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Synoptic scale disturbances of the Indian summer monsoon as simulated in a high resolution climate model

MPG-Autoren
http://pubman.mpdl.mpg.de/cone/persons/resource/persons37102

Bengtsson,  Lennart
MPI for Meteorology, Max Planck Society;

http://pubman.mpdl.mpg.de/cone/persons/resource/persons37141

Esch,  Monika
MPI for Meteorology, Max Planck Society;

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c005p243.pdf
(Verlagsversion), 3MB

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Zitation

Lal, M., Bengtsson, L., Cubasch, U., Esch, M., & Schlese, U. (1995). Synoptic scale disturbances of the Indian summer monsoon as simulated in a high resolution climate model. Climate Research, 5, 243-258. doi:10.3354/cr005243.


Zitierlink: http://hdl.handle.net/11858/00-001M-0000-0014-A00D-B
Zusammenfassung
The Hamburg atmospheric general circulation model ECHAM3 at T106 resolution (1.125* lat./lon.) has considerable skill in reproducing the observed seasonal reversal of mean sea level pressure, the location of the summer heat low as well as the position of the monsoon trough over the Indian subcontinent. The present-day climate and its seasonal cycle are realistically simulated by the model over this region. The model simulates the structure, intensity, frequency, movement and lifetime of monsoon depressions remarkably well. The number of monsoon depressions/storms simulated by the model in a year ranged from 5 to 12 with an average frequency of 8.4 yr-1, not significantly different from the observed climatology. The model also simulates the interannual variability in the formation of depressions over the north Bay of Bengal during the summer monsoon season. In the warmer atmosphere under doubled CO2 conditions, the number of monsoon depressions/cyclonic storms forming in Indian seas in a year ranged from 5 to 11 with an average frequency of 7.6 yr-1, not significantly different from those inferred in the control run of the model. However, under doubled CO2 conditions, fewer depressions formed in the month of June. Neither the lowest central pressure nor the maximum wind speed changes appreciably in monsoon depressions identified under simulated enhanced greenhouse conditions. The analysis suggests there will be no significant changes in the number and intensity of monsoon depressions in a warmer atmosphere.