Planetary Boundary Layer and aerosol interactions over the Indian sub-continent

被引:8
|
作者
Patil, M. N. [1 ]
Patil, S. D. [1 ]
Waghmare, R. T. [1 ]
Dharmaraj, T. [1 ]
机构
[1] Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India
关键词
Planetary Boundary Layer; Indian summer monsoon; Aerosols; Green house gases; VOLCANIC-ERUPTIONS; TROPOSPHERIC OZONE; BLACK CARBON; NEW-DELHI; CLIMATE; ATMOSPHERE; TEMPERATURE; RADIATION; HEIGHT; TRENDS;
D O I
10.1016/j.jastp.2014.02.007
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
Aerosols, both natural as well as anthropogenic, affect the radiative forcing of Earth's climate and reduce surface albedo. The Planetary Boundary Layer (PBL) height, which depends upon surface heat budget, is analyzed considering the increase in green house gases (GHGs) from pre-industrial to post-industrial era. The PBL climatology shows deeper PBL during pre-monsoon and summer monsoon seasons as compared to post-monsoon and winter. The PBL height has decreased in post-industrial decade compared to pre-industrial decade. The PBL height reduction is due to increasing aerosol and GHGs' concentrations in the recent decades, which causes surface warming and upper tropospheric cooling. Similarly, due to higher loading of the volcanic aerosol injected from the low latitude eruptions, the atmospheric circulation has been affected. (C) 2014 Elsevier Ltd. All rights reserved.
引用
收藏
页码:38 / 42
页数:5
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