Zobrazeno 1 - 10
of 27
pro vyhledávání: '"Russell J. Qualls"'
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-8 (2024)
Abstract Evaporation rates and land surface temperatures can be modified by planned water availability as well as land use and land cover changes. In general, a higher evaporation rate via its associated latent heat flux yields a cooler surface. Here
Externí odkaz:
https://doaj.org/article/73bf0b66e3e04eb0a2e6228e622d3274
Autor:
Richard D. Crago, Russell J. Qualls
Publikováno v:
Water Resources Research. 57
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8d79da3b1eb8951ce376bb88d043bda0
https://doi.org/10.1029/2020wr028299
https://doi.org/10.1029/2020wr028299
Autor:
Craig D. Woodruff, Russell J. Qualls
Publikováno v:
Water Resources Research. 55:6869-6885
Snow acts as a vital source of water especially in areas where streamflow relies on snowmelt. The spatiotemporal pattern of snow cover has tremendous value for snowmelt modeling. Instantaneous snow extent can be observed by remote sensing. Cloud cove
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b11d7a502b41abf98e26cb3f02226b03
https://doi.org/10.1029/2018wr024546
https://doi.org/10.1029/2018wr024546
Publikováno v:
Journal of Geophysical Research: Atmospheres. 126
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a733cd2e50c62c5f83b9be85f6e7e58
https://doi.org/10.1029/2021jd034685
https://doi.org/10.1029/2021jd034685
Autor:
Russell J. Qualls, Richard D. Crago
Publikováno v:
Water Resources Research. 56
Potential (wet surface) evaporation is the basis for many methods to estimate actual evaporation. Penman's (1948, https://doi.org/10.1098/rspa.1948.0037) combination of energy budget with mass and energy transfer equations can be depicted on temperat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15da85ec747bea95b5d64e0cc4a13d0e
https://doi.org/10.1029/2019wr026766
https://doi.org/10.1029/2019wr026766
Publikováno v:
Journal of Geophysical Research: Atmospheres. 122:264-278
An important scaling consideration is introduced into the formulation of the complementary relationship (CR) of land surface evapotranspiration (ET) by specifying the maximum possible evaporation rate (Epmax) of a small water body (or wet patch) as a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e25e8c1ae9dbd97e27afe6fd04e48e2b
https://doi.org/10.1002/2016jd025611
https://doi.org/10.1002/2016jd025611
Publikováno v:
Water Resources Research. 52:8461-8471
Recent research into the complementary relationship (CR) between actual and apparent potential evaporation has resulted in numerous alternative forms for the CR. Inspired by Brutsaert [2015], who derived a general CR in the form y=function(x), where
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c830a1149adb69b0e73a3c8b411a91a7
https://doi.org/10.1002/2016wr019753
https://doi.org/10.1002/2016wr019753
Publikováno v:
Journal of Hydrology. 540:914-922
The original and revised versions of the generalized complementary relationship (GCR) of evaporation (ET) were tested with six-digit Hydrologic Unit Code (HUC6) level long-term (1981–2010) water-balance data (sample size of 334). The two versions o
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81e374115477f8b173b96c49a95bc177
https://doi.org/10.1016/j.jhydrol.2016.07.001
https://doi.org/10.1016/j.jhydrol.2016.07.001
Autor:
Richard D. Crago, Russell J. Qualls
Publikováno v:
Water Resources Research. 50:3396-3408
Land surface temperature (LST) plays a key role in governing the land surface energy budget, and measurements or estimates of LST are an integral part of many land surface models and methods to estimate land surface sensible heat (H) and latent heat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::983306847ca29450ba1812d198def8cf
https://doi.org/10.1002/2013wr015223
https://doi.org/10.1002/2013wr015223