The onset process of the 2018/2019 Indonesian–Australian summer monsoon: The importance of the air–sea interaction

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 satelli...

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Main Authors: Yongliang Duan, Hongwei Liu, Ming Feng, Xiangzhou Song, Kuiping Li, Lin Liu, Baochao Liu, Guang Yang, Weidong Yu
Format: Article
Language:English
Published: Frontiers Media S.A. 2023-01-01
Series:Frontiers in Marine Science
Subjects:
Online Access:https://www.frontiersin.org/articles/10.3389/fmars.2022.1089493/full
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author Yongliang Duan
Yongliang Duan
Yongliang Duan
Hongwei Liu
Ming Feng
Ming Feng
Xiangzhou Song
Kuiping Li
Kuiping Li
Kuiping Li
Lin Liu
Lin Liu
Lin Liu
Baochao Liu
Baochao Liu
Baochao Liu
Guang Yang
Guang Yang
Guang Yang
Weidong Yu
Weidong Yu
Weidong Yu
Weidong Yu
author_facet Yongliang Duan
Yongliang Duan
Yongliang Duan
Hongwei Liu
Ming Feng
Ming Feng
Xiangzhou Song
Kuiping Li
Kuiping Li
Kuiping Li
Lin Liu
Lin Liu
Lin Liu
Baochao Liu
Baochao Liu
Baochao Liu
Guang Yang
Guang Yang
Guang Yang
Weidong Yu
Weidong Yu
Weidong Yu
Weidong Yu
author_sort Yongliang Duan
collection DOAJ
description 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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spelling doaj.art-3c095d91a601455080495b618a9698552023-01-09T08:24:31ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452023-01-01910.3389/fmars.2022.10894931089493The onset process of the 2018/2019 Indonesian–Australian summer monsoon: The importance of the air–sea interactionYongliang Duan0Yongliang Duan1Yongliang Duan2Hongwei Liu3Ming Feng4Ming Feng5Xiangzhou Song6Kuiping Li7Kuiping Li8Kuiping Li9Lin Liu10Lin Liu11Lin Liu12Baochao Liu13Baochao Liu14Baochao Liu15Guang Yang16Guang Yang17Guang Yang18Weidong Yu19Weidong Yu20Weidong Yu21Weidong Yu22Key Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaCAS Key Laboratory of Ocean Circulation and Waves, Institute of Oceanology, Chinese Academy of Sciences, and Qingdao National Laboratory for Marine Science and Technology, Qingdao, ChinaCSIRO Oceans and Atmosphere, Crawley, WA, AustraliaCentre for Southern Hemisphere Oceans Research, Hobart, TAS, AustraliaKey Laboratory of Marine Hazards Forecasting, Ministry of Natural Resources, Hohai University, Nanjing, ChinaKey Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaKey Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaKey Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaKey Laboratory of Marine Science and Numerical Modeling, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, ChinaShandong Key Laboratory of Marine Science and Numerical Modeling, Qingdao, ChinaLaboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao, ChinaSchool of Atmospheric Sciences, Sun Yat-Sen University, Zhuhai, ChinaKey Laboratory of Tropical Atmosphere-Ocean System (Sun Yat-Sen University), Ministry of Education, Zhuhai, China0Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai, ChinaThe 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.https://www.frontiersin.org/articles/10.3389/fmars.2022.1089493/fullsummer monsoon onsetair-sea interactionMadden-Julian oscillationheat budgetbuoy observation
spellingShingle Yongliang Duan
Yongliang Duan
Yongliang Duan
Hongwei Liu
Ming Feng
Ming Feng
Xiangzhou Song
Kuiping Li
Kuiping Li
Kuiping Li
Lin Liu
Lin Liu
Lin Liu
Baochao Liu
Baochao Liu
Baochao Liu
Guang Yang
Guang Yang
Guang Yang
Weidong Yu
Weidong Yu
Weidong Yu
Weidong Yu
The onset process of the 2018/2019 Indonesian–Australian summer monsoon: The importance of the air–sea interaction
Frontiers in Marine Science
summer monsoon onset
air-sea interaction
Madden-Julian oscillation
heat budget
buoy observation
title The onset process of the 2018/2019 Indonesian–Australian summer monsoon: The importance of the air–sea interaction
title_full The onset process of the 2018/2019 Indonesian–Australian summer monsoon: The importance of the air–sea interaction
title_fullStr The onset process of the 2018/2019 Indonesian–Australian summer monsoon: The importance of the air–sea interaction
title_full_unstemmed The onset process of the 2018/2019 Indonesian–Australian summer monsoon: The importance of the air–sea interaction
title_short The onset process of the 2018/2019 Indonesian–Australian summer monsoon: The importance of the air–sea interaction
title_sort onset process of the 2018 2019 indonesian australian summer monsoon the importance of the air sea interaction
topic summer monsoon onset
air-sea interaction
Madden-Julian oscillation
heat budget
buoy observation
url https://www.frontiersin.org/articles/10.3389/fmars.2022.1089493/full
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