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首页> 外文期刊>Tellus, Series B. Chemical and Physical Meteorology >Observation-based 3-D view of aerosol radiative properties over Indian Continental Tropical Convergence Zone: implications to regional climate
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Observation-based 3-D view of aerosol radiative properties over Indian Continental Tropical Convergence Zone: implications to regional climate

机译:基于观测的印度大陆热带辐合带气溶胶辐射特性的3-D视图:对区域气候的影响

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摘要

Spatial and vertical distributions of aerosol radiative properties over Indian Continental Tropical Convergence Zone (CTCZ) up to 6 km altitude during the pre-monsoon and monsoon seasons of 2008 have been measured and reported for the first time. Inter-seasonal and intra-seasonal comparisons of different aerosol properties below and above the boundary layer are carried out in and among different regions of CTCZ. During pre-monsoon, aerosol layers were found to be present up to altitude as high as 6 km over the Indo-Gangetic Plains and Himalayan foothills. A large increase in absorption coefficients (by two to five times) near the Himalayan foothills and coastal India than the background values may be attributed to extensive biomass burning as supported by fire counts data. During monsoon, the aerosols were mostly confined to lower troposphere. However, absorbing aerosols were found to rebuild much faster than scattering aerosols after rains. Heating rates were very high over urban city of Bareilly peaking around 2 km during the pre-monsoon. The HR values over urban Kanpur during monsoon were comparable to Bareilly during pre-monsoon. Negligible latitudinal gradient of heating rate from the Himalayan foothill to central India was observed during both the seasons.
机译:首次测量并报告了2008年季风前和季风季节内印度洋热带收敛带(CTCZ)高达6 km高度的气溶胶辐射特性的空间和垂直分布。在CTCZ的不同区域内和之间,对边界层以下和之上的不同气溶胶特性进行了季节间和季节内比较。在季风爆发前,人们发现印度-恒河平原和喜马拉雅山麓地区的气溶胶层高达6 km。喜马拉雅山麓和印度沿海地区的吸收系数比背景值大幅增加(增加了2到5倍),这可能是由于火计数数据所支持的大量生物质燃烧。在季风期间,气溶胶主要局限于对流层下部。但是,发现雨后吸收的气溶胶的重建速度比散布的气溶胶的重建快得多。季风前,城市Bareilly的供暖率非常高,大约在2公里左右。季风期间坎普尔市区的HR值与季风爆发前的Bareilly相当。在两个季节中,从喜马拉雅山麓到印度中部的升温速率的纬度梯度都可以忽略不计。

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