Long term characteristics of aerosols over Pune, central India-Effect on radiative forcing

被引:0
|
作者
Bhaskar, V. Vizaya [1 ]
Soni, V. K. [2 ]
Panicker, A. S. [3 ]
机构
[1] Indian Meteorol Dept, Pune 411005, Maharashtra, India
[2] Indian Meteorol Dept, New Delhi 110003, India
[3] Indian Inst Trop Meteorol, Pune 411008, Maharashtra, India
来源
MAUSAM | 2017年 / 68卷 / 01期
关键词
Sun photometer (MICROTOPS II); AOT; AOT(500); Angstrom exponent; Heating rates; DIURNAL VARIABILITY; OPTICAL-PROPERTIES; CENTRAL HIMALAYAS; IMPACTS; OZONE; DEPTH;
D O I
暂无
中图分类号
P4 [大气科学(气象学)];
学科分类号
0706 ; 070601 ;
摘要
Sun photometer (MICROTOPS II) and Sun -sky radiometer (POM-02, Prede) data for 2003-2013 period are used to study the optical and temporal characteristics of aerosols and their effect on radiative forcing over Pune, central India. The daily mean aerosol optical thickness at 500 nm (AOT(500)) and Angstrom exponent (a) for the study period were 0.77 +/- 0.22 0.92 +/- 0.24 respectively. Short wave aerosol radiative forcing (ARF) computed for the year 2013 using Santa Barbara Discrete-ordinate Atmospheric Radiatiye Transfer (SBDART) model, showed ARF at surface (SUF) and top of the atmosphere (TOA) was negative indicating dominance of scattering type aerosols. AOT, single scattering albedo (SSA) and asymmetry parameter (ASP) derived from Sun sky radiometer showed more AOT and ASP and less SSA during April / May to August indicating prevalence of absorbing soil dust in this period. Atmospheric heating varied from +14.3 to 20.5 W/m(2) and was more in monsoon (+ 35.4 W/m(2)). ARF at SUP was found to be a strong function of AOT(500) (R-2= 0.90). The radiative forcing efficiency inferred to scattering nature of aerosols at SUF (-66.2 W/m(2)/ AOT), TOA (- 0.2 W/m(2) / AOT) and atmosphere (ATM) (+ 66.0 W/m(2) /AOT). The atmospheric heating rates varied from 0.94 K/day in post monsoon to 2.78 K/day in monsoon. Monthly, seasonal and diurnal variability of AOT500 and a with role of meteorological factors are also discussed.
引用
收藏
页码:119 / 130
页数:12
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