期刊
JOURNAL OF CLIMATE
卷 25, 期 8, 页码 2578-2582出版社
AMER METEOROLOGICAL SOC
DOI: 10.1175/JCLI-D-11-00721.1
关键词
-
资金
- National Science Foundation [ATM-0904092]
- Div Atmospheric & Geospace Sciences
- Directorate For Geosciences [0904092] Funding Source: National Science Foundation
An approach to climate change feedback analysis is described in which tropospheric relative humidity replaces specific humidity as the state variable that, along with the temperature structure, surface albedos, and clouds, controls the magnitude of the response of global mean surface temperature to a radiative forcing. Despite being simply a regrouping of terms in the feedback analysis, this alternative perspective has the benefit of removing most of the pervasive cancellation between water and lapse-rate feedbacks seen in models. As a consequence, the individual feedbacks have less scatter than in the traditional formulation. The role of cloud feedbacks in controlling climate sensitivity is also reflected more clearly in the new formulation.
作者
我是这篇论文的作者
点击您的名字以认领此论文并将其添加到您的个人资料中。
推荐
暂无数据