Zobrazeno 1 - 10
of 13
pro vyhledávání: '"Anna K. D. Pfohl"'
Publikováno v:
Water, Vol 16, Iss 12, p 1665 (2024)
After peak snowmelt, baseflow is the primary contributor to streamflow in snow-dominated watersheds. These low flows provide important water for municipal, agricultural, and recreational purposes once peak flows have been allocated. This study examin
Externí odkaz:
https://doaj.org/article/efb8f6bee5a741e4a34a9b4da7a7750e
Autor:
Steven R. Fassnacht, Kazuyoshi Suzuki, Jessica E. Sanow, Graham A. Sexstone, Anna K. D. Pfohl, Molly E. Tedesche, Bradley M. Simms, Eric S. Thomas
Publikováno v:
Water, Vol 15, Iss 12, p 2196 (2023)
The snow surface is at the interface between the atmosphere and Earth. The surface of the snowpack changes due to its interaction with precipitation, wind, humidity, short- and long-wave radiation, underlying terrain characteristics, and land cover.
Externí odkaz:
https://doaj.org/article/fd3393adb97648218e0e5becc408c1bd
Autor:
Anna K. D. Pfohl, Steven R. Fassnacht
Publikováno v:
Hydrology, Vol 10, Iss 4, p 75 (2023)
Current streamflow timing metrics, such as the center of volume, or COV, use flow days, which are days at which a specific total streamflow volume, such as 50% for COV, has passed a given point. These metrics have been used as indicators for changes
Externí odkaz:
https://doaj.org/article/3b823213448c4c81b0f255487e638deb
Autor:
Steven R. Fassnacht, Caroline R. Duncan, Anna K. D. Pfohl, Ryan W. Webb, Jeffrey E. Derry, William E. Sanford, Danielle C. Reimanis, Lenka G. Doskocil
Publikováno v:
Hydrology, Vol 9, Iss 3, p 47 (2022)
The presence of dust on the snowpack accelerates snowmelt. This has been observed through snowpack and hydrometeorological measurements at a small study watershed in southwestern Colorado. For a 13-year period, we quantified the annual dust-enhanced
Externí odkaz:
https://doaj.org/article/38c5aa14429a40e192cb14edd4776239
Autor:
Isaac J. Y. Schrock, Steven R. Fassnacht, Antonio-Juan Collados-Lara, William E. Sanford, Anna K. D. Pfohl, Enrique Morán-Tejeda
Publikováno v:
Hydrology, Vol 8, Iss 3, p 124 (2021)
The spatial characteristics and patterns of snow accumulation and ablation inform the amount of water stored and subsequently available for runoff and the timing of snowmelt. This paper characterizes the snow accumulation phase to investigate the spa
Externí odkaz:
https://doaj.org/article/54a8b6dd0b9747d7b766cf7f4d06043e
Autor:
Steven R. Fassnacht, Arren Mendezona Allegretti, Niah B. H. Venable, María E. Fernández-Giménez, Sukh Tumenjargal, Martin Kappas, Melinda J. Laituri, Batjav Batbuyan, Anna K. D. Pfohl
Publikováno v:
Hydrology, Vol 5, Iss 3, p 46 (2018)
Across the globe, station-based meteorological data are analyzed to estimate the rate of change in precipitation. However, in sparsely populated regions, like Mongolia, stations are few and far between, leaving significant gaps in station-derived pre
Externí odkaz:
https://doaj.org/article/2cb373dd17b74c20a5887dd16e316afc
Autor:
Thomas, Steven R. Fassnacht, Kazuyoshi Suzuki, Jessica E. Sanow, Graham A. Sexstone, Anna K. D. Pfohl, Molly E. Tedesche, Bradley M. Simms, Eric S.
Publikováno v:
Water; Volume 15; Issue 12; Pages: 2196
The snow surface is at the interface between the atmosphere and Earth. The surface of the snowpack changes due to its interaction with precipitation, wind, humidity, short- and long-wave radiation, underlying terrain characteristics, and land cover.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=multidiscipl::b0ef3e69f5441ad32a84c4d58f585946
Autor:
Steven R. Fassnacht, Antonio-Juan Collados-Lara, Anna K. D. Pfohl, Isaac J. Y. Schrock, Enrique Morán-Tejeda, William E. Sanford
Publikováno v:
Hydrology, Vol 8, Iss 124, p 124 (2021)
Hydrology
Volume 8
Issue 3
Hydrology
Volume 8
Issue 3
The spatial characteristics and patterns of snow accumulation and ablation inform the amount of water stored and subsequently available for runoff and the timing of snowmelt. This paper characterizes the snow accumulation phase to investigate the spa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1382b6f28b30906b5970c4ffdd7a6cb1
https://www.mdpi.com/2306-5338/8/3/124
https://www.mdpi.com/2306-5338/8/3/124
Autor:
Antonio-Juan Collados-Lara, Eulogio Pardo-Igúzquiza, Anna K. D. Pfohl, Kira Puntenney-Desmond, Enrique Morán-Tejeda, Steven R. Fassnacht, David Pulido-Velazquez, Niah B.H. Venable
Publikováno v:
International Journal of Climatology. 41
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f77d48a1b75acd7f99a8532a9a1420a
https://doi.org/10.1002/joc.6778
https://doi.org/10.1002/joc.6778
Autor:
Stephanie K. Kampf, C. Ma, A. N. Weber, Martin Kappas, Anna K. D. Pfohl, Steven R. Fassnacht, Juan I. López-Moreno
Publikováno v:
Frontiers of Earth Science. 11:505-514
Understanding the rate of snowmelt helps inform how water stored as snow will transform into streamflow. Data from 87 snow telemetry (SNOTEL) stations across the Southern Rocky Mountains were used to estimate spatio-temporal melt factors. Decreases i
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ae81bbaffc34f114f2db9c5fdad4c2c5
https://doi.org/10.1007/s11707-017-0641-4
https://doi.org/10.1007/s11707-017-0641-4