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Chemistry of rain events in West Africa: evidence of dust and biogenic influence in convective systems
Chemistry of rain events West Africa dust and biogenic influence convective systems
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2010/10/11
This paper documents the chemical composition of 7 rain events associated with mesoscale convective systems sampled at the supersite of Banizoumbou, Niger, during the first special observation periods...
Aerosol size-dependent below-cloud scavenging by rain and snow in the ECHAM5-HAM
size-dependent below-cloud scavenging rain snow ECHAM5-HAM
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2009/7/23
Wet deposition processes are highly efficient in the removal of aerosols from the atmosphere, and thus strongly influence global aerosol concentrations, and clouds, and their respective radiative forc...
Physical properties of the sub-micrometer aerosol over the Amazon rain forest during the wet-to-dry season transition - comparison of modeled and measured CCN concentrations
sub-micrometer aerosol Amazon rain forest wet-to-dry season transition
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2009/3/9
Sub-micrometer atmospheric aerosol particles were studied in the Amazon region, 125 km northeast of Manaus, Brazil (-1°55.2'S, 59°28.1'W). The measurements were performed during the wet-to-dry transit...
Comparison of rain gauge observations with modeled precipitation over Cyprus using Contiguous Rain Area analysis
rain gauge observations modeled precipitation Cyprus Contiguous Rain Area
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2009/2/16
Verification of modeled rainfall with precipitation observed by a rain gauge network has been performed in a case study over the Cyprus Island. Cyprus has a relatively dense rain gauge network. The ap...
Seasonal variation of ozone deposition to a tropical rain forest in southwest Amazonia
ozone deposition tropical rain forest southwest Amazonia
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2008/12/23
Within the project EUropean Studies on Trace gases and Atmospheric CHemistry as a contribution to Large-scale Biosphere-atmosphere experiment in Amazonia (LBA-EUSTACH), we performed tower-based eddy c...
Effect of explicit urban land surface representation on the simulation of the 26 July 2005 heavy rain event over Mumbai, India
explicit urban land heavy rain Mumbai India
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2008/11/24
We investigate whether explicit representation of the urban land surface improves the simulation of the record-breaking 24-h heavy rain event that occurred over Mumbai, India on 26 July 2005 as the ev...
Corrigendum to“Influence of Giant CCN on warm rain processes in the ECHAM5 GCM”published in Atmos. Chem. Phys., 8, 2949–2963, 2008.
Influence Giant CCN ECHAM5 GCM
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2008/11/19
Corrigendum to "Influence of Giant CCN on warm rain processes in the ECHAM5 GCM" published in Atmos. Chem. Phys., 8, 2949–2963, 2008.
Introduction of prognostic rain in ECHAM5: design and single column model simulations
prognostic rain ECHAM5 single column model
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2008/11/10
Prognostic equations for the rain mass mixing ratio and the rain drop number concentration are introduced into the large-scale cloud microphysics parameterization of the ECHAM5 general circulation mod...
Aerosols' influence on the interplay between condensation, evaporation and rain in warm cumulus cloud
Aerosols' influence interplay condensation evaporation warm cumulus cloud
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2008/10/24
A numerical cloud model is used to study the influence of aerosol on the microphysics and dynamics of moderate-sized, coastal, convective clouds that develop under the same meteorological conditions....