Micro pulse lidar observations of mineral dust layer in the lower troposphere over the southwest coast of Peninsular India during the Asian summer monsoon season

被引:40
|
作者
Mishra, Manoj Kumar [1 ]
Rajeev, K. [1 ]
Thampi, Bijoy V. [1 ]
Parameswaran, K. [1 ]
Nair, Anish Kumar M. [1 ]
机构
[1] Vikram Sarabhai Space Ctr, Space Phys Lab, Thiruvananthapuram 695022, Kerala, India
关键词
Aerosol transport; Mineral dust; Lidar; Asian summer monsoon; Indian region; REGIONAL AEROSOL DISTRIBUTION; ARABIAN SEA; SATELLITE-OBSERVATIONS; OPTICAL-PROPERTIES; TRANSPORT; OCEAN;
D O I
10.1016/j.jastp.2010.08.012
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
A large aerosol plume with optical depth exceeding 0.7 engulfs most parts of the Arabian Sea during the Asian summer monsoon season. Based on Micro Pulse Lidar observations during the June-September period of 2008 and 2009, the present study depicts, for the first time, the existence of an elevated dust layer occurring very frequently in the altitude band of 1-3.5 km over the west coast of peninsular India with relatively large values of linear depolarization ratio (delta(L)). Large values of delta(L) indicate the dominance of significantly non-spherical aerosols. The aerosol optical depth of this layer (0.2) is comparable to that of the entire atmospheric column during dust-free days. Back-trajectory analysis clearly shows the advection of airmass from the arid regions of Arabia and the west Arabian Sea, through the altitude region centered around 3 km. This is in contrast to the airmass below 1 km originating from the pristine Indian Ocean region which contains relatively spherical aerosols of marine origin with delta(L) generally <0.05. (C) 2010 Elsevier Ltd. All rights reserved.
引用
收藏
页码:1251 / 1259
页数:9
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