Deutsch
 
Hilfe Datenschutzhinweis Impressum
  DetailsucheBrowse

Datensatz

DATENSATZ AKTIONENEXPORT

Freigegeben

Forschungspapier

Simulation of the present-day climate with the ECHAM model: Impact of model physics and resolution

MPG-Autoren
/persons/resource/persons37308

Roeckner,  Erich
MPI for Meteorology, Max Planck Society;

/persons/resource/persons37087

Arpe,  Klaus
MPI for Meteorology, Max Planck Society;

/persons/resource/persons37102

Bengtsson,  Lennart
MPI for Meteorology, Max Planck Society;

Dümenil,  Lydia
MPI for Meteorology, Max Planck Society;

/persons/resource/persons37141

Esch,  Monika
MPI for Meteorology, Max Planck Society;

Externe Ressourcen
Es sind keine externen Ressourcen hinterlegt
Volltexte (beschränkter Zugriff)
Für Ihren IP-Bereich sind aktuell keine Volltexte freigegeben.
Volltexte (frei zugänglich)

093-Report.pdf
(Verlagsversion), 12MB

Ergänzendes Material (frei zugänglich)
Es sind keine frei zugänglichen Ergänzenden Materialien verfügbar
Zitation

Roeckner, E., Arpe, K., Bengtsson, L., Brinkop, S., Dümenil, L., Esch, M., et al. (1992). Simulation of the present-day climate with the ECHAM model: Impact of model physics and resolution. Report / Max-Planck-Institut für Meteorologie, 93.


Zitierlink: https://hdl.handle.net/11858/00-001M-0000-0014-A078-C
Zusammenfassung
A detailed description of the third-generation atmospheric general circulation model ECHAM is presen-
ted. The climatology of ECHAM3, as simulated at low and high resolution (T21 and T42, respectively),
is compared with ECMWF analyses (1981-1990) and also with the climatology of two earlier low reso-
lution versions ECHAM 1 and ECHAM2.
At low resolution, the impact of the improved model physics is evident primarily in the simulated time-
mean state which is more successfully reproduced by the more recent model versions, particularly by
ECHAM3. The impact of increased horizontal resolution can be identified not on] v by a generally impro-
ved time-mean circulation, particularly in the Southern Hemisphere, but mosbsignificantly by the incre-
ased level of high-frequency variability. In the low-frequency range, however, the impact of increased
horizontal resolution is modest, and all models fail to reproduce the observed level of low-frequency
intraseasonal variability