Wet Scavenging in WRF‐Chem Simulations of Parameterized Convection for a Severe Storm During the DC3 Field Campaign

Deep convection can transport surface moisture and pollution from the planetary boundary layer to the upper troposphere (UT) within a few minutes. The convective transport of precursors of both ozone and aerosols from the planetary boundary layer affects the concentrations of these constituents in t...

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Veröffentlicht in:	Journal of geophysical research. Atmospheres 2019-07, Vol.124 (13), p.7413-7428
Hauptverfasser:	Li, Y., Pickering, K. E., Barth, M. C., Bela, M. M., Cummings, K. A., Allen, D. J.
Format:	Artikel
Sprache:	eng
Schlagworte:	Aerosols Atmospheric chemistry Boundary layers Cloud parameterization Clouds Computer simulation Convection Convective transport deep convective transport Earth Freezing Gases Geophysics Hydrogen peroxide ice retention factor Mixing ratio Organic chemistry Ozone Ozone mixing ratio Parameterization Planetary boundary layer Pollution dispersion Precursors Radiation Radiation budget Rain Rain water Scavenging Simulation Storms Sulfur dioxide Thunderstorms Trace gases Transport Troposphere Upper troposphere Water pollution Weather forecasting wet scavenging WRF‐Chem
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