Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Molly E. Tedesche"'
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:
Steven R. Fassnacht, Glenn G. Patterson, Niah B.H. Venable, Mikaela L. Cherry, Anna K.D. Pfohl, Jessica E. Sanow, Molly E. Tedesche
Publikováno v:
Hydrology, Vol 7, Iss 3, p 38 (2020)
Historically, snowpack trends have been assessed using one fixed date to represent peak snow accumulation prior to the onset of melt. Subsequent trend analyses have considered the peak snow water equivalent (SWE), but the date of peak SWE can vary by
Externí odkaz:
https://doaj.org/article/9ab63b1fe15a41af84fd8cde4d6a1f22
Extent Changes in the Perennial Snowfields of Gates of the Arctic National Park and Preserve, Alaska
Publikováno v:
Hydrology, Vol 6, Iss 2, p 53 (2019)
Perennial snowfields in Gates of the Arctic National Park and Preserve (GAAR) in the central Brooks Range of Alaska are a critical component of the cryosphere. They serve as habitat for an array of wildlife, including caribou, a species that is cruci
Externí odkaz:
https://doaj.org/article/548bbaf7807845aab5154066a7e293f4
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.
Perennial snowfields, such as those found in the Brooks Range in Alaska, are critical to alpine and arctic ecosystems, as they influence downslope hydrology, vegetation, geology, and serve as habitat for an array of wildlife, including caribou. Carib
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5cf2151f050542d40876a57f9b699a8
https://doi.org/10.22541/essoar.167591078.86003631/v1
https://doi.org/10.22541/essoar.167591078.86003631/v1
Much of the world’s water resource infrastructure was designed for specific regional snowmelt regimes under the assumption of a stable climate. However, as climate continues to change, this infrastructure is experiencing rapid regime shifts that te
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b842c4f9b01b1c2cc04e22aefa5381a0
https://doi.org/10.22541/essoar.167340718.86199797/v1
https://doi.org/10.22541/essoar.167340718.86199797/v1
Perennial snowfields are a critical part of the alpine ecosystem, serving as habitat for an array of wildlife species, and influencing downslope hydrology, vegetation, geology, and permafrost. In this study, perennial snowfield extents in the Brooks
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9490b9369a370c0065db3cab45199296
https://tc.copernicus.org/preprints/tc-2022-143/
https://tc.copernicus.org/preprints/tc-2022-143/
Publikováno v:
Frontiers of Earth Science. 11:469-481
In high elevation semi-arid rangelands, sagebrush and other shrubs can affect transport and deposition of wind-blown snow, enabling the formation of snowdrifts. Datasets from three field experiments were used to investigate the scales of spatial vari
Autor:
Jessica E. Sanow, Anna K. D. Pfohl, Molly E. Tedesche, Mikaela Cherry, Steven R. Fassnacht, Glenn G. Patterson, Niah B.H. Venable
Publikováno v:
Hydrology
Volume 7
Issue 3
Hydrology, Vol 7, Iss 38, p 38 (2020)
Volume 7
Issue 3
Hydrology, Vol 7, Iss 38, p 38 (2020)
Historically, snowpack trends have been assessed using one fixed date to represent peak snow accumulation prior to the onset of melt. Subsequent trend analyses have considered the peak snow water equivalent (SWE), but the date of peak SWE can vary by