An integrated campaign for investigation of winter-time continental haze over Indo-Gangetic Basin and its radiative effects.

Sci Total Environ

Environmental Sciences Section, Bose Institute, Kolkata, India; Center for Astroparticle Physics and Space Science, Bose Institute, Kolkata, India; National Facility on Astroparticle Physics and Space Science, Darjeeling, India.

Published: November 2015

AI Article Synopsis

  • An integrated study was conducted from December 2013 to February 2014 to analyze continental haze from the Indo-Gangetic Basin (IGB) to the Bay of Bengal (BoB), measuring its radiative effects at three locations in eastern India: Kolkata, Siliguri, and Sundarban.
  • The highest aerosol optical depth (AOD) was recorded in Kolkata, with significant black carbon concentrations, indicating urban pollution's impact on haze levels.
  • Findings show that this winter-time haze contributes to high aerosol radiative forcing, particularly over Kolkata, influencing regional climate and potentially affecting monsoonal patterns.

Article Abstract

An outflow of continental haze occurs from Indo-Gangetic Basin (IGB) in the North to Bay of Bengal (BoB) in the South. An integrated campaign was organized to investigate this continental haze during December 2013-February 2014 at source and remote regions within IGB to quantify its radiative effects. Measurements were carried out at three locations in eastern India; 1) Kalas Island, Sundarban (21.68°N, 88.57°E) - an isolated island along the north-east coast of BoB, 2) Kolkata (22.57°N, 88.42°E) - an urban metropolis and 3) Siliguri (26.70°N, 88.35°E) - an urban region at the foothills of eastern Himalayas. Ground-based AOD (at 0.5 μm) is observed to be maximum (1.25±0.18) over Kolkata followed by Siliguri (0.60±0.17) and minimum over Sundarban (0.53±0.18). Black carbon concentration is found to be maximum at Kolkata (21.6±6.6 μg·m(-3)) with almost equal concentrations at Siliguri (12.6±5.2 μg·m(-3)) and Sundarban (12.3±3.0 μg·m(-3)). Combination of MODIS-AOD and back-trajectories analysis shows an outflow of winter-time continental haze originating from central IGB and venting out through Sundarban towards BoB. This continental haze with high extinction coefficient is identified up to central BoB using CALIPSO observations and is found to contribute ~75% to marine AOD over central BoB. This haze produces significantly high aerosol radiative forcing within the atmosphere over Kolkata (75.4 Wm(-2)) as well as over Siliguri and Sundarban (40 Wm(-2)) indicating large forcing over entire IGB, from foothills of the Himalayas to coastal region. This winter-time continental haze also causes about similar radiative heating (1.5 K·day(-1)) from Siliguri to Sundarban which is enhanced over Kolkata (3 K·day(-1)) due to large emission of local urban aerosols. This high aerosol heating over entire IGB and coastal region of BoB can have considerable impact on the monsoonal circulation and more importantly, such haze transported over to BoB can significantly affect the marine hydrological cycle.

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http://dx.doi.org/10.1016/j.scitotenv.2015.06.085DOI Listing

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