TY - JOUR
T1 - Sea surface height fluctuations relevant to Indian summer monsoon over the northwestern Indian Ocean
AU - Zhang, Xiaolin
AU - Mochizuki, Takashi
N1 - Funding Information:
This work was supported by JSPS KAKENHI, Grant Numbers JP19H05703 and JP17K05661.
Funding Information:
We gratefully acknowledge the discussions with Drs. Ruixin Huang, Mikhail Karpytchev, Yu Kosaka, and Tomoki Tozuka for their significant improvements to our work. We also thank Dr. S. Behera and the two reviewers for their helpful comments.
Publisher Copyright:
Copyright © 2022 Zhang and Mochizuki.
PY - 2022/11/8
Y1 - 2022/11/8
N2 - We examined the interannual variations in sea surface height (SSH) over the northwestern Indian Ocean during 1993–2016, by using in situ observations along the east coast of the Arabian Peninsula together with satellite observations, objective analysis, and reanalysis. Focusing on the impacts of the Indian summer monsoon relative to the El Niño Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD) modes, we found that the monsoon predominantly controls the summertime SSH variations at the in situ observatories, consistent with satellite observations. The monsoon is closely related to the SSH at a specific observatory in almost all seasons, whereas the wintertime SSH is strongly influenced by ENSO and IOD at other observatories. These SSH variations with local modulations in the coastal area were accompanied by basin-scale variations. The reduced southwesterly monsoon wind, for example, is found with the reduced ocean upwelling narrowly confined near the coast and the upper ocean temperature rise implying reduced meridional heat transport over the south of the Arabian Peninsula.
AB - We examined the interannual variations in sea surface height (SSH) over the northwestern Indian Ocean during 1993–2016, by using in situ observations along the east coast of the Arabian Peninsula together with satellite observations, objective analysis, and reanalysis. Focusing on the impacts of the Indian summer monsoon relative to the El Niño Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD) modes, we found that the monsoon predominantly controls the summertime SSH variations at the in situ observatories, consistent with satellite observations. The monsoon is closely related to the SSH at a specific observatory in almost all seasons, whereas the wintertime SSH is strongly influenced by ENSO and IOD at other observatories. These SSH variations with local modulations in the coastal area were accompanied by basin-scale variations. The reduced southwesterly monsoon wind, for example, is found with the reduced ocean upwelling narrowly confined near the coast and the upper ocean temperature rise implying reduced meridional heat transport over the south of the Arabian Peninsula.
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U2 - 10.3389/fclim.2022.1008776
DO - 10.3389/fclim.2022.1008776
M3 - Article
AN - SCOPUS:85142248543
SN - 2624-9553
VL - 4
JO - Frontiers in Climate
JF - Frontiers in Climate
M1 - 1008776
ER -