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[

] 110

H

ealth

droughts and floods in Asian countries,

3

others have

suggested that BC leads to the advancement and inten-

sification of monsoons.

4

There have been reports that BC

blocks sunlight from reaching the Earth’s surface and leads

to reduced crop yields.

5

As most of these are based on

model outputs, which use transport model simulations as

input for the global/regional distribution of BC, they are

not adequately validated. Limited validation exercises have

shown that the transport models underperform, at least

in simulating BC, over India.

6

All these point to the need

for and importance of accurate measurements of BC from

ground and airborne platforms.

Evolution of BC studies

Systematic and long-term measurements of BC over the

Indian region was initiated in 2000, under the ISRO-GBP

Aerosol Climatology and Effects project, in response

to recommendations made in an interim assessment

of the aerosol characteristics over the region in 1998.

The first long-term measurement was initiated in 2000

Atmospheric aerosols, particulate suspension in the atmosphere,

affects radiation balance by scattering and absorbing the radiation

(direct effects), modifying the microphysical and radiative properties of

clouds (indirect effects), and degrading air quality with adverse effects

on health. Among the various aerosol types, there has been increased

interest in BC aerosols due to their high absorption characteristics over

a wide wavelength range from ultraviolet to infrared. In addition to

exerting its own radiative impacts, BC can substantially alter the radia-

tive properties of the entire aerosol system and their ability to act as

cloud condensation nuclei. The overall effect of aerosols when viewed

from space is a brightening of the planet and net climatic cooling at the

surface. However, BC contributes significantly to dimming as well as to

the warming of the lower atmosphere, producing an effect analogous to

greenhouse warming, which is amplified if the BC aerosol layer occurs

over highly reflective landmass (snow/ice /glaciers) or highly scattered

clouds.

1

On the other hand, BC within the cloud can lead to ‘cloud

burn-off’ and a reduction of cloud cover.

2

In addition to these climate

implications, BC is a health hazard and is believed to be carcinogenic.

In recent years there have been several studies of the climate impact

of BC aerosols. While some of these have argued that BC intensifies

Source: ARFI

Top panels: The instrumented aircraft used to measure BC profiles (left) and the inside view of the aircraft with instruments. Bottom

Panels: Locations of aircraft measurements of BC with aircraft symbol (left). The altitude distribution of BC over Indian region during

winter and pre-monsoon seasons (right panels).