Observation-Based Longwave Cloud Radiative Kernels Derived from the A-Train

被引:32
作者
Yue, Qing [1 ]
Kahn, Brian H. [1 ]
Fetzer, Eric J. [1 ]
Schreier, Mathias [1 ]
Wong, Sun [1 ]
Chen, Xiuhong [2 ]
Huang, Xianglei [2 ]
机构
[1] CALTECH, Jet Prop Lab, 4800 Oak Grove Dr,Mail Stop 233-302C, Pasadena, CA 91109 USA
[2] Univ Michigan, Dept Atmospher Ocean & Space Sci, Ann Arbor, MI 48109 USA
基金
美国国家航空航天局;
关键词
CLIMATE FEEDBACKS; MODIS; INSTRUMENT; SATELLITE; MISSION; SYSTEM; ISCCP; ATMOSPHERES; DIMENSION; PRODUCTS;
D O I
10.1175/JCLI-D-15-0257.1
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The authors present a new method to derive both the broadband and spectral longwave observation-based cloud radiative kernels (CRKs) using cloud radiative forcing (CRF) and cloud fraction (CF) for different cloud types using multisensor A-Train observations and MERRA data collocated on the pixel scale. Both observation-based CRKs and model-based CRKs derived from the Fu-Liou radiative transfer model are shown. Good agreement between observation-and model-derived CRKs is found for optically thick clouds. For optically thin clouds, the observation-based CRKs show a larger radiative sensitivity at TOA to cloud-cover change than model-derived CRKs. Four types of possible uncertainties in the observed CRKs are investigated: 1) uncertainties in Moderate Resolution Imaging Spectroradiometer cloud properties, 2) the contributions of clear-sky changes to the CRF, 3) the assumptions regarding clear-sky thresholds in the observations, and 4) the assumption of a single-layer cloud. The observation-based CRKs show the TOA radiative sensitivity of cloud types to unit cloud fraction change as observed by the A-Train. Therefore, a combination of observation-based CRKs with cloud changes observed by these instruments over time will provide an estimate of the short-term cloud feedback by maintaining consistency between CRKs and cloud responses to climate variability.
引用
收藏
页码:2023 / 2040
页数:18
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