The Effect of Atmospheric Transmissivity on Model and Observational Estimates of the Sea Ice Albedo Feedback
The Effect of Atmospheric Transmissivity on Model and Observational Estimates of the Sea Ice Albedo Feedback
复制标题
大气透过率对海冰反照率反馈模式和观测估计的影响
DOI：
10.1175/jcli-d-19-0674.1
复制
发表时间：
2020-07
影响因子：
4.9
通讯作者：
A. Donohoe;E. Blanchard‐Wrigglesworth;A. Schweiger;P. Rasch
中科院分区：
文献类型：
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作者：
A. Donohoe;E. Blanchard‐Wrigglesworth;A. Schweiger;P. Rasch
海冰-冰量反馈（SIAF）是海冰敏感度（IS）和辐射敏感度（IS）的乘积。
AbstractThe sea ice-albedo feedback (SIAF) is the product of the ice sensitivity (IS), that is, how much the surface albedo in sea ice regions changes as the planet warms, and the radiative sensiti...