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The onset process of the 2018/2019 Indonesian-Australian summer monsoon: The importance of the air-sea interaction
被引:0
|作者:
Duan, Yongliang
[1
,2
,3
]
Liu, Hongwei
[4
,5
]
Feng, Ming
[6
,7
]
Song, Xiangzhou
[8
]
Li, Kuiping
[1
,2
,3
]
Liu, Lin
[1
,2
,3
]
Liu, Baochao
[1
,2
,3
]
Yang, Guang
[1
,2
,3
]
Yu, Weidong
[2
,9
,10
]
机构:
[1] Minist Nat Resources, Inst Oceanog 1, Key Lab Marine Sci & Numer Modeling, Qingdao, Peoples R China
[2] Qingdao Natl Lab Marine Sci & Technol, Lab Reg Oceanog & Numer Modeling, Qingdao, Peoples R China
[3] Shandong Key Lab Marine Sci & Numer Modeling, Qingdao, Peoples R China
[4] Chinese Acad Sci, Inst Oceanol, CAS Key Lab Ocean Circulat & Waves, Qingdao, Peoples R China
[5] Qingdao Natl Lab Marine Sci & Technol, Qingdao, Peoples R China
[6] CSIRO Oceans & Atmosphere, Crawley, WA, Australia
[7] Ctr Southern Hemisphere Oceans Res, Hobart, Tas, Australia
[8] Hohai Univ, Key Lab Marine Hazards Forecasting, Minist Nat Resources, Nanjing, Peoples R China
[9] Sun Yat Sen Univ, Sch Atmospher Sci, Zhuhai, Peoples R China
[10] Southern Marine Sci & Engn Guangdong Lab Zhuhai, Key Lab Trop Atmosphere Ocean Syst, Minist Educ, Zhuhai, Peoples R China
基金:
中国国家自然科学基金;
关键词:
summer monsoon onset;
air-sea interaction;
Madden-Julian oscillation;
heat budget;
buoy observation;
INDIAN-OCEAN;
EASTWARD PROPAGATION;
TEMPERATURE;
VARIABILITY;
OSCILLATION;
ADVECTION;
DYNAMICS;
FLUXES;
BUDGET;
DARWIN;
D O I:
10.3389/fmars.2022.1089493
中图分类号:
X [环境科学、安全科学];
学科分类号:
08 ;
0830 ;
摘要:
The Madden-Julian oscillation (MJO) and its associated air-sea interactions during the onset process of the 2018/2019 Indonesian-Australian summer monsoon (IASM) are investigated based on the in situ data from a moored buoy off the coast of northwest Australia, along with ERA5 reanalysis and satellite data. The results verify that the IASM onset in mid-December 2018 was triggered by the first-branch eastward-propagating MJO (FEMJO) originating from the tropical Indian Ocean. However, the strong negative SST anomaly (SSTA) was evident off northwest Australia, which weakens FEMJO over northern Australia and shifts the convective center further northward. The mixed layer heat budget analysis based on the buoy observations reveals that the increased latent heat loss that occurred before the arrival of the FEMJO convection was primarily attributed to the large air-sea temperature difference and strong winds, resulting in the pronounced SSTA.
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