Observed Impact of the South Asian Summer Monsoon on the Local Meteorology in the Himalayas

被引:13
|
作者
Zhou Libo [1 ]
Zou Han [1 ]
Ma Shupo [1 ]
Li Peng [1 ]
机构
[1] Chinese Acad Sci, Inst Atmospher Phys, LAPC, Beijing 100029, Peoples R China
来源
ACTA METEOROLOGICA SINICA | 2012年 / 26卷 / 02期
基金
中国国家自然科学基金;
关键词
the South Asian summer monsoon; the Himalayas; local meteorology; LARGE-SCALE CIRCULATION; KALI-GANDAKI VALLEY; TIBETAN PLATEAU; INTERANNUAL VARIABILITY; DIURNAL WINDS; CHINA SEA; ONSET; EVOLUTION; PRECIPITATION; TRANSITION;
D O I
10.1007/s13351-012-0206-0
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
The South Asian summer monsoon (SASM) is the most important climate system in Asia. Using observational data from the HEST2006 (Himalayan Exchange between the Surface and Troposphere 2006) campaign and large-scale grid data, this paper analyzed the SASM impact on local meteorological parameters including radiation, temperature, humidity, and wind in the Himalayas. The SASM experienced one active and one break period during the HEST2006 campaign. The local meteorological parameters exhibit great differences between the active period and the break period of the SASM. The radiation fluxes are greater in the break period than in the active period. The air temperature and specific humidity are lower, but soil temperature and wind speed are higher in the break period than in the active period. Further analysis indicates that the SASM greatly affects the meteorological features of the Himalayan region.
引用
收藏
页码:205 / 215
页数:11
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