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Dipole pattern in aerosol-induced atmospheric warming trends over the Indian subcontinent in the last two decades

Bibliographic Data

ID15547630
AuthorsShambhu Sharan Srivastava (0009-0007-4415-9469, Indian Institute of Technology Delhi, corresponding author), Sagnik Dey (0000-0002-0604-0869, Korea University)
Year2025
Volume20
Issue4
Pages044005-044005
Publication date2025-02-27
Open AccessYes
TypeARTICLE
VenueEnvironmental Research Letters (JOURNAL)
Journal identifiersISSN: 1748-9326 • E-ISSN: 1748-9326
PublisherIOP Publishing (PUBLISHER • GB)
DOI10.1088/1748-9326/adbb04
OpenAlexW4408012385
LanguageEN
References cited46

Understanding the patterns of aerosol-induced perturbation in radiation budget and its drivers is crucial in climate science. Here, we examined spatio-temporal trends in aerosol-induced atmospheric warming and the top-of-the-atmosphere (TOA) and surface cooling over the Indian Subcontinent under clear-sky and all-sky conditions using clouds and the earth’s radiant energy system data for the period 2000–2021. Overall, the regional mean TOA and surface cooling were found to increase by 0.06 W m −2 yr −1 and 0.09 W m −2 yr −1 , respectively. Over the last two decades, the aerosol-induced atmospheric warming in all-sky conditions increased over the subcontinent landmass and outflow regions over the ocean while it declined over dust-dominated arid regions. This dipole pattern was driven by a combination of an overall increase in aerosol optical depth, a gradual increase in the fraction of scattering aerosols over the Indian landmass dominated by anthropogenic sources, a decline in dust loading over the arid sources. As a result, atmospheric warming efficiency declined in most parts of the Indian subcontinent. A comparative meta-analysis revealed that aerosol-induced atmospheric warming was over-estimated by the existing studies where aerosol direct radiative forcings were estimated by 1-D radiative transfer model utilizing modeled optical properties based on incomplete information about in-situ physico-chemical properties derived from ground-based measurements. Our analysis showed that TOA and surface cooling by aerosols were higher in clear-sky conditions relative to the actual all-sky condition by up to 11 W m −2 and 16 W m −2 , respectively; therefore, atmospheric warming reported for clear-sky conditions would be biased high over the subcontinent. As India embarked on a clean air mission, changes in aerosol loading and its composition are expected to alter the dipole pattern further in the future, impacting the regional climate via dynamic feedback

Aerosol · Atmospheric sciences · Climatology · Geography · Indian subcontinent · Meteorology · Atmospheric aerosols and clouds · Climate variability and models · Environmental Science · Urban Heat Island Mitigation · Geology · History

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Highly citedNo
Open DOIOpen Access
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