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Multi-year investigations of aerosols from an island station, Port Blair, in the Bay of Bengal: climatology and source impacts

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TLDR
In this paper, the spectral aerosol optical depth (AOD) using multi-wavelength solar radiometer (MWR) for a period of seven years (from 2002 to 2008) from the island location, Port Blair (11.63° N, 92.7° E, PBR) in the Bay of Bengal (BoB), along with the concurrent measurements of the size distribution of near-surface aerosols, have been analyzed to delineate the climatological features of aerosols over eastern BoB.
Abstract
. Long-term measurements of spectral aerosol optical depth (AOD) using multi-wavelength solar radiometer (MWR) for a period of seven years (from 2002 to 2008) from the island location, Port Blair (11.63° N, 92.7° E, PBR) in the Bay of Bengal (BoB), along with the concurrent measurements of the size distribution of near-surface aerosols, have been analyzed to delineate the climatological features of aerosols over eastern BoB. In order to identity the contribution of different aerosol types from distinct sources, concentration weighted trajectory (CWT) analysis has been employed. Climatologically, AODs increase from January to reach peak value of ~0.4 (at 500 nm) in March, followed by a weak decrease towards May. Over this general pattern, significant modulations of intra-seasonal time scales, caused by the changes in the relative strength of distinctively different sources, are noticed. The derivative (α') of the Angstrom wavelength exponent α in the wavelength domain, along with CWT analysis, are used to delineate the different important aerosol types that influence this remote island. Corresponding changes in the aerosol size distributions are inferred from the numerical inversion of the spectral AODs as well from (surface) measurements. The analyses revealed that advection plays a major role in modifying the aerosol properties over the remote island location, the potential sources contributing to the accumulation mode (coarse mode) aerosols over eastern BoB being the East Asia and South China regions (Indian mainland and the oceanic regions).

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Aerosol climatology at Delhi in the western Indo‐Gangetic Plain: Microphysics, long‐term trends, and source strengths

TL;DR: In this paper, the authors present the climatology of aerosol microphysics, its trends, and impact of potential sources based on the long term measurements (for a period of 11.5 years from December 2001 to May 2012) in the spectral range 340-1020 nm from an urban center Delhi (28.6°N, 77.3°E, 238 m mean sea level).
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Seasonal variation of surface and vertical profile of aerosol properties over a tropical urban station Hyderabad, India

TL;DR: In this paper, one year measurement of vertical profiles of volume backscatter and extinction coefficient, aerosol optical depth (AOD), mass concentration of black carbon (BC) and composite aerosol along with thermodynamic structure of the atmosphere has been carried out over an urban tropical location of Hyderabad (17.47°N, 78.58°E), India, during April 2009 to March 2010.

Aerosol characterization at the Saharan AERONET site Tamanrasset [Discussion paper]

TL;DR: In this paper, more than two years of columnar atmospheric aerosol measurements (2006-2009) at the Tamanrasset site (22.79° N, 5.53° E, 1377 m a.s.l.), in the heart of the Sahara, are analyzed.
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Long-Range Transport of Mineral Dust to the Northeast Indian Ocean: Regional versus Remote Sources and the Implications

TL;DR: In this article, the relative importance, transport path, and relative importance of satellite remote sensing data with vertical profiles of atmospheric thermodynamics and regional climate model simulations are investigated. But the relative significance of the transport path is not investigated.
References
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Climate Effects of Black Carbon Aerosols in China and India

TL;DR: A global climate model used to investigate possible aerosol contributions to trends in China and India found precipitation and temperature changes in the model that were comparable to those observed if the aerosols included a large proportion of absorbing black carbon (“soot”), similar to observed amounts.
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Wavelength dependence of the optical depth of biomass burning, urban, and desert dust aerosols

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Journal ArticleDOI

Atmospheric brown clouds: impacts on South Asian climate and hydrological cycle.

TL;DR: An ensemble of coupled ocean-atmosphere simulations from 1930 to 2000 suggest that absorbing aerosols in atmospheric brown clouds may have played a major role in the observed regional climate and hydrological cycle changes and have masked as much as 50% of the surface warming due to the global increase in greenhouse gases.
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