HR: 0800h
AN: GC51A-0156    [Abstracts]
TI: The weakening of the Indian Monsoon-ENSO relationship in the '80s and '90s and low frequency variability in the Tropical Atlantic
AU: * Bracco, A
EM: abracco@gatech.edu
AF: EAS Georgia institute of Technology, 311 Ferst Dr, Atlanta, ga 30306, United States
AU: Kucharski, F
EM: kucharsk@ictp.it
AF: Earth System Physics Section, ICTP, Strada Costiera 11, trieste, ts 34014, Italy
AU: Molteni, F
EM: franco.molteni@ecmwf.int
AF: ECMWF, Shinfield Park, Reading, RG2 9AX, United Kingdom
AB: The Indian Monsoon-El Nino Southern Oscillation (ENSO) relationship, according to which a drier than normal monsoon season precedes peak El Nino conditions, weakened significantly during the last two decades of the 20th century. In this work an ensemble of integrations of an Atmospherical General Circulation Model (AGCM) coupled to an ocean model in the Indian basin and forced with observed sea surface temperatures (SSTs) elsewhere is used to investigate the causes of such a weakening.
The observed interdecadal variability of the Monsoon-ENSO relationship during the period 1950-1999 is realistically simulated by the model and a dominant portion of the variability is associated to changes in the tropical Atlantic SSTs in boreal summer.
In correspondance to ENSO, the tropical Atlantic SSTs display negative anomalies south of the Equator in the last quarter of the 20th century and weakly positive anomalies in the previous period. Those anomalies in turn produce heating anomalies which excite a Rossby wave response in the Indian Ocean in both the model and in reanalysis data, impacting the time-mean monsoon circulation.
The proposed mechanism of remote response of the Indian rainfall to the tropical Atlantic SST anomalies induced by ENSO is further tested using the AGCM coupled to the ocean model in the Indian basin and forced by climatological SSTs in the Atlantic Ocean and observed anomalies SSTs elsewhere. In this second ensemble the ENSO-Monsoon relationship is characterized by a stable and strong anticorrelation through the whole second half of the XX century.
DE: 1616 Climate variability (1635, 3305, 3309, 4215, 4513)
DE: 1620 Climate dynamics (0429, 3309)
DE: 1626 Global climate models (3337, 4928)
DE: 1635 Oceans (1616, 3305, 4215, 4513)
SC: Global Environmental Change [GC]
MN: 2007 Fall Meeting