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80
70
60
50
40
30
20
10
0
Hissar
Delhi
Dehradun
Bareilly
Lucknow
Allahabad
Gorakhpur
Patna
Calcutta
20
18
16
14
12
10
8
6
4
2
0
Lucknow
Hissar
Delhi
Dehradun
Bareilly
Allahabad
Gorakhpur
Patna
Calcutta
2000-01
2001-02
2002-03
2003-04
2004-05
2005-06
Average
1.6
1.4
1.2
1
0.8
0.6
0.4
0.2
0
Lucknow
Hissar
Delhi
Dehradun
Bareilly
Allahabad
Gorakhpur
Patna
Calcutta
2000-01
2001-02
2002-03
2003-04
2004-05
2005-06
Average
Fig. 3.4 Inter annual variations of relative humidity, air temperature, and wind speed during win-
ter 2000-2006 over nine locations in IGP from surface meteorological stations
The forcing effi ciency indicates the absorbing nature of aerosol, while the intercept
can be treated as the shortwave fl ux when no aerosol is present in the atmosphere.
Here, the Clouds and the Earth's Radiant Energy System (CERES, see Wielicki
et al. 1995 ) Single Scanner Footprint (SSF) shortwave fl ux data at TOA were used to
derive the aerosol radiative forcing effi ciency in conjunction with the MODIS
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