The spectral dimension of longwave feedback in the CMIP3 and CMIP5 experiments

被引:18
|
作者
Huang, Xianglei [1 ]
Chen, Xiuhong [1 ]
Soden, Brian J. [2 ]
Liu, Xu [3 ]
机构
[1] Univ Michigan, Dept Atmospher Ocean & Space Sci, Ann Arbor, MI 48109 USA
[2] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Miami, FL 33149 USA
[3] NASA, Langley Res Ctr, Hampton, VA 23665 USA
关键词
radiative feedback; spectral feedback; lapse rate feedback; water vapor feedback; RADIATIVE KERNEL TECHNIQUE; CLIMATE FEEDBACKS; CLOUD FEEDBACK;
D O I
10.1002/2014GL061938
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Radiative feedback is normally discussed in terms of the change of broadband flux. Yet it has an intrinsic dimension of spectrum. A set of longwave (LW) spectral radiative kernels (SRKs) is constructed and validated in a similar way as the broadband radiative kernel. The LW broadband feedback derived using this SRK are consistent with those from the broadband radiative kernels. As an application, the SRK is applied to 12 general circulation models (GCMs) from the Coupled Model Intercomparison Project Phase 3 and 12 GCMs from the Coupled Model Intercomparison Project Phase 5 simulations to derive the spectrally resolved Planck, lapse rate, and LW water vapor feedback. The spectral details of the Planck feedback from different GCMs are essentially the same, but the lapse rate and LW water vapor feedback do reveal spectrally dependent difference among GCMs. Spatial distributions of the feedback at different spectral regions are also discussed. The spectral feedback analysis provides us another dimension to understand and evaluate the modeled radiative feedback.
引用
收藏
页码:7830 / 7837
页数:8
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