Effects of monsoon onset vortex on heat budget in the mixed layer of the Bay of Bengal

Kang XU; Boqi LIU; Yu LIU; Weiqiang WANG; Zhuoqi HE

doi:10.1007/s00343-019-9061-5

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Effects of monsoon onset vortex on heat budget in the mixed layer of the Bay of Bengal

Special Section on Indo-Pac Project | Updated：2023-04-27

- Effects of monsoon onset vortex on heat budget in the mixed layer of the Bay of Bengal
- Effects of monsoon onset vortex on heat budget in the mixed layer of the Bay of Bengal
- 海洋湖沼学报（英文） 2020年38卷第6期页码：1616-1631
- Affiliations：
  
  1.State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, China
  2.Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou), Guangzhou 511458, China
  3.Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences, Guangzhou 510301, China
  4.State Key Laboratory of Severe Weather and Institute of Climate System, Chinese Academy of Meteorological Sciences, Beijing 100081, China
  5.Institute of Deep-sea Science and Engineering, Chinese Academy of Sciences, Sanya 572000, China
  6.University of Chinese Academy of Sciences, Beijing 100049, China
  7.Laboratory for Regional Oceanography and Numerical Modeling, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China
  8.State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China
- Author bio：
  
  XU Kang, xukang@scsio.ac.cn
- Funds：
  
  the Strategic Priority Research Program of Chinese Academy of Sciences(XDA20060502);the Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou)(GML2019ZD0306);the National Natural Science Foundation of China(41776023);the National Natural Science Foundation of China(41731173);the National Natural Science Foundation of China(41521005);the National Natural Science Foundation of China(41676013);the National Natural Science Foundation of China(41775052);the National Natural Science Foundation of China(41506003);the Rising Star Foundation of the South China Sea Institute of Oceanology(NHXX2018WL0201);the Innovation Academy of South China Sea Ecology and Environmental Engineering, Chinese Academy of Sciences(ISEE2018PY06);the Independent Research Project Program of State Key Laboratory of Tropical Oceanography(LTOZZ1802);the Basic Scientific Research and Operation Foundation of the CAMS(2018Z006);the Basic Scientific Research and Operation Foundation of the CAMS(2017R001);© Chinese Society for Oceanology and Limnology, Science Press and Springer-Verlag GmbH Germany, part of Springer Nature 2020
- DOI：10.1007/s00343-019-9061-5
  中图分类号：
- 收稿：2019-03-11，
  
  录用：2019-7-19，
  
  网络首发：2019-08-26，
  
  纸质出版：2020-11
- Accepted：
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Effects of monsoon onset vortex on heat budget in the mixed layer of the Bay of Bengal[J]. 海洋湖沼学报（英文）, 2020,38(6):1616-1631.

Kang XU, Boqi LIU, Yu LIU, et al. Effects of monsoon onset vortex on heat budget in the mixed layer of the Bay of Bengal[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1616-1631.
Effects of monsoon onset vortex on heat budget in the mixed layer of the Bay of Bengal[J]. 海洋湖沼学报（英文）, 2020,38(6):1616-1631. DOI： 10.1007/s00343-019-9061-5.

Kang XU, Boqi LIU, Yu LIU, et al. Effects of monsoon onset vortex on heat budget in the mixed layer of the Bay of Bengal[J]. Journal of Oceanology and Limnology, 2020, 38(6): 1616-1631. DOI： 10.1007/s00343-019-9061-5.

摘要

Abstract

We investigated the effects of monsoon onset vortex (MOV) on the mixed layer heat budget in the Bay of Bengal (BOB) in spring 2003 using the reanalysis datasets. The results suggest that the solar radiation flux penetrating the mixed layer and the existence of barrier layer are both able to modulate the effects of MOV on the evolution of sea surface temperature (SST) in the BOB. Prior to the formation of BOB MOV

the local SST raised quickly due to mass of solar radiation reaching the sea surface under the clear-sky condition. Meanwhile

since the mixed layer was shallow before the onset of the Asian summer monsoon (ASM)

some solar radiation flux could penetrate to directly heat the deeper water

which partly offset the warming effect of shortwave radiation. On the other hand

the in-situ SST started to cool due to the upwelling of cold water when the MOV generated over the BOB

along with the rapidly increased surface wind speed and its resultant deeper mixed layer. As the MOV developed and moved northward

the SST tended to decrease remarkably because of the strong upward surface latent heat flux over the BOB ascribed to the wind-evaporation mechanism. However

the MOV-related precipitation brought more fresh water into the upper ocean to produce a thicker barrier layer

whose thermal barrier effect damped the cooling effect of entrainment upwelling on the decrease tendency of the BOB SST. In other words

the thermal barrier effect could slow down the decreasing trend of the BOB SST even after the onset of ASM

which facilitated the further enhancement of the MOV.

关键词

Keywords

references

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