Aerosol radiative effects on mesoscale cloud–precipitation variables over Northeast Asia during the MAPS-Seoul 2015 campaign. (January 2018)

• Record Type: Journal Article
• Authors: Park, Shin-Young; Lee, Hyo-Jung; Kang, Jeong-Eon; Lee, Taehyoung; Kim, Cheol-Hee
• Is Part Of: Atmospheric environment. Volume 172(2018)
• Page Start: 109
• Page End: 123
• Publication Date: 2018-01
• Subjects: WRF-Chem -- Aerosol-cloud-radiation interaction -- Aerosol effects -- MAPS-Seoul 2015; Air -- Pollution -- Periodicals; Air -- Pollution -- Meteorological aspects -- Periodicals; 551.51
• DOI: 10.1016/j.atmosenv.2017.10.044
• Languages: English
• ISSNs: 1352-2310

Abstract

Abstract: The online model, Weather Research and Forecasting Model with Chemistry (WRF-Chem) is employed to interpret the effects of aerosol-cloud-precipitation interaction on mesoscale meteorological fields over Northeast Asia during the Megacity Air Pollution Study-Seoul (MAPS-Seoul) 2015 campaign. The MAPS-Seoul campaign is a pre-campaign of the Korea-United States Air Quality (KORUS-AQ) campaign conducted over the Korean Peninsula. We validated the WRF-Chem simulations during the campaign period, and analyzed aerosol-warm cloud interactions by diagnosing both aerosol direct, indirect, and total effects. The results demonstrated that aerosol directly decreased downward shortwave radiation up to −44% (−282 W m −2 ) for this period and subsequently increased downward longwave radiation up to +15% (∼52 W m −2 ) in the presence of low-level clouds along the thematic area. Aerosol increased cloud fraction indirectly up to ∼24% with the increases of both liquid water path and the droplet number mixing ratio. Precipitation properties were altered both directly and indirectly. Direct effects simply changed cloud-precipitation quantities via simple updraft process associated with perturbed radiation and temperature, while indirect effects mainly suppressed precipitation, but sometimes increased precipitation in the higher relative humidity atmosphere or near vapor-saturated condition. The total aerosol effects caused a time lag of the precipitation rate with the delayed onset time of up to 9 h. This implies the importance of aerosol effects in improving mesoscale precipitation rate prediction in the online approach in the presence of non-linear warm cloud. Highlights: Aerosol-derived perturbations of daily weather prediction variables were studied. Mesoscale fields were better characterized by aerosol-cloud-radiation interaction. Lag of rain onset time ∼9 h was derived by aerosol effects during MAPS-Seoul campaign. Aerosol effects on rain enhanced over the downstream due to transboundary process.