کد مقاله | کد نشریه | سال انتشار | مقاله انگلیسی | نسخه تمام متن |
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1777042 | 1523655 | 2012 | 10 صفحه PDF | دانلود رایگان |
Contribution of semitransparent cirrus (STC) to the scattering properties of particulates in the UTLS region is examined over the Indian region using the lidar data from Gadanki (13.5°N, 79.2°E) and SAGE-II measurements from 30°S to 30°N in the longitude region 70–90°E within the feasibility of these measurements. While the contribution of STC to particulate optical depth (τp) in UT is found to be quite significant in the equatorial and off-equatorial regions in both the hemispheres during summer, this is very small during winter in the off-equatorial regions. Dense STCs in UT also influences the aerosol scattering below the cloud-base and above the cloud-top (LS). This STC influence in LS is quite significant in the northern hemisphere and almost insignificant over the southern hemisphere, where the STC-cover as well as its optical depth is relatively low. This hemispheric difference is attributed to relatively strong tropospheric convection in the northern hemisphere.
► STCs significantly contribute to optical scattering in the UT region.
► Dense STCs in the UT region influence aerosol scattering above and below the cloud.
► IGWs originating from deep convection during ASM transports particulates to LS region.
► B–D circulation could be playing an important role in the troposphere–stratosphere exchange during winter.
Journal: Journal of Atmospheric and Solar-Terrestrial Physics - Volume 74, January 2012, Pages 1–10