Improving snow albedo processes in WRF/SSiB regional climate model to assess impact of dust and black carbon in snow on surface energy balance and hydrology over western U.S

Autor: Oaida, CM, Xue, Y, Flanner, MG, Skiles, SMK, De Sales, F, Painter, TH

Publikováno v: Oaida, CM; Xue, Y; Flanner, MG; Skiles, SMK; De Sales, F; & Painter, TH. (2015). Improving snow albedo processes in WRF/SSiB regional climate model to assess impact of dust and black carbon in snow on surface energy balance and hydrology over western U.S.. Journal of Geophysical Research, 120(8), 3228-3248. doi: 10.1002/2014JD022444. UCLA: Retrieved from: http://www.escholarship.org/uc/item/5fd9b7kt
Journal of Geophysical Research, vol 120, iss 8

© 2015. American Geophysical Union. All Rights Reserved. Two important factors that control snow albedo are snow grain growth and presence of light-absorbing impurities (aerosols) in snow. However, current regional climate models do not include such

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::0208b5c0bd1b6ababf4187f5aeac9828
http://www.escholarship.org/uc/item/5fd9b7kt