The impacts of dust aerosol and convective available potential energy on precipitation vertical structure in southeastern China as seen from multisource observations
School of Earth and Space Science, Comparative Planetary Excellence
Innovation Center, University of Science and Technology of China, Hefei
230026, China
School of Earth and Space Science, Comparative Planetary Excellence
Innovation Center, University of Science and Technology of China, Hefei
230026, China
State Key Laboratory of Fire Science, University of Science and
Technology of China, Hefei 230026, China
Institut de recherche sur les forêts, Université du Québec en Abitibi-Témiscamingue (UQAT), Rouyn-Noranda, J9X 5E4, Canada
Shuping Yang
School of Earth and Space Science, Comparative Planetary Excellence
Innovation Center, University of Science and Technology of China, Hefei
230026, China
Chun Zhao
School of Earth and Space Science, Comparative Planetary Excellence
Innovation Center, University of Science and Technology of China, Hefei
230026, China
School of Earth and Space Science, Comparative Planetary Excellence
Innovation Center, University of Science and Technology of China, Hefei
230026, China
Chen Huang
School of Earth and Space Science, Comparative Planetary Excellence
Innovation Center, University of Science and Technology of China, Hefei
230026, China
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Total article views: 3,822 (including HTML, PDF, and XML)
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Total article views: 3,213 (including HTML, PDF, and XML)
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The impacts of atmospheric dust aerosols and cloud dynamic conditions on precipitation vertical development in southeastern China were studied using multiple satellite observations. It was found that the precipitating drops under dusty conditions grow faster in the middle layer but slower in the upper and lower layers compared with their pristine counterparts. Quantitative estimation of the sensitivity of the precipitation top temperature to the dust aerosol optical depth is also provided.
The impacts of atmospheric dust aerosols and cloud dynamic conditions on precipitation vertical...
