Dipole pattern in aerosol-induced atmospheric warming trends over the Indian subcontinent in the last two decades
Bibliographic Data
| ID | 15547630 |
|---|---|
| Authors | Shambhu Sharan Srivastava (0009-0007-4415-9469, Indian Institute of Technology Delhi, corresponding author), Sagnik Dey (0000-0002-0604-0869, Korea University) |
| Year | 2025 |
| Volume | 20 |
| Issue | 4 |
| Pages | 044005-044005 |
| Publication date | 2025-02-27 |
| Open Access | Yes |
| Type | ARTICLE |
| Venue | Environmental Research Letters (JOURNAL) |
| Journal identifiers | ISSN: 1748-9326 • E-ISSN: 1748-9326 |
| Publisher | IOP Publishing (PUBLISHER • GB) |
| DOI | 10.1088/1748-9326/adbb04 |
| OpenAlex | W4408012385 |
| Language | EN |
| References cited | 46 |
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
| Highly cited | No |
|---|