Implementation of aerosol-cloud interactions in the regional atmosphere-aerosol model COSMO-Muscat(5.0) and evaluation using satellite data
dc.bibliographicCitation.firstPage | 2231 | |
dc.bibliographicCitation.issue | 6 | |
dc.bibliographicCitation.journalTitle | Geoscientific model development : GMD | eng |
dc.bibliographicCitation.lastPage | 2246 | |
dc.bibliographicCitation.volume | 10 | |
dc.contributor.author | Dipu, Sudhakar | |
dc.contributor.author | Quaas, Johannes | |
dc.contributor.author | Wolke, Ralf | |
dc.contributor.author | Stoll, Jens | |
dc.contributor.author | Mühlbauer, Andreas | |
dc.contributor.author | Sourdeval, Odran | |
dc.contributor.author | Salzmann, Marc | |
dc.contributor.author | Heinold, Bernd | |
dc.contributor.author | Tegen, Ina | |
dc.date.accessioned | 2023-02-27T08:51:29Z | |
dc.date.available | 2023-02-27T08:51:29Z | |
dc.date.issued | 2017 | |
dc.description.abstract | The regional atmospheric model Consortium for Small-scale Modeling (COSMO) coupled to the Multi-Scale Chemistry Aerosol Transport model (Muscat) is extended in this work to represent aerosol-cloud interactions. Previously, only one-way interactions (scavenging of aerosol and in-cloud chemistry) and aerosol-radiation interactions were included in this model. The new version allows for a microphysical aerosol effect on clouds. For this, we use the optional two-moment cloud microphysical scheme in COSMO and the online-computed aerosol information for cloud condensation nuclei concentrations (Cccn), replacing the constant Cccn profile. In the radiation scheme, we have implemented a droplet-size-dependent cloud optical depth, allowing now for aerosol-cloud-radiation interactions. To evaluate the models with satellite data, the Cloud Feedback Model Intercomparison Project Observation Simulator Package (COSP) has been implemented. A case study has been carried out to understand the effects of the modifications, where the modified modeling system is applied over the European domain with a horizontal resolution of 0.25°g × g0.25°. To reduce the complexity in aerosol-cloud interactions, only warm-phase clouds are considered. We found that the online-coupled aerosol introduces significant changes for some cloud microphysical properties. The cloud effective radius shows an increase of 9.5g%, and the cloud droplet number concentration is reduced by 21.5g%. | eng |
dc.description.version | publishedVersion | eng |
dc.identifier.uri | https://oa.tib.eu/renate/handle/123456789/11540 | |
dc.identifier.uri | http://dx.doi.org/10.34657/10574 | |
dc.language.iso | eng | |
dc.publisher | Katlenburg-Lindau : Copernicus | |
dc.relation.doi | https://doi.org/10.5194/gmd-10-2231-2017 | |
dc.relation.essn | 1991-9603 | |
dc.rights.license | CC BY 3.0 Unported | |
dc.rights.uri | https://creativecommons.org/licenses/by/3.0 | |
dc.subject.ddc | 910 | |
dc.subject.other | aerosol | eng |
dc.subject.other | atmospheric modeling | eng |
dc.subject.other | climate feedback | eng |
dc.subject.other | cloud | eng |
dc.subject.other | cloud condensation nucleus | eng |
dc.subject.other | cloud droplet | eng |
dc.subject.other | cloud microphysics | eng |
dc.subject.other | cloud radiative forcing | eng |
dc.subject.other | regional climate | eng |
dc.subject.other | satellite data | eng |
dc.title | Implementation of aerosol-cloud interactions in the regional atmosphere-aerosol model COSMO-Muscat(5.0) and evaluation using satellite data | eng |
dc.type | Article | eng |
dc.type | Text | eng |
tib.accessRights | openAccess | |
wgl.contributor | TROPOS | |
wgl.subject | Geowissenschaften | ger |
wgl.type | Zeitschriftenartikel | ger |
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