Global S&T Development Trend Analysis Platform of Resources and Environment
DOI | 10.1002/joc.6133 |
Atmospheric heat sinks over the western Tibetan Plateau associated with snow depth in late spring | |
Xiao, Zhixiang1,2; Duan, Anmin2,3; Wang, Ziqian4,5,6 | |
2019-11-15 | |
发表期刊 | INTERNATIONAL JOURNAL OF CLIMATOLOGY |
ISSN | 0899-8418 |
EISSN | 1097-0088 |
出版年 | 2019 |
卷号 | 39期号:13页码:5170-5180 |
文章类型 | Article |
语种 | 英语 |
国家 | Peoples R China |
英文摘要 | The atmospheric heat source/sink (AHS) and snow cover/depth over the Tibetan Plateau (TP) in late spring play important roles in modulating the evolution of Asian summer monsoons. However, quantitative estimation of the AHS over the TP is still a large challenge because of limited observational data. In this work, both data analyses and numerical simulations from the Weather Research and Forecasting model with an updated daily snow-depth data set are conducted to explore the intrinsic connection between the AHS and snow depth over the TP in May. Data analyses indicate that only a weak negative relationship exists between snow depth and the AHS over the western TP. On the other hand, despite the overall consistency in the spatial pattern of the AHS between the reanalysis data sets and the Weather Research and Forecasting model, a strong cooling effect (about -14.4W/m(2)) appears over the western TP (32 degrees-40 degrees N, 70 degrees-78 degrees E) and the Nyenchen Tanglha Mountains in the simulation, where the altitude is above 4,000m with thick snow cover. This characteristic is opposite to that observed in reanalysis data sets. Further analysis indicates that the underestimated atmospheric net longwave radiative cooling effect that is associated with snow depth may exaggerate the atmospheric heat source in current reanalysis data sets. Large uncertainties in the AHS still exist in current state-of-the-art reanalysis data sets, especially over the regions of the TP covered by snow. |
英文关键词 | atmospheric heat source sink snow depth Tibetan plateau WRF simulation |
领域 | 气候变化 |
收录类别 | SCI-E |
WOS记录号 | WOS:000492795100016 |
WOS关键词 | INTERANNUAL VARIABILITY ; SENSIBLE HEAT ; SUMMER RAINFALL ; REANALYSIS ; PRECIPITATION ; CIRCULATION ; MONSOON ; FLUX ; ASIA |
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/225439 |
专题 | 环境与发展全球科技态势 |
作者单位 | 1.Guangxi Meteorol Observ, Nanning, Peoples R China; 2.Chinese Acad Sci, Inst Atmospher Phys, State Key Lab Numer Modeling Atmospher Sci & Geop, Beijing, Peoples R China; 3.Chinese Acad Sci, Ctr Excellence Tibetan Plateau Earth Sci, Beijing, Peoples R China; 4.Sun Yat Sen Univ, Sch Atmospher Sci, Guangzhou, Guangdong, Peoples R China; 5.Sun Yat Sen Univ, Guangdong Prov Key Lab Climate Change & Nat Disas, Guangzhou, Guangdong, Peoples R China; 6.Southern Marine Sci & Engn Guangdong Lab Zhuhai, Zhuhai, Peoples R China |
推荐引用方式 GB/T 7714 | Xiao, Zhixiang,Duan, Anmin,Wang, Ziqian. Atmospheric heat sinks over the western Tibetan Plateau associated with snow depth in late spring[J]. INTERNATIONAL JOURNAL OF CLIMATOLOGY,2019,39(13):5170-5180. |
APA | Xiao, Zhixiang,Duan, Anmin,&Wang, Ziqian.(2019).Atmospheric heat sinks over the western Tibetan Plateau associated with snow depth in late spring.INTERNATIONAL JOURNAL OF CLIMATOLOGY,39(13),5170-5180. |
MLA | Xiao, Zhixiang,et al."Atmospheric heat sinks over the western Tibetan Plateau associated with snow depth in late spring".INTERNATIONAL JOURNAL OF CLIMATOLOGY 39.13(2019):5170-5180. |
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