Zobrazeno 1 - 10
of 857
pro vyhledávání: '"J, Shellito"'
Publikováno v:
Hydrology and Earth System Sciences, Vol 25, Pp 4185-4208 (2021)
Accurate estimation of terrestrial water storage (TWS) at a high spatiotemporal resolution is important for reliable assessments of regional water resources and climate variability. Individual components of TWS include soil moisture, snow, groundwate
Externí odkaz:
https://doaj.org/article/955b3b841a3f4cf1af53cd603f3f00a3
Publikováno v:
Hydrology and Earth System Sciences, Vol 22, Pp 1649-1663 (2018)
Drydown periods that follow precipitation events provide an opportunity to assess controls on soil evaporation on a continental scale. We use SMAP (Soil Moisture Active Passive) observations and Noah simulations from drydown periods to quantify th
Externí odkaz:
https://doaj.org/article/23c1c9c0018541a689e421e88cb0a634
Akademický článek
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Autor:
John H. Prueger, David D. Bosch, Chandra Holifield Collins, Mark S. Seyfried, Stan Livingston, Michael H. Cosh, Joseph A. Santanello, Patricia Lawston-Parker, John D. Bolten, Patrick J. Starks, P. J. Shellito, Sujay V. Kumar
Publikováno v:
Journal of Hydrometeorology. 21:2041-2060
The utility of hydrologic land surface models (LSMs) can be enhanced by using information from observational platforms, but mismatches between the two are common. This study assesses the degree to which model agreement with observations is affected b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0331f0443c43a80760bff0a251f77519
https://doi.org/10.1175/jhm-d-19-0280.1
https://doi.org/10.1175/jhm-d-19-0280.1
Accurate estimation of terrestrial water storage (TWS) at a meaningful spatiotemporal resolution is important for reliable assessments of regional water resources and climate variability. Individual components of TWS include soil moisture, snow, grou
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1bfc5b44c7b9e7a3cb40d08979fdfa78
https://doi.org/10.5194/hess-2020-665
https://doi.org/10.5194/hess-2020-665
Autor:
Cindy J. Shellito
Publikováno v:
Journal of College Science Teaching.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d15ea867ededd58fd92570e61a586525
https://doi.org/10.2505/4/jcst20_049_03_10
https://doi.org/10.2505/4/jcst20_049_03_10
Publikováno v:
Hydrology and Earth System Sciences, Vol 22, Pp 1649-1663 (2018)
Drydown periods that follow precipitation events provide an opportunity to assess controls on soil evaporation on a continental scale. We use SMAP (Soil Moisture Active Passive) observations and Noah simulations from drydown periods to quantify the r
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5d9a5ca0202b20023b48a90a53f398e0
https://www.hydrol-earth-syst-sci.net/22/1649/2018/hess-22-1649-2018.pdf
https://www.hydrol-earth-syst-sci.net/22/1649/2018/hess-22-1649-2018.pdf
Publikováno v:
Journal of Hydrometeorology. 17:2275-2292
Soil hydraulic properties (SHPs) control infiltration and redistribution of moisture in a soil column. The Noah land surface model (LSM) default simulation selects SHPs according to a location’s mapped soil texture class. SHPs are instead estimated
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce06f9498e4fcf7b4bcc13a86bfe87c0
https://doi.org/10.1175/jhm-d-15-0153.1
https://doi.org/10.1175/jhm-d-15-0153.1
Autor:
Peter J. Shellito, Eric E. Small
Drydown periods that follow precipitation events provide an opportunity to assess the mechanisms by which soil moisture dissipates from the land surface. We use SMAP (Soil Moisture Active Passive) observations and Noah simulations from drydown period
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ab2e0c868dc41864e8129dcb1228aea4
https://doi.org/10.5194/hess-2017-338
https://doi.org/10.5194/hess-2017-338