Toward Understanding the Diverse Impacts of Air-Sea Interactions on MJO Simulations

被引:13
作者
Fu, Joshua-Xiouhua [1 ,2 ,3 ]
Wang, Wanqiu [4 ]
Shinoda, Toshiaki [5 ]
Ren, Hong-Li [3 ]
Jia, Xiaolong [3 ]
机构
[1] Univ Hawaii Manoa, IPRC, SOEST, Honolulu, HI 96822 USA
[2] Fudan Univ, Inst Atmospher Sci, Shanghai, Peoples R China
[3] China Meteorol Adm, Natl Climate Ctr, Beijing, Peoples R China
[4] NOAA, Climate Predict Ctr, NWS, NCEP, College Pk, MD USA
[5] Texas A&M Univ, Corpus Christi, TX USA
基金
美国国家科学基金会;
关键词
diverse air-sea coupling; MJO simulations; different cumulus schemes; different SST conditions; NCEP GFS; MADDEN-JULIAN OSCILLATION; TROPICAL INTRASEASONAL OSCILLATION; GENERAL-CIRCULATION MODELS; SURFACE TEMPERATURE; INDIAN-OCEAN; WESTERN PACIFIC; ATMOSPHERIC VARIABILITY; WEATHER PREDICTION; SST VARIABILITY; FORECAST SYSTEM;
D O I
10.1002/2017JC013187
中图分类号
P7 [海洋学];
学科分类号
0707 ;
摘要
The role of air-sea interactions on MJO simulations has long been recognized. However, the reasons for the variation of the impacts of air-sea coupling among different models are still elusive. In this study, we used NCEP GFS under different cumulus schemes and SST conditions to explore this issue. We focused on the Oct-MJO and Nov-MJO during the DYNAMO IOP. We show that the effects of SST-feedback on MJO simulations not only vary between these two MJO events, but are also very sensitive to the specifics of cumulus schemes and intraseasonal SST forcing. The Oct-MJO basically reinvigorates over Indian Ocean in association with the arrival of global circumnavigating mode. The Nov-MJO is largely reinvigorated by a robust intraseasonal SST anomaly over Indian Ocean. We found that SST-feedback is crucial for the existence of the Nov-MJO, but has little effect on the Oct-MJO. This finding raises the possibility that the occurrence of some MJO events may be rooted in air-sea interactions. These results suggest that the diverse impacts of air-sea coupling on MJO simulations can be attributed to at least the following three potential causes: (i) diverse responses of ocean to individual MJO events in nature; (ii) diverse behaviors of various cumulus parameterizations; and (iii) diverse intraseasonal SST anomalies in coupled models. Either a too weak internal MJO mode in atmospheric models or a too weak intraseasonal SST anomaly in coupled models would lead to the underestimation of the impacts of air-sea coupling on MJO simulations.
引用
收藏
页码:8855 / 8875
页数:21
相关论文
共 118 条
[1]  
Anderson SP, 1996, J CLIMATE, V9, P3056, DOI 10.1175/1520-0442(1996)009<3056:SBFATM>2.0.CO
[2]  
2
[3]  
ARAKAWA A, 1974, J ATMOS SCI, V31, P674, DOI 10.1175/1520-0469(1974)031<0674:IOACCE>2.0.CO
[4]  
2
[5]   Advances in simulating atmospheric variability with the ECMWF model:: From synoptic to decadal time-scales [J].
Bechtold, Peter ;
Koehler, Martin ;
Jung, Thomas ;
Doblas-Reyes, Francisco ;
Leutbecher, Martin ;
Rodwell, Mark J. ;
Vitart, Frederic ;
Balsamo, Gianpaolo .
QUARTERLY JOURNAL OF THE ROYAL METEOROLOGICAL SOCIETY, 2008, 134 (634) :1337-1351
[6]   Impacts of Idealized Air-Sea Coupling on Madden-Julian Oscillation Structure in the Superparameterized CAM [J].
Benedict, James J. ;
Randall, David A. .
JOURNAL OF THE ATMOSPHERIC SCIENCES, 2011, 68 (09) :1990-2008
[7]  
Bhat GS, 2004, J ATMOS OCEAN TECH, V21, P1283, DOI 10.1175/1520-0426(2004)021<1283:SSTOTB>2.0.CO
[8]  
2
[9]  
BJERKNES J, 1969, MON WEATHER REV, V97, P163, DOI 10.1175/1520-0493(1969)097<0163:ATFTEP>2.3.CO
[10]  
2