The regional aerosol-climate model REMO-HAM

REMO-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 stra...

Full description

Bibliographic Details
Main Authors: J.-P. Pietikäinen, D. O'Donnell, C. Teichmann, U. Karstens, S. Pfeifer, J. Kazil, R. Podzun, S. Fiedler, H. Kokkola, W. Birmili, C. O'Dowd, U. Baltensperger, E. Weingartner, R. Gehrig, G. Spindler, M. Kulmala, J. Feichter, D. Jacob, A. Laaksonen
Format: Article
Language:English
Published: Copernicus Publications 2012-11-01
Series:Geoscientific Model Development
Online Access:http://www.geosci-model-dev.net/5/1323/2012/gmd-5-1323-2012.pdf
_version_ 1811320225536147456
author J.-P. Pietikäinen
D. O'Donnell
C. Teichmann
U. Karstens
S. Pfeifer
J. Kazil
R. Podzun
S. Fiedler
H. Kokkola
W. Birmili
C. O'Dowd
U. Baltensperger
E. Weingartner
R. Gehrig
G. Spindler
M. Kulmala
J. Feichter
D. Jacob
A. Laaksonen
author_facet J.-P. Pietikäinen
D. O'Donnell
C. Teichmann
U. Karstens
S. Pfeifer
J. Kazil
R. Podzun
S. Fiedler
H. Kokkola
W. Birmili
C. O'Dowd
U. Baltensperger
E. Weingartner
R. Gehrig
G. Spindler
M. Kulmala
J. Feichter
D. Jacob
A. Laaksonen
author_sort J.-P. Pietikäinen
collection DOAJ
description REMO-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 km<sup>2</sup> and 10 × 10 km<sup>2</sup>. 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.
first_indexed 2024-04-13T12:56:15Z
format Article
id doaj.art-fe354d4816914a10aebc073ed10c9d57
institution Directory Open Access Journal
issn 1991-959X
1991-9603
language English
last_indexed 2024-04-13T12:56:15Z
publishDate 2012-11-01
publisher Copernicus Publications
record_format Article
series Geoscientific Model Development
spelling doaj.art-fe354d4816914a10aebc073ed10c9d572022-12-22T02:46:03ZengCopernicus PublicationsGeoscientific Model Development1991-959X1991-96032012-11-01561323133910.5194/gmd-5-1323-2012The regional aerosol-climate model REMO-HAMJ.-P. PietikäinenD. O'DonnellC. TeichmannU. KarstensS. PfeiferJ. KazilR. PodzunS. FiedlerH. KokkolaW. BirmiliC. O'DowdU. BaltenspergerE. WeingartnerR. GehrigG. SpindlerM. KulmalaJ. FeichterD. JacobA. LaaksonenREMO-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 km<sup>2</sup> and 10 × 10 km<sup>2</sup>. 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.http://www.geosci-model-dev.net/5/1323/2012/gmd-5-1323-2012.pdf
spellingShingle J.-P. Pietikäinen
D. O'Donnell
C. Teichmann
U. Karstens
S. Pfeifer
J. Kazil
R. Podzun
S. Fiedler
H. Kokkola
W. Birmili
C. O'Dowd
U. Baltensperger
E. Weingartner
R. Gehrig
G. Spindler
M. Kulmala
J. Feichter
D. Jacob
A. Laaksonen
The regional aerosol-climate model REMO-HAM
Geoscientific Model Development
title The regional aerosol-climate model REMO-HAM
title_full The regional aerosol-climate model REMO-HAM
title_fullStr The regional aerosol-climate model REMO-HAM
title_full_unstemmed The regional aerosol-climate model REMO-HAM
title_short The regional aerosol-climate model REMO-HAM
title_sort regional aerosol climate model remo ham
url http://www.geosci-model-dev.net/5/1323/2012/gmd-5-1323-2012.pdf
work_keys_str_mv AT jppietikainen theregionalaerosolclimatemodelremoham
AT dodonnell theregionalaerosolclimatemodelremoham
AT cteichmann theregionalaerosolclimatemodelremoham
AT ukarstens theregionalaerosolclimatemodelremoham
AT spfeifer theregionalaerosolclimatemodelremoham
AT jkazil theregionalaerosolclimatemodelremoham
AT rpodzun theregionalaerosolclimatemodelremoham
AT sfiedler theregionalaerosolclimatemodelremoham
AT hkokkola theregionalaerosolclimatemodelremoham
AT wbirmili theregionalaerosolclimatemodelremoham
AT codowd theregionalaerosolclimatemodelremoham
AT ubaltensperger theregionalaerosolclimatemodelremoham
AT eweingartner theregionalaerosolclimatemodelremoham
AT rgehrig theregionalaerosolclimatemodelremoham
AT gspindler theregionalaerosolclimatemodelremoham
AT mkulmala theregionalaerosolclimatemodelremoham
AT jfeichter theregionalaerosolclimatemodelremoham
AT djacob theregionalaerosolclimatemodelremoham
AT alaaksonen theregionalaerosolclimatemodelremoham
AT jppietikainen regionalaerosolclimatemodelremoham
AT dodonnell regionalaerosolclimatemodelremoham
AT cteichmann regionalaerosolclimatemodelremoham
AT ukarstens regionalaerosolclimatemodelremoham
AT spfeifer regionalaerosolclimatemodelremoham
AT jkazil regionalaerosolclimatemodelremoham
AT rpodzun regionalaerosolclimatemodelremoham
AT sfiedler regionalaerosolclimatemodelremoham
AT hkokkola regionalaerosolclimatemodelremoham
AT wbirmili regionalaerosolclimatemodelremoham
AT codowd regionalaerosolclimatemodelremoham
AT ubaltensperger regionalaerosolclimatemodelremoham
AT eweingartner regionalaerosolclimatemodelremoham
AT rgehrig regionalaerosolclimatemodelremoham
AT gspindler regionalaerosolclimatemodelremoham
AT mkulmala regionalaerosolclimatemodelremoham
AT jfeichter regionalaerosolclimatemodelremoham
AT djacob regionalaerosolclimatemodelremoham
AT alaaksonen regionalaerosolclimatemodelremoham