth sciences; Earth sciences

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APA (6^th Edition):

Egli, L. E. (2011). Spatial variability of seasonal snow cover at different scales in the Swiss Alps. (Doctoral Dissertation). ETH Zürich. Retrieved from http://hdl.handle.net/20.500.11850/152954

Chicago Manual of Style (16^th Edition):

Egli, Luca Edoardo. “Spatial variability of seasonal snow cover at different scales in the Swiss Alps.” 2011. Doctoral Dissertation, ETH Zürich. Accessed April 12, 2021. http://hdl.handle.net/20.500.11850/152954.

MLA Handbook (7^th Edition):

Egli, Luca Edoardo. “Spatial variability of seasonal snow cover at different scales in the Swiss Alps.” 2011. Web. 12 Apr 2021.

Vancouver:

Egli LE. Spatial variability of seasonal snow cover at different scales in the Swiss Alps. [Internet] [Doctoral dissertation]. ETH Zürich; 2011. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/20.500.11850/152954.

Council of Science Editors:

Egli LE. Spatial variability of seasonal snow cover at different scales in the Swiss Alps. [Doctoral Dissertation]. ETH Zürich; 2011. Available from: http://hdl.handle.net/20.500.11850/152954

24. Ibanez, Anatole Vera. Snökyla för is och komfort : Möjligheter att använda snö för komfortkyla och isproduktion vid Rocklundas idrottsarenor.

Degree: Society and Engineering, 2017, Mälardalen University

URL: http://urn.kb.se/resolve?urn=urn:nbn:se:mdh:diva-37481

► The idea of snow cooling in this case is to save snow from winter to summer and to use it for air conditioning and… (more)

▼ The idea of snow cooling in this case is to save snow from winter to summer and to use it for air conditioning and for saving energy in the production of ice in hockey arenas. Today in Sweden, snow power on a large scale is used only on one place, the hospital in Sundsvall. There you’ll find a pond with 70 000 m³ of snow. The melt water in the pond is heated up while cooling down warm air from the hospital, before circulating back to the pond where it regains a low temperature passing through the snow. The idea was to examine the possibility to use such a system in Västerås, at the multiple sports arenas at Rocklunda, partly for air conditioning and partly for ice production. This work was made possible through gathering information on snow storage and on the Sundsvall snow cooling plant, by interviewing people with insight in the Sundsvall hospital and Rocklunda sports arenas and by calculating the electricity consumption, necessary amount of snow and making an LCC-analysis. For air conditioning the melt water would be used like in Sundsvall but for ice production the melt water would be used for condensing the cooling media in the heat pump at a lower temperature then it would do while cooling with air or river water during summer. Annual electricity savings of 120 and 154 MWh for the arenas were made for 2016 and 2017 when using the snow for ice production. For the air conditioning the saving were estimated to around 55 MWh per year. A snow dispatch hatch in one of the hockey arenas made an alternative to a full-scale snow cooling system. Using this hatch for temporal snow power could save up to 62 MWh per year when used for ice production and 38 MWh when used for air conditioning. The estimated costs for construction of said system proved to be too expensive for making a full-scale snow power system a reality. For ice production a storage of 103 000 m³ of snow was needed which made for a result of -57 MSEK in the LCC-analysis. For the air conditioning alone, a storage of 6 000 m³ was needed which made for a result of -4.2 MSEK. The snow dispose hatch, even without the need of snow storage, resulted in -5.9 MSEK for ice production and -1.6 MSEK for air conditioning. With more thoroughly estimations of the investment costs, together with global warming and thus bigger potential for saving energy, this might be a promising investment in the future.

Subjects/Keywords: snow cooling; air condition; ice production; free cooling; nature cooling; cooling machine; melt water; snökyla; komfortkyla; isproduktion; frikyla; naturkyla; kylmaskin; smältvatten; Energy Systems; Energisystem

…snölagring, ’snow power’, ’snow storage’ och ’snow cooling’. 3.2 Beräkningar Beräkningar för…

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APA (6^th Edition):

Ibanez, A. V. (2017). Snökyla för is och komfort : Möjligheter att använda snö för komfortkyla och isproduktion vid Rocklundas idrottsarenor. (Thesis). Mälardalen University. Retrieved from http://urn.kb.se/resolve?urn=urn:nbn:se:mdh:diva-37481

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Chicago Manual of Style (16^th Edition):

Ibanez, Anatole Vera. “Snökyla för is och komfort : Möjligheter att använda snö för komfortkyla och isproduktion vid Rocklundas idrottsarenor.” 2017. Thesis, Mälardalen University. Accessed April 12, 2021. http://urn.kb.se/resolve?urn=urn:nbn:se:mdh:diva-37481.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

MLA Handbook (7^th Edition):

Ibanez, Anatole Vera. “Snökyla för is och komfort : Möjligheter att använda snö för komfortkyla och isproduktion vid Rocklundas idrottsarenor.” 2017. Web. 12 Apr 2021.

Vancouver:

Ibanez AV. Snökyla för is och komfort : Möjligheter att använda snö för komfortkyla och isproduktion vid Rocklundas idrottsarenor. [Internet] [Thesis]. Mälardalen University; 2017. [cited 2021 Apr 12]. Available from: http://urn.kb.se/resolve?urn=urn:nbn:se:mdh:diva-37481.

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

Council of Science Editors:

Ibanez AV. Snökyla för is och komfort : Möjligheter att använda snö för komfortkyla och isproduktion vid Rocklundas idrottsarenor. [Thesis]. Mälardalen University; 2017. Available from: http://urn.kb.se/resolve?urn=urn:nbn:se:mdh:diva-37481

Note: this citation may be lacking information needed for this citation format:
Not specified: Masters Thesis or Doctoral Dissertation

25. Trenouth, William Robert. Highway Stormwater Runoff Quality: Investigation of Improved Operational, Predictive and Treatment Approaches.

Degree: PhD, School of Engineering, 2017, University of Guelph

URL: https://atrium.lib.uoguelph.ca/xmlui/handle/10214/10427

► Highway stormwater runoff from large, multi-lane highways is one of the leading causes of watercourse impairment worldwide. Road runoff frequently carries within it a substantial… (more)

▼ Highway stormwater runoff from large, multi-lane highways is one of the leading causes of watercourse impairment worldwide. Road runoff frequently carries within it a substantial physicochemical pollutant burden which includes sediments, nutrients, petroleum hydrocarbons and heavy metals. In seasonally-cold climates, winter maintenance activities entail the use of road salts, which constitute an additional source of pollutant loading to the road surface. A multi-pronged approach was used to improve the state of practice surrounding highway design, management and the methodological application of treatment approaches. First, a simple road salt application optimization tool was developed in order to help highway maintenance managers utilize a sound, scientifically defensible methodology when making determinations related to the frequency, timing and rate of road salt application. Data from three sites was used to modify the temperature index (TI) model to include sinusoidal variance in the daily melt coefficient, in addition to considerations related to the surficial rerouting of snow as well as the melt point depression caused by salt’s interaction with snow and ice. The second avenue of investigation led to the development of artificial neural networks (ANNs) capable of predicting the runoff concentration statistical distribution parameters for common heavy metals (Cu, Zn, Cr, Pb) and total suspended solid (TSS) event mean concentrations (EMCs) within highway stormwater runoff. The third avenue of investigation focused on the assessment and testing of novel treatment media for the purpose of enhancing existing roadside ditches in environmentally sensitive areas (ESAs). Blast furnace (BF) slag, basic oxygenated furnace (BOF) slag, iron-enriched overburden (IRON) and wood chips (WC) were tested. The long-term removal of Cr, Co, Cu, Pb, Ni and Zn within repacked soil columns ranged from 46-98%. The fourth research effort focused on the development of a methodological framework for designing enhanced roadside ditch systems for application in ESAs. The feasibility of this framework is demonstrated through a field-scale pilot study, complemented by three years of real-time monitoring data. Three different types of impermeable liner – compacted clay (CC), high density polyethylene (HDPE) and linear low-density polyethylene (LLDPE) – were tested for their ability to prevent stormwater egress from the facility. Advisors/Committee Members: Gharabaghi, Bahram (advisor).

Subjects/Keywords: Highway Runoff; Water Quality Prediction; Artificial Neural Networks; Temperature Index; Snow Hydrology; Snowmelt; Salt-induced Melt; Filtration; Heavy Metals; Soil Column

…terms of its ability to estimate snow melt. While not a comprehensive, physically-based… …ultrasonic snow depth sensor, the TI method was found to perform best when the melt coefficient was… …thermally-induced and rain-on snow melt, and these two modes of energy addition to the snowpack… …road salts lowers the melting point of snow, thereby contributing to the generation of melt… …snowpack in order to provide an estimate of snow melt (Walter et al., 2005). However…

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APA (6^th Edition):

Trenouth, W. R. (2017). Highway Stormwater Runoff Quality: Investigation of Improved Operational, Predictive and Treatment Approaches. (Doctoral Dissertation). University of Guelph. Retrieved from https://atrium.lib.uoguelph.ca/xmlui/handle/10214/10427

Chicago Manual of Style (16^th Edition):

Trenouth, William Robert. “Highway Stormwater Runoff Quality: Investigation of Improved Operational, Predictive and Treatment Approaches.” 2017. Doctoral Dissertation, University of Guelph. Accessed April 12, 2021. https://atrium.lib.uoguelph.ca/xmlui/handle/10214/10427.

MLA Handbook (7^th Edition):

Trenouth, William Robert. “Highway Stormwater Runoff Quality: Investigation of Improved Operational, Predictive and Treatment Approaches.” 2017. Web. 12 Apr 2021.

Vancouver:

Trenouth WR. Highway Stormwater Runoff Quality: Investigation of Improved Operational, Predictive and Treatment Approaches. [Internet] [Doctoral dissertation]. University of Guelph; 2017. [cited 2021 Apr 12]. Available from: https://atrium.lib.uoguelph.ca/xmlui/handle/10214/10427.

Council of Science Editors:

Trenouth WR. Highway Stormwater Runoff Quality: Investigation of Improved Operational, Predictive and Treatment Approaches. [Doctoral Dissertation]. University of Guelph; 2017. Available from: https://atrium.lib.uoguelph.ca/xmlui/handle/10214/10427

ETH Zürich

26. Braun, Ludwig Nikolaus. Simulation of snowmelt-runoff in lowland and lower alpine regions of Switzerland.

Degree: 1984, ETH Zürich

URL: http://hdl.handle.net/20.500.11850/138299

Subjects/Keywords: SCHNEESCHMELZE (HYDROLOGIE); ABFLUSSMENGE IN FLÜSSEN (HYDROLOGIE); SCHWEIZ (MITTELEUROPA). SCHWEIZERISCHE EIDGENOSSENSCHAFT; SNOW MELT (HYDROLOGY); RIVER DISCHARGE (HYDROLOGY); SWITZERLAND (CENTRAL EUROPE). SWISS CONFEDERATION; info:eu-repo/classification/ddc/550; Earth sciences

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Braun, L. N. (1984). Simulation of snowmelt-runoff in lowland and lower alpine regions of Switzerland. (Doctoral Dissertation). ETH Zürich. Retrieved from http://hdl.handle.net/20.500.11850/138299

Chicago Manual of Style (16^th Edition):

Braun, Ludwig Nikolaus. “Simulation of snowmelt-runoff in lowland and lower alpine regions of Switzerland.” 1984. Doctoral Dissertation, ETH Zürich. Accessed April 12, 2021. http://hdl.handle.net/20.500.11850/138299.

MLA Handbook (7^th Edition):

Braun, Ludwig Nikolaus. “Simulation of snowmelt-runoff in lowland and lower alpine regions of Switzerland.” 1984. Web. 12 Apr 2021.

Vancouver:

Braun LN. Simulation of snowmelt-runoff in lowland and lower alpine regions of Switzerland. [Internet] [Doctoral dissertation]. ETH Zürich; 1984. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/20.500.11850/138299.

Council of Science Editors:

Braun LN. Simulation of snowmelt-runoff in lowland and lower alpine regions of Switzerland. [Doctoral Dissertation]. ETH Zürich; 1984. Available from: http://hdl.handle.net/20.500.11850/138299

27. Elmabrok, Younis M. Impact of climate change on hydropower production in Sacramento River hydrologic region.

Degree: MS, Civil Engineering (Water Resources Engineering, 2015, California State University – Sacramento

URL: http://hdl.handle.net/10211.3/139844

► California has the most extensive water supply systems in the country. California reservoirs, more than 1000 reservoirs, play a major role in meeting the state???s… (more)

▼ California has the most extensive water supply systems in the country. California reservoirs, more than 1000 reservoirs, play a major role in meeting the state???s water demand (ACWA, 2013). These reservoirs require careful planning and management in order to achieve the optimal balance between different demand sectors. Some of these reservoirs contribute to the state???s power supply through different hydropower plants. Beside some hydraulic and design parameters, the amount of produced hydropower is determined by amount of released water and the available storage. The amount of released water from any reservoir is a function of many factors, such as: climate, precipitation and inflows, demands and environmental requirements downstream. This study examines the implication of Climate Change and Warming on Hydropower production in Sacramento River hydrological region. A simulation model of the study area is built using Water Elevation and Planning System (WEAP). Three main reservoirs for hydropower generation in the study area were included: Shasta Reservoir, Oroville Reservoir, and Folsom Reservoir. Snowpack in west upper slope of the Sierra Nevada Mountains plays a major role in the hydrology of Sacramento River basin. Studies, (Franco et al. 2011) and (Rheinheimer et al. 2014), have shown a possible increase in the California???s air temperature from 1.5 °C to 6 °C, with an expected greater impact on the upper Sierra Nevada Mountains. To assess the impact of such possible increase in air temperature, three warming scenarios were developed. The historical climate data (1964-2014) was collected for each catchment. Then for future projections (2014-2064), three air temperature increase scenarios were developed. The scenarios are 0 °C (no change, for comparison), 2 °C, 4 °C and 6 °C. Air temperature was the only parameter changed, other parameters such as precipitation remained unchanged. The result obtained from the model shows that the increase in air temperature can yield a considerable change in hydropower production. Under 6 °C increase scenario, the reduction in the total hydropower supply over the 50 years (2015-2064) was 9.43% for Shasta, 6.76% Oroville, and 6.44% for Folsom reservoir. Advisors/Committee Members: Merayyan, Saad.

Subjects/Keywords: Snow melt; Climate change; Climate change scenarios; Water evaluation and planning; WEAP; water resources management; Hydropower; Sacramento River Basin; Shasta; Oroville; Folsom; Soil moisture method

…dominated basins (Rheinheimer et al. 2014 ). Most of the snow pack in Sacramento River… …falling as snow. That will also change the seasonal snowmelt patterns, more runoff in winter and… …less in the summer. Such 2 decrease in snow fraction will result in a decrease in the a…

10 more images…

Record Details Similar Records Cite « Share

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Elmabrok, Y. M. (2015). Impact of climate change on hydropower production in Sacramento River hydrologic region. (Masters Thesis). California State University – Sacramento. Retrieved from http://hdl.handle.net/10211.3/139844

Chicago Manual of Style (16^th Edition):

Elmabrok, Younis M. “Impact of climate change on hydropower production in Sacramento River hydrologic region.” 2015. Masters Thesis, California State University – Sacramento. Accessed April 12, 2021. http://hdl.handle.net/10211.3/139844.

MLA Handbook (7^th Edition):

Elmabrok, Younis M. “Impact of climate change on hydropower production in Sacramento River hydrologic region.” 2015. Web. 12 Apr 2021.

Vancouver:

Elmabrok YM. Impact of climate change on hydropower production in Sacramento River hydrologic region. [Internet] [Masters thesis]. California State University – Sacramento; 2015. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/10211.3/139844.

Council of Science Editors:

Elmabrok YM. Impact of climate change on hydropower production in Sacramento River hydrologic region. [Masters Thesis]. California State University – Sacramento; 2015. Available from: http://hdl.handle.net/10211.3/139844

ETH Zürich

28. Leinss, Silvan. Depth, anisotropy, and water equivalent of snow estimated by radar interferometry and polarimetry.

Degree: 2015, ETH Zürich

URL: http://hdl.handle.net/20.500.11850/113806

Subjects/Keywords: RADAR SIGNAL PROCESSING (RADAR ENGINEERING); PRECIPITATIONS + RAINFALL + SNOW (HYDROLOGY); RADARSIGNALVERARBEITUNG (RADARTECHNIK); POLARIZATION, DOUBLE REFRACTION, DISPERSION IN ANISOTROPIC BODIES (OPTICS); SCHNEEDECKE + IHRE TIEFE, TEMPERATUR UND DICHTE (METEOROLOGIE); NIEDERSCHLAG + REGEN + SCHNEE (HYDROLOGIE); RADAR OBSERVATIONS (METEOROLOGY); SNOW COVER, INCLUDING DEPTH, TEMPERATURE AND DENSITY (METEOROLOGY); POLARISATION, DOPPELBRECHUNG, DISPERSION IN ANISOTROPEN KÖRPERN (OPTIK); WATER SUPPLY FROM SNOW COVER, SNOW MELT (METEOROLOGY); RADARBEOBACHTUNGEN (METEOROLOGIE); WASSERVORRAT AUS SCHNEESCHMELZE (METEOROLOGIE); info:eu-repo/classification/ddc/550; info:eu-repo/classification/ddc/550; info:eu-repo/classification/ddc/550; Earth sciences; Earth sciences; Earth sciences

Record Details Similar Records Cite « Share

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Leinss, S. (2015). Depth, anisotropy, and water equivalent of snow estimated by radar interferometry and polarimetry. (Doctoral Dissertation). ETH Zürich. Retrieved from http://hdl.handle.net/20.500.11850/113806

Chicago Manual of Style (16^th Edition):

Leinss, Silvan. “Depth, anisotropy, and water equivalent of snow estimated by radar interferometry and polarimetry.” 2015. Doctoral Dissertation, ETH Zürich. Accessed April 12, 2021. http://hdl.handle.net/20.500.11850/113806.

MLA Handbook (7^th Edition):

Leinss, Silvan. “Depth, anisotropy, and water equivalent of snow estimated by radar interferometry and polarimetry.” 2015. Web. 12 Apr 2021.

Vancouver:

Leinss S. Depth, anisotropy, and water equivalent of snow estimated by radar interferometry and polarimetry. [Internet] [Doctoral dissertation]. ETH Zürich; 2015. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/20.500.11850/113806.

Council of Science Editors:

Leinss S. Depth, anisotropy, and water equivalent of snow estimated by radar interferometry and polarimetry. [Doctoral Dissertation]. ETH Zürich; 2015. Available from: http://hdl.handle.net/20.500.11850/113806

ETH Zürich

29. Moeser, Charles David. The Influence of Forest Canopy Structure on Snow Hydrology.

Degree: 2015, ETH Zürich

URL: http://hdl.handle.net/20.500.11850/155380

Subjects/Keywords: KRONENDACH (FORSTÖKOLOGIE); SCHNEE + EISNADELN + GRAUPELN (METEOROLOGIE); SCHNEESCHMELZE (HYDROLOGIE); NIEDERSCHLAGSMENGE + ISOHYETEN + REGENMENGE (METEOROLOGIE); ABFLUSSMENGE IN FLÜSSEN (HYDROLOGIE); DAVOS, KREIS UND ORT (KANTON GRAUBÜNDEN); FOREST CANOPY (FOREST ECOLOGY); SNOW + SLEET + GRANULAR SNOW + ICE NEEDLES (METEOROLOGY); SNOW MELT (HYDROLOGY); PRECIPITATION AMOUNT + ISOHYETS (METEOROLOGY); RIVER DISCHARGE (HYDROLOGY); DAVOS, SUB-DISTRICT AND LOCALITY (CANTON OF GRISONS); info:eu-repo/classification/ddc/630; info:eu-repo/classification/ddc/550; Agriculture; Earth sciences

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Moeser, C. D. (2015). The Influence of Forest Canopy Structure on Snow Hydrology. (Doctoral Dissertation). ETH Zürich. Retrieved from http://hdl.handle.net/20.500.11850/155380

Chicago Manual of Style (16^th Edition):

Moeser, Charles David. “The Influence of Forest Canopy Structure on Snow Hydrology.” 2015. Doctoral Dissertation, ETH Zürich. Accessed April 12, 2021. http://hdl.handle.net/20.500.11850/155380.

MLA Handbook (7^th Edition):

Moeser, Charles David. “The Influence of Forest Canopy Structure on Snow Hydrology.” 2015. Web. 12 Apr 2021.

Vancouver:

Moeser CD. The Influence of Forest Canopy Structure on Snow Hydrology. [Internet] [Doctoral dissertation]. ETH Zürich; 2015. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/20.500.11850/155380.

Council of Science Editors:

Moeser CD. The Influence of Forest Canopy Structure on Snow Hydrology. [Doctoral Dissertation]. ETH Zürich; 2015. Available from: http://hdl.handle.net/20.500.11850/155380

ETH Zürich

30. Dadić, Ružica. Monitoring and modeling snow accumulation processes in glacierized Alpine basins.

Degree: 2008, ETH Zürich

URL: http://hdl.handle.net/20.500.11850/150891

Subjects/Keywords: SCHNEEVERTEILUNG + SCHNEEVORKOMMEN (METEOROLOGIE); WASSERVORRAT AUS GLETSCHERN (HYDROMETEOROLOGIE); WASSERVORRAT AUS SCHNEESCHMELZE (METEOROLOGIE); KLIMATOLOGIE BESTIMMTER GEBIETE UND ORTE (KLIMATOLOGIE); LAWINEN (METEOROLOGIE); NIEDERSCHLAG-ABFLUSSVERHÄLTNIS (HYDROLOGIE); MASSEN- UND ENERGIEBILANZ VON GLETSCHERN (GLAZIOLOGIE); WASSERHAUSHALT VON EINZUGSGEBIETEN, FLUSSGEBIETEN (HYDROLOGIE); GEBIRGSGLETSCHER (GLAZIOLOGIE); GLAZIOLOGISCHE MODELLEXPERIMENTE (GLAZIOLOGIE); ALPEN (EUROPÄISCHE GEBIRGE); EVOLÈNE (KANTON WALLIS); SNOW SURVEY + SNOW DISTRIBUTION + SNOW ABUNDANCE (METEOROLOGY); WATER SUPPLY FROM GLACIERS (HYDROMETEOROLOGY); WATER SUPPLY FROM SNOW COVER, SNOW MELT (METEOROLOGY); CLIMATOLOGY OF PARTICULAR REGIONS AND PLACES (CLIMATOLOGY); AVALANCHES (METEOROLOGY); RAINFALL-RUNOFF RELATION (HYDROLOGY); MASS AND ENERGY BALANCE OF GLACIERS (GLACIOLOGY); WATER BALANCE OF DRAINAGE BASINS (HYDROLOGY); MOUNTAIN GLACIERS (GLACIOLOGY); GLACIOLOGICAL MODEL EXPERIMENTS (GLACIOLOGY); ALPS (EUROPEAN MOUNTAINS); EVOLÈNE (CANTON OF VALAIS); info:eu-repo/classification/ddc/550; info:eu-repo/classification/ddc/550; Earth sciences; Earth sciences

Record Details Similar Records Cite « Share

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APA · Chicago · MLA · Vancouver · CSE | Export to Zotero / EndNote / Reference Manager

APA (6^th Edition):

Dadić, R. (2008). Monitoring and modeling snow accumulation processes in glacierized Alpine basins. (Doctoral Dissertation). ETH Zürich. Retrieved from http://hdl.handle.net/20.500.11850/150891

Chicago Manual of Style (16^th Edition):

Dadić, Ružica. “Monitoring and modeling snow accumulation processes in glacierized Alpine basins.” 2008. Doctoral Dissertation, ETH Zürich. Accessed April 12, 2021. http://hdl.handle.net/20.500.11850/150891.

MLA Handbook (7^th Edition):

Dadić, Ružica. “Monitoring and modeling snow accumulation processes in glacierized Alpine basins.” 2008. Web. 12 Apr 2021.

Vancouver:

Dadić R. Monitoring and modeling snow accumulation processes in glacierized Alpine basins. [Internet] [Doctoral dissertation]. ETH Zürich; 2008. [cited 2021 Apr 12]. Available from: http://hdl.handle.net/20.500.11850/150891.

Council of Science Editors:

Dadić R. Monitoring and modeling snow accumulation processes in glacierized Alpine basins. [Doctoral Dissertation]. ETH Zürich; 2008. Available from: http://hdl.handle.net/20.500.11850/150891

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