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scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

scostep 2010 (stp12) - Leibniz-Institut für Atmosphärenphysik an der ...

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STP12 Abstracts<br />

Berlin, 12 - 16 July <strong>2010</strong><br />

SCOSTEP Symposium <strong>2010</strong><br />

On the contribution of black carbon radiative forcing to the total aerosol radiative<br />

forcing over <strong>an</strong> urb<strong>an</strong> environment<br />

P<strong>an</strong>icker Abhilash 1 , P<strong>an</strong>dithurai G 1 , Safai P. D 1 , Lee Dong-In 2 , Dipu S 1<br />

1 Indi<strong>an</strong> <strong>Institut</strong>e of Tropical Meteorology, India, 2 Pukyong National University, korea<br />

In this paper we discuss the extent of Black Carbon (BC) radiative forcing in total aerosol<br />

atmospheric radiative forcing over Pune, <strong>an</strong> urb<strong>an</strong> site in India. Collocated measurementsof<br />

aerosol optical properties, chemical composition <strong>an</strong>d BC were carried out for a period of six<br />

months (during October 2004 to May 2005) over the site. Chemical composition data sets of<br />

water soluble, insoluble <strong>an</strong>d BC components were used in Optical Properties of Aerosols <strong>an</strong>d<br />

Clouds (OPAC) to <strong>der</strong>ive aerosol optical properties for composite aerosols. The BC fraction<br />

alone was used in OPAC to <strong>der</strong>ive optical properties solely for BC aerosols. The aerosol<br />

optical properties for composite aerosols <strong>an</strong>d BC aerosols were separately used in SBDART<br />

model to <strong>der</strong>ive aerosol radiative forcing due to composite aerosols <strong>an</strong>d solely due to BC<br />

aerosols. The atmospheric radiative forcing for composite aerosols were found to be +35.5,<br />

+32.9 <strong>an</strong>d +47.6 Wm -2 during post-monsoon, winter <strong>an</strong>d pre-monsoon seasons respectively.<br />

The average BC mass fraction found to be 4.83, 6.33 <strong>an</strong>d 4 µgm -3 during the above seasons<br />

contributing around 2.5 to 6% to the total aerosol load. The atmospheric radiative forcing<br />

estimated due to BC aerosols was +18.8, + 23.4 <strong>an</strong>d +17.2 Wm -2 , respectively during the<br />

above seasons. The study suggests that even though BC contributes only 2.2 to 6% to the total<br />

aerosols load; it is contributing <strong>an</strong> average of around 55% to the total lower atmospheric<br />

aerosol forcing due to strong radiative absorption, <strong>an</strong>d thus enh<strong>an</strong>cing greenhouse warming.

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