Prediction of the Indian summer monsoon rainfall using a state-of-the-art coupled ocean-atmosphere model

被引:0
作者
Janakiraman, S. [2 ]
Ved, Mohit [2 ]
Laveti, Ramesh Naidu [2 ]
Yadav, Priyanka [1 ]
Gadgil, Sulochana [1 ]
机构
[1] Indian Inst Sci, Ctr Atmospher & Ocean Sci, Bangalore 560012, Karnataka, India
[2] CDAC, Bangalore 560038, Karnataka, India
来源
CURRENT SCIENCE | 2011年 / 100卷 / 03期
关键词
Ocean-atmosphere model; prediction; rainfall; summer monsoon; CLIMATE FORECAST SYSTEM; VARIABILITY; SIMULATIONS;
D O I
暂无
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A state-of-the-art model of the coupled ocean-atmosphere system, the climate forecast system (CFS), from the National Centres for Environmental Prediction (NCEP), USA, has been ported onto the PARAM Padma parallel computing system at the Centre for Development of Advanced Computing (CDAC), Bangalore and retrospective predictions for the summer monsoon (June-September) season of 2009 have been generated, using five initial conditions for the atmosphere and one initial condition for the ocean for May 2009. Whereas a large deficit in the Indian summer monsoon rainfall (ISMR; June-September) was experienced over the Indian region (with the all-India rainfall deficit by 22% of the average), the ensemble average prediction was for above-average rainfall during the summer monsoon. The retrospective predictions of ISMR with CFS from NCEP for 1981-2008 have been analysed. The retrospective predictions from NCEP for the summer monsoon of 1994 and that from CDAC for 2009 have been compared with the simulations for each of the seasons with the stand-alone atmospheric component of the model, the global forecast system (GFS), and observations. It has been shown that the simulation with GFS for 2009 showed deficit rainfall as observed. The large error in the prediction for the monsoon of 2009 can be attributed to a positive Indian Ocean Dipole event seen in the prediction from July onwards, which was not present in the observations. This suggests that the error could be reduced with improvement of the ocean model over the equatorial Indian Ocean.
引用
收藏
页码:354 / 362
页数:9
相关论文
共 26 条
[1]   Relation between intraseasonal and interannual variability of the South Asian monsoon in the National Centers for Environmental Predictions forecast systems [J].
Achuthavarier, Deepthi ;
Krishnamurthy, V. .
JOURNAL OF GEOPHYSICAL RESEARCH-ATMOSPHERES, 2010, 115
[2]  
Adler RF, 2003, J HYDROMETEOROL, V4, P1147, DOI 10.1175/1525-7541(2003)004<1147:TVGPCP>2.0.CO
[3]  
2
[4]   Coupled dynamics over the Indian Ocean: spring initiation of the Zonal Mode [J].
Annamalai, H ;
Murtugudde, R ;
Potemra, J ;
Xie, SP ;
Liu, P ;
Wang, B .
DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY, 2003, 50 (12-13) :2305-2330
[5]  
[Anonymous], PLATINUM JUBILEE SPE
[6]  
Drbohlav H.K.L., 2010, J CLIMATE, DOI DOI 10.1175/2010JCL12356.1
[7]   Triggering of the positive Indian Ocean dipole events by severe cyclones over the Bay of Bengal [J].
Francis, P. A. ;
Gadgil, Sulochana ;
Vinayachandran, P. N. .
TELLUS SERIES A-DYNAMIC METEOROLOGY AND OCEANOGRAPHY, 2007, 59 (04) :461-475
[8]   Towards understanding the unusual Indian monsoon in 2009 [J].
Francis, P. A. ;
Gadgil, Sulochana .
JOURNAL OF EARTH SYSTEM SCIENCE, 2010, 119 (04) :397-415
[9]  
Francis PA, 2009, CURR SCI INDIA, V97, P1291
[10]  
Gadgil S, 2005, CURR SCI INDIA, V88, P1389