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DOI | 10.1175/JCLI-D-18-0720.1 |
The Dominant Role of Snow/Ice Albedo Feedback Strengthened by Black Carbon in the Enhanced Warming over the Himalayas | |
Ma, Jieru1; Zhang, Tinghan1; Guan, Xiaodan1; Hu, Xiaoming2,3; Duan, Anmin4; Liu, Jingchen1 | |
2019-09-01 | |
发表期刊 | JOURNAL OF CLIMATE |
ISSN | 0894-8755 |
EISSN | 1520-0442 |
出版年 | 2019 |
卷号 | 32期号:18页码:5883-5899 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
英文摘要 | An obvious warming trend in winter over the Tibetan Plateau (TP) in the recent decades has been widely discussed, with studies emphasizing the dominant effects of local radiative factors, including those due to black carbon (BC). The Himalayas are one of the largest snowpack- and ice-covered regions in the TP, and an ideal area to investigate local radiative effects on climate change. In this study, the coupled climate feedback response analysis method (CFRAM) is applied to quantify the magnitude of warming over the Himalayas induced by different external forcing factors and climate feedback processes. The results show that snow/ice albedo feedback (SAF) resulted in a warming of approximately 2.6C and was the primary contributor to enhanced warming over the Himalayas in recent decades. This warming was much greater than the warming induced by dynamic and other radiative factors. In particular, the strong radiative effects of BC on the warming over the Himalayas are identified by comparing control and BC-perturbed experiments of the Community Earth System Model (CESM). As a result of strong BC effects on the Himalayas, evaporation and reduced precipitation were strengthened, accounting for local drying and land degradation, which intensified warming. These results suggest that more investigations on the local radiative effects on the climate and ecosystem are needed, especially in the high-altitude cryosphere. |
英文关键词 | Aerosols Albedo Climate change Feedback Snow cover Surface temperature |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000481422200003 |
WOS关键词 | PROCESS-BASED DECOMPOSITION ; TIBETAN PLATEAU ; CLIMATE-CHANGE ; ALTITUDINAL DEPENDENCE ; GROUND MEASUREMENTS ; REGIONAL CLIMATE ; SUMMER MONSOON ; MIXING STATE ; GRAIN SHAPE ; HEAT FLUXES |
WOS类目 | Meteorology & Atmospheric Sciences |
WOS研究方向 | Meteorology & Atmospheric Sciences |
引用统计 | |
文献类型 | 期刊论文 |
条目标识符 | http://119.78.100.173/C666/handle/2XK7JSWQ/186775 |
专题 | 气候变化 |
作者单位 | 1.Lanzhou Univ, Key Lab Semiarid Climate Change, Minist Educ, Coll Atmospher Sci, Lanzhou, Gansu, Peoples R China; 2.Sun Yat Sen Univ, Sch Atmospher Sci, Guangzhou, Guangdong, Peoples R China; 3.Sun Yat Sen Univ, Guangdong Prov Key Lab Climate Change & Nat Disas, Guangzhou, Guangdong, Peoples R China; 4.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modelling Atmospher Sci & Geo, Beijing, Peoples R China |
推荐引用方式 GB/T 7714 | Ma, Jieru,Zhang, Tinghan,Guan, Xiaodan,et al. The Dominant Role of Snow/Ice Albedo Feedback Strengthened by Black Carbon in the Enhanced Warming over the Himalayas[J]. JOURNAL OF CLIMATE,2019,32(18):5883-5899. |
APA | Ma, Jieru,Zhang, Tinghan,Guan, Xiaodan,Hu, Xiaoming,Duan, Anmin,&Liu, Jingchen.(2019).The Dominant Role of Snow/Ice Albedo Feedback Strengthened by Black Carbon in the Enhanced Warming over the Himalayas.JOURNAL OF CLIMATE,32(18),5883-5899. |
MLA | Ma, Jieru,et al."The Dominant Role of Snow/Ice Albedo Feedback Strengthened by Black Carbon in the Enhanced Warming over the Himalayas".JOURNAL OF CLIMATE 32.18(2019):5883-5899. |
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