Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Tyler S. Harrington"'
Publikováno v:
npj Climate and Atmospheric Science, Vol 4, Iss 1, Pp 1-14 (2021)
Abstract Sea ice melt and ocean heat accumulation in the Arctic are strongly influenced by the presence of atmospheric water vapor during summer. While the relationships between water vapor concentration, radiation, and surface energy fluxes in the A
Externí odkaz:
https://doaj.org/article/c24a299418bb430ea4764ba0469ba10d
Publikováno v:
Environmental Research: Climate, Vol 2, Iss 4, p 045010 (2023)
Over the course of a season, a location’s precipitation is comprised of moisture sourced from a diverse set of geographic regions. Seasonal extremes in precipitation may arise from changes in the contribution of one or several of these sources. Her
Externí odkaz:
https://doaj.org/article/97ded4af443949d8a2a6e23d0d864c59
Land surface evapotranspiration (ET) is a major source of moisture for the global hydrologic cycle. Though the influence of the land surface is well documented, moisture tracking analysis has often relied on offline tracking approaches that require s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b591f903dbdc8ae8ef4deee83c320607
https://doi.org/10.5194/hess-2021-284
https://doi.org/10.5194/hess-2021-284
Publikováno v:
npj Climate and Atmospheric Science, Vol 4, Iss 1, Pp 1-14 (2021)
Sea ice melt and ocean heat accumulation in the Arctic are strongly influenced by the presence of atmospheric water vapor during summer. While the relationships between water vapor concentration, radiation, and surface energy fluxes in the Arctic are
Land surface moisture plays a crucial role in precipitation patterns across the globe. Evapotranspiration (the combination of ground evaporation (E), canopy evaporation (I), and transpiration (T)) from the land surface can influence precipitation thr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4979d9b1561e7c5b0ba90d78cbc5aa69
https://doi.org/10.5194/egusphere-egu21-8856
https://doi.org/10.5194/egusphere-egu21-8856