The regional aerosol-climate model REMO-HAM

dc.bibliographicCitation.firstPage1323eng
dc.bibliographicCitation.issue6eng
dc.bibliographicCitation.lastPage1339eng
dc.bibliographicCitation.volume5
dc.contributor.authorPietikäinen, J.-P.
dc.contributor.authorO'Donnell, D.
dc.contributor.authorTeichmann, C.
dc.contributor.authorKarstens, U.
dc.contributor.authorPfeifer, S.
dc.contributor.authorKazil, J.
dc.contributor.authorPodzun, R.
dc.contributor.authorFiedler, S.
dc.contributor.authorKokkola, H.
dc.contributor.authorBirmili, W.
dc.contributor.authorO'Dowd, C.
dc.contributor.authorBaltensperger, U.
dc.contributor.authorWeingartner, E.
dc.contributor.authorGehrig, R.
dc.contributor.authorSpindler, G.
dc.contributor.authorKulmala, M.
dc.contributor.authorFeichter, J.
dc.contributor.authorJacob, D.
dc.contributor.authorLaaksonen, A.
dc.date.accessioned2018-01-11T11:16:17Z
dc.date.available2019-06-26T17:21:18Z
dc.date.issued2012
dc.description.abstractREMO-HAM is a new regional aerosol-climate model. It is based on the REMO regional climate model and includes most of the major aerosol processes. The structure for aerosol is similar to the global aerosol-climate model ECHAM5-HAM, for example the aerosol module HAM is coupled with a two-moment stratiform cloud scheme. On the other hand, REMO-HAM does not include an online coupled aerosol-radiation nor a secondary organic aerosol module. In this work, we evaluate the model and compare the results against ECHAM5-HAM and measurements. Four different measurement sites were chosen for the comparison of total number concentrations, size distributions and gas phase sulfur dioxide concentrations: Hyytiälä in Finland, Melpitz in Germany, Mace Head in Ireland and Jungfraujoch in Switzerland. REMO-HAM is run with two different resolutions: 50 × 50 km2 and 10 × 10 km2. Based on our simulations, REMO-HAM is in reasonable agreement with the measured values. The differences in the total number concentrations between REMO-HAM and ECHAM5-HAM can be mainly explained by the difference in the nucleation mode. Since we did not use activation nor kinetic nucleation for the boundary layer, the total number concentrations are somewhat underestimated. From the meteorological point of view, REMO-HAM represents the precipitation fields and 2 m temperature profile very well compared to measurement. Overall, we show that REMO-HAM is a functional aerosol-climate model, which will be used in further studies.eng
dc.description.versionpublishedVersioneng
dc.formatapplication/pdf
dc.identifier.urihttps://doi.org/10.34657/1363
dc.identifier.urihttps://oa.tib.eu/renate/handle/123456789/849
dc.language.isoengeng
dc.publisherMünchen : European Geopyhsical Unioneng
dc.relation.doihttps://doi.org/10.5194/gmd-5-1323-2012
dc.relation.ispartofseriesGeoscientific Model Development, Volume 5, Issue 6, Page 1323-1339eng
dc.rights.licenseCC BY 3.0 Unportedeng
dc.rights.urihttps://creativecommons.org/licenses/by/3.0/eng
dc.subjectaerosoleng
dc.subjectboundary layereng
dc.subjectclimate modelingeng
dc.subjectgas phase reactioneng
dc.subjectmeteorologyeng
dc.subjectnucleationeng
dc.subjectnumerical modeleng
dc.subjectregional climateeng
dc.subjectsize distributioneng
dc.subjectsulfur dioxideeng
dc.subjecttemperature profileeng
dc.subject.ddc550eng
dc.titleThe regional aerosol-climate model REMO-HAMeng
dc.typearticleeng
dc.typeTexteng
dcterms.bibliographicCitation.journalTitleGeoscientific Model Developmenteng
tib.accessRightsopenAccesseng
wgl.contributorTROPOSeng
wgl.subjectGeowissenschafteneng
wgl.typeZeitschriftenartikeleng
Files
Original bundle
Now showing 1 - 1 of 1
Loading...
Thumbnail Image
Name:
gmd-5-1323-2012.pdf
Size:
2.18 MB
Format:
Adobe Portable Document Format
Description: