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DOI | 10.3390/rs9090883 |
Quantifying Snow Albedo Radiative Forcing and Its Feedback during 2003-2016 | |
Xiao, Lin; Che, Tao![]() | |
发表日期 | 2017 |
EISSN | 2072-4292 |
卷号 | 9期号:9 |
英文摘要 | Snow albedo feedback is one of the most crucial feedback processes that control equilibrium climate sensitivity, which is a central parameter for better prediction of future climate change. However, persistent large discrepancies and uncertainties are found in snow albedo feedback estimations. Remotely sensed snow cover products, atmospheric reanalysis data and radiative kernel data are used in this study to quantify snow albedo radiative forcing and its feedback on both hemispheric and global scales during 2003-2016. The strongest snow albedo radiative forcing is located north of 30 degrees N, apart from Antarctica. In general, it has large monthly variation and peaks in spring. Snow albedo feedback is estimated to be 0.18 +/- 0.08 W.m(-2).degrees C-1 and 0.04 +/- 0.02 W.m(-2).degrees C-1 on hemispheric and global scales, respectively. Compared to previous studies, this paper focuses specifically on quantifying snow albedo feedback and demonstrates three improvements: (1) used high spatial and temporal resolution satellite-based snow cover data to determine the areas of snow albedo radiative forcing and feedback; (2) provided detailed information for model parameterization by using the results from (1), together with accurate description of snow cover change and constrained snow albedo and snow-free albedo data; and (3) effectively reduced the uncertainty of snow albedo feedback and increased its confidence level through the block bootstrap test. Our results of snow albedo feedback agreed well with other partially observation-based studies and indicate that the 25 Coupled Model Intercomparison Project Phase 5 (CMIP5) models might have overestimated the snow albedo feedback, largely due to the overestimation of surface albedo change between snow-covered and snow-free surface in these models. |
英文关键词 | snow albedo radiative forcing; snow albedo feedback; radiative kernel; remote sensing |
WOS研究方向 | Environmental Sciences & Ecology ; Geology ; Remote Sensing ; Imaging Science & Photographic Technology |
WOS类目 | Environmental Sciences ; Geosciences, Multidisciplinary ; Remote Sensing ; Imaging Science & Photographic Technology |
WOS关键词 | CLIMATE FEEDBACKS ; KERNEL TECHNIQUE ; MODEL ; CIRCULATION ; COVER ; CLOUD ; ICE ; AMPLIFICATION ; VARIABILITY ; SENSITIVITY |
WOS记录号 | WOS:000414138700013 |
来源期刊 | REMOTE SENSING
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来源机构 | 中国科学院西北生态环境资源研究院 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/241048 |
作者单位 | [Xiao, Lin; Che, Tao; Dai, Liyun] Chinese Acad Sci, Key Lab Remote Sensing Gansu Prov, Heihe Remote Sensing Expt Res Stn, Northwest Inst Ecoenvironm & Resources, Lanzhou 730000, Gansu, Peoples R China; [Xiao, Lin] Univ Chinese Acad Sci, Beijing 100049, Peoples R China; [Che, Tao] Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing 100101, Peoples R China; [Chen, Linling] Nansen Environm & Remote Sensing Ctr, N-5006 Bergen, Norway; [Xie, Hongjie] Univ Texas San Antonio, Lab Remote Sensing & Geoinformat, Dept Geol Sci, 1 UTSA Circle, San Antonio, TX 78249 USA; [Dai, Liyun] Jiangsu Ctr Collaborat Innovat Geog Informat Reso, Nanjing 210023, Jiangsu, Peoples R China |
推荐引用方式 GB/T 7714 | Xiao, Lin,Che, Tao,Chen, Linling,et al. Quantifying Snow Albedo Radiative Forcing and Its Feedback during 2003-2016[J]. 中国科学院西北生态环境资源研究院,2017,9(9). |
APA | Xiao, Lin,Che, Tao,Chen, Linling,Xie, Hongjie,&Dai, Liyun.(2017).Quantifying Snow Albedo Radiative Forcing and Its Feedback during 2003-2016.REMOTE SENSING,9(9). |
MLA | Xiao, Lin,et al."Quantifying Snow Albedo Radiative Forcing and Its Feedback during 2003-2016".REMOTE SENSING 9.9(2017). |
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