ePrints@IIScePrints@IISc Home | About | Browse | Latest Additions | Advanced Search | Contact | Help

Dust absorption over the "Great Indian Desert" inferred using ground-based and satellite remote sensing

Moorthy, Krishna K and Babu, Suresh S and Satheesh, SK and Srinivasan, J and Dutt, CBS (2007) Dust absorption over the "Great Indian Desert" inferred using ground-based and satellite remote sensing. In: Journal of Geophysical Research Atmospheres, 112 (D09206). pp. 1-10.

[img] PDF
Dust_absorption.pdf - Published Version
Restricted to Registered users only

Download (500kB) | Request a copy
Official URL: http://www.agu.org/pubs/crossref/2007/2006JD007690...


Mineral dust is the single largest contributor of natural aerosols over land. Dust aerosols exhibit high variability in their radiative effects because their composition varies locally. This arises because of the regional distinctiveness of the soil characteristics as well as the accumulation of other aerosol species, such as black carbon, on dust while airborne. To accurately estimate the climate impact of dust, spatial and temporal distribution of its radiative properties are essential. However, this is poorly understood over many regions of the world, including the Indian region. In this paper, infrared (IR) radiance $(10.5–12.5 \hspace{2mm} \mu m)$ acquired from METEOSAT-5 satellite (∼5-km resolution) is used to retrieve dust aerosol characteristics over the “Great Indian Desert” and adjacent regions. The infrared radiance depression on account of the presence of dust in the atmosphere has been used as an index of dust load, called the Infrared Difference Dust Index (IDDI). Simultaneous, ground-based spectral optical depths estimated at visible and near-infrared wavelengths (using a multiwavelength solar radiometer) are used along with the IDDI to infer the dust absorption. The inferred single scattering albedo of dust was in the range of 0.88–0.94. We infer that dust over the Indian desert is of more absorbing nature (compared with African dust). Seasonally, the absorption is least in summer and most in winter. The large dust absorption leads to lower atmospheric warming of 0.7–1.2 K $day^{-1}$.

Item Type: Journal Article
Publication: Journal of Geophysical Research Atmospheres
Publisher: American Geophysical Union
Additional Information: Copyright of this article belongs to American Geophysical Union.
Keywords: Aerosols;Remote sensing;Dust absorption
Department/Centre: Division of Mechanical Sciences > Centre for Atmospheric & Oceanic Sciences
Date Deposited: 21 Aug 2007
Last Modified: 02 Feb 2012 10:02
URI: http://eprints.iisc.ac.in/id/eprint/11666

Actions (login required)

View Item View Item