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DOI10.1029/2020JD033998
Monsoon Clouds Control the Summer Surface Energy Balance on East Rongbuk Glacier (6,523 m Above Sea Level), the Northern of Mt. Qomolangma (Everest)
Liu, Weigang; Zhang, Dongqi; Qin, Xiang; van den Broeke, Michiel R.; Jiang, Youyan; Yang, Diyi; Ding, Minghu
通讯作者Zhang, DQ ; Ding, MH (通讯作者),Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing, Peoples R China. ; Zhang, DQ ; Ding, MH (通讯作者),Chinese Acad Meteorol Sci, Inst Tibetan Plateau & Polar Meteorol, Beijing, Peoples R China. ; Ding, MH (通讯作者),Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Lanzhou, Peoples R China.
发表日期2021
ISSN2169-897X
EISSN2169-8996
卷号126期号:8
英文摘要To identify the atmospheric controls of the summertime glacier surface energy balance in the Himalayas, in situ meteorological data collected at 6,523 m above sea level during May-July 2005 were obtained and analyzed. Our results showed that net shortwave radiation (103 W m(-2)) and turbulent sensible heat flux (12 W m(-2)) acted as energy sources, and net longwave radiation (-62 W m(-2)) and turbulent latent heat flux (-20 W m(-2)) represented heat sinks. Cloud cover controlled the summer surface energy balance. During the active period of the South Asian Summer Monsoon, the frequent cloud coverage increased the incoming longwave radiation more than it decreased the incident solar radiation. Intensification (weakening) of the South Asian Summer Monsoon strengthened (suppressed) surface melting. The melt energy measured during the nonmonsoon period was small due to the energy consumption associated with glacier volume warming, energy loss from sublimation, and large heat loss through net longwave radiation due to the low amount of incoming longwave radiation caused by the low cloudiness. The comparison of glacier surface energy balances on the Tibetan Plateau shows that on continental glaciers, net radiation is lower and accounts for a smaller contribution to energy sources, and the dominant energy sinks are sublimation and evaporation, rather than melting, which is the primary energy sink for maritime/subcontinental glaciers. This implies an important spatial variability in glacial sensitivity to different climatic conditions on the Tibetan Plateau. Key Points Based on in situ data obtained at 6,523 m above sea level, the glacier surface energy balance and its atmospheric controls are examined Clouds governed the surface energy balance by decreasing the incident solar radiation less than increasing the incoming longwave radiation The dominant energy sinks shift from sublimation/evaporation on highly continental glaciers to melting on maritime/subcontinental glaciers
关键词WESTERN QILIAN MOUNTAINSDEBRIS-COVERED GLACIERSRADIATIVE FLUX PARAMETERIZATIONSINCOMING LONGWAVE RADIATIONMASS-BALANCETIBETAN PLATEAUSOLAR-RADIATIONSCALAR ROUGHNESSMELTING GLACIERSABLATION ZONE
英文关键词glacier; melting; surface energy balance; Tibetan Plateau
语种英语
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
WOS记录号WOS:000664863900018
来源期刊JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES
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/254621
作者单位[Liu, Weigang] China Meteorol Adm, Key Lab Arid Climat Change & Reducing Disaster Ga, Key Open Lab Arid Climate Change & Disaster Reduc, Inst Arid Meteorol, Lanzhou, Peoples R China; [Zhang, Dongqi; Ding, Minghu] Chinese Acad Meteorol Sci, State Key Lab Severe Weather, Beijing, Peoples R China; [Zhang, Dongqi; Ding, Minghu] Chinese Acad Meteorol Sci, Inst Tibetan Plateau & Polar Meteorol, Beijing, Peoples R China; [Qin, Xiang; Ding, Minghu] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, State Key Lab Cryospher Sci, Lanzhou, Peoples R China; [van den Broeke, Michiel R.] Univ Utrecht, Inst Marine & Atmospher Res, Utrecht, Netherlands; [Jiang, Youyan] Lanzhou Reg Climate Ctr, Lanzhou, Peoples R China; [Yang, Diyi] Haining Meteorol Bur, Haining, Peoples R China
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Liu, Weigang,Zhang, Dongqi,Qin, Xiang,et al. Monsoon Clouds Control the Summer Surface Energy Balance on East Rongbuk Glacier (6,523 m Above Sea Level), the Northern of Mt. Qomolangma (Everest)[J]. 中国科学院西北生态环境资源研究院,2021,126(8).
APA Liu, Weigang.,Zhang, Dongqi.,Qin, Xiang.,van den Broeke, Michiel R..,Jiang, Youyan.,...&Ding, Minghu.(2021).Monsoon Clouds Control the Summer Surface Energy Balance on East Rongbuk Glacier (6,523 m Above Sea Level), the Northern of Mt. Qomolangma (Everest).JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES,126(8).
MLA Liu, Weigang,et al."Monsoon Clouds Control the Summer Surface Energy Balance on East Rongbuk Glacier (6,523 m Above Sea Level), the Northern of Mt. Qomolangma (Everest)".JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES 126.8(2021).
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