Aerosol-CCN characteristics and dynamics associated with a pre-monsoon dust storm over a high-altitude site in Western Ghats, India

Aerosol-CCN characteristics and dynamics during a pre-monsoon dust storm (April 6–11, 2015) over a high-altitude site ((17.92°N, 73.66°E, and 1348 m above mean sea level (MSL)) in Western Ghats, India, has been studied using ground-based observations, satellite, and reanalysis datasets. Spatial dist...

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Veröffentlicht in:Environmental science and pollution research international 2023-10, Vol.30 (50), p.109372-109388
Hauptverfasser: Parambil, Leena Parakkatt, Kumar, Vasudevan Anil, Vijayakumar, Katta, Basheer, Anas Ibnu, Sravanthi, Nukapothula, Patil, Rohit Dilip, Pandithurai, Govindan
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Sprache:eng
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Zusammenfassung:Aerosol-CCN characteristics and dynamics during a pre-monsoon dust storm (April 6–11, 2015) over a high-altitude site ((17.92°N, 73.66°E, and 1348 m above mean sea level (MSL)) in Western Ghats, India, has been studied using ground-based observations, satellite, and reanalysis datasets. Spatial distribution of dust surface mass concentration along with the back trajectory analysis showed the Arabian Desert area (Rub-Al-khali desert) as the source region and strong westerly winds transported the dust particles toward the Indian subcontinent. High values noticed in the surface PM 10 (PM 2.5 ), i.e., ~ 450 (~ 130) µg m −3 , MODIS AOD 550nm (0.6), and MERRA 2 dust surface mass concentration (5 × 10 −7  kg m −3 ) along MODIS true color images confirmed the dust storm event on April 6, 2015 over the observational site. Size-segregated aerosol number concentration measured from ground-based observations showed the dominance of Aitken, accumulation, and coarse mode particles during dust period. CCN concentrations at 0.1, 0.3, 0.5, 0.7, and 0.9% SS were analyzed. A low value of CCN concentration and activation fraction (~ 0.3) near surface was noticed during dust storm day, suggesting insoluble mineral dust particle being transported. Analyzed vertical velocity during pre-dust period showed downdraft between 900 and 750 hPa, suggesting dust transport from upper altitudes toward the observational site. WRF-Chem model simulation also captured the dust storm event, and the results are in good agreement with the observation with a significance of 95% confidence level.
ISSN:1614-7499
0944-1344
1614-7499
DOI:10.1007/s11356-023-30025-6