Investigation of Urban Land Use Change and Aerosol Indirect Effects on Frontal Rainfall Near Coastal Regions: A Case Study of a Rainstorm Over the Pearl River Delta in South China
Abstract
River Delta on October 13, 2011, using the WRF-ARW model with 1992 and 2011 land use data and varied cloud condensation nuclei (CCN)
concentrations. Results showed total rainfall and intensity decreased with higher CCN, with greater suppression under high urbanization
(13.29% reduction vs. 7.91% under low urbanization) due to enhanced ice- and graupel-phase processes. ULUC increased rainfall via urban
heat/dry island effects extending the planetary boundary layer, favoring heavy rain.
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[1]Albrecht, B.A. (1989). Aerosols, cloud microphysics, and fractional cloudiness.Science, 245, 1227–1230.
[2]Alexander, L.V. et al. (2006). Global observed changes in daily climate extremes of temperature and precipitation.Journal of Geophysical Research, 111, D05109.
[3]Givati A, Rosenfeld D. 2004. Quantifying precipitation suppression due to air pollution. Journal of Applied Meteorology 43:1038–
1056.
[4]Lin WS, Zhang L, Du D, Yang L, Lin H, Zhang Y, Li J. 2009. Quantification of land use/land cover changes in Pearl River Delta and
its impact on regional climate in summer using numerical modeling. Regional Environmental Change 9: 75-82.
[5]Rose, D. et al. (2010). Cloud condensation nuclei near Guangzhou, China.Atmospheric Chemistry and Physics, 10, 3365–3383.
[6]Tao, W.-K. et al. (2012). Impact of aerosols on convective clouds and precipitation.Reviews of Geophysics, 50, 2011RG000369.
DOI: http://dx.doi.org/10.18686/ag.v9i1.14184
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