The regional aerosol-climate model REMO-HAM

dc.contributor.authorPietikäinen, Joni-Pekka
dc.contributor.authorO'Donnell, Denis
dc.contributor.authorTeichmann, Christopher
dc.contributor.authorKarstens, Ute
dc.contributor.authorPfeifer, Samuel
dc.contributor.authorKazil, Jan
dc.contributor.authorPodzun, Ralf
dc.contributor.authorFiedler, Susann
dc.contributor.authorKokkola, Harri
dc.contributor.authorBirmili, Wolfram
dc.contributor.authorO'Dowd, Colin D.
dc.contributor.authorBaltensperger, Urs
dc.contributor.authorWeingartner, Ernest
dc.contributor.authorGehrig, Robert
dc.contributor.authorSpindler, Gerald
dc.contributor.authorKulmala, Markku
dc.contributor.authorFeichter, Johann
dc.contributor.authorJacob, Daniela
dc.contributor.authorLaaksonen, Aatto
dc.date.accessioned2024-06-25T07:42:12Z
dc.date.available2024-06-25T07:42:12Z
dc.date.issued2012-11-01
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.
dc.identifier.doi10.5194/gmd-5-1323-2012
dc.identifier.issn1991-9603
dc.identifier.issn1991-959X
dc.identifier.urihttps://irf.fhnw.ch/handle/11654/46248
dc.identifier.urihttps://doi.org/10.26041/fhnw-9366
dc.issue6
dc.language.isoen
dc.publisherCopernicus
dc.relation.ispartofGeoscientific Model Development
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subject.ddc550 - Geowissenschaften
dc.subject.ddc500 - Naturwissenschaften und Mathematik
dc.titleThe regional aerosol-climate model REMO-HAM
dc.type01A - Beitrag in wissenschaftlicher Zeitschrift
dc.volume5
dspace.entity.typePublication
fhnw.InventedHereNo
fhnw.ReviewTypeAnonymous ex ante peer review of a complete publication
fhnw.affiliation.hochschuleHochschule für Technik und Umwelt FHNWde_CH
fhnw.affiliation.institutlnstitut für Sensorik und Elektronikde_CH
fhnw.openAccessCategoryGold
fhnw.pagination1323-1339
fhnw.publicationStatePublished
relation.isAuthorOfPublication05dd9a19-7a24-4325-805a-2d121483b168
relation.isAuthorOfPublication.latestForDiscovery05dd9a19-7a24-4325-805a-2d121483b168
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