An Intrathermocline Eddy Observed in the Northeastern Bay of Bengal

Abstract An intrathermocline eddy (ITE) was detected to the northwest of Preparis Channel by in situ measurements in January 2018. The ITE had a horizontal extent of approximately 200 km and a maximum velocity of approximately 60 cm/s at core depths between 75 and 130 m. This ITE was generated by th...

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Main Authors: Xiwu Zhou, Yun Qiu, Xinyu Lin, Hui Teng, Cherry Aung
Format: Article
Language:English
Published: Wiley 2022-06-01
Series:Geophysical Research Letters
Subjects:
Online Access:https://doi.org/10.1029/2022GL099201
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author Xiwu Zhou
Yun Qiu
Xinyu Lin
Hui Teng
Cherry Aung
author_facet Xiwu Zhou
Yun Qiu
Xinyu Lin
Hui Teng
Cherry Aung
author_sort Xiwu Zhou
collection DOAJ
description Abstract An intrathermocline eddy (ITE) was detected to the northwest of Preparis Channel by in situ measurements in January 2018. The ITE had a horizontal extent of approximately 200 km and a maximum velocity of approximately 60 cm/s at core depths between 75 and 130 m. This ITE was generated by the transformation from a preexisting surface‐intensified anticyclonic eddy (SAE). The blocking of the northeast monsoon by the Arakan Yoma Mountains resulted in a weak wind stress on the leeward side of the mountains. This caused positive Ekman pumping around Preparis Channel together with eddy wind‐driven upwelling, shoaling the upper thermocline in the SAE, and thus turning it into an ITE. Among the 71 anticyclonic eddies detected by Argo profiles around Preparis Channel from 2003 to 2018, approximately 60% were ITEs, indicating that Preparis Channel could be the main source for ITE generation in Bay of Bengal.
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publishDate 2022-06-01
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spelling doaj-art-c6407bc14158454e8978d167671901652025-01-22T14:38:16ZengWileyGeophysical Research Letters0094-82761944-80072022-06-014912n/an/a10.1029/2022GL099201An Intrathermocline Eddy Observed in the Northeastern Bay of BengalXiwu Zhou0Yun Qiu1Xinyu Lin2Hui Teng3Cherry Aung4Third Institute of Oceanography Ministry of Natural Resources Xiamen ChinaThird Institute of Oceanography Ministry of Natural Resources Xiamen ChinaThird Institute of Oceanography Ministry of Natural Resources Xiamen ChinaThird Institute of Oceanography Ministry of Natural Resources Xiamen ChinaMarine Science Department Myeik University Tanintharyi MyanmarAbstract An intrathermocline eddy (ITE) was detected to the northwest of Preparis Channel by in situ measurements in January 2018. The ITE had a horizontal extent of approximately 200 km and a maximum velocity of approximately 60 cm/s at core depths between 75 and 130 m. This ITE was generated by the transformation from a preexisting surface‐intensified anticyclonic eddy (SAE). The blocking of the northeast monsoon by the Arakan Yoma Mountains resulted in a weak wind stress on the leeward side of the mountains. This caused positive Ekman pumping around Preparis Channel together with eddy wind‐driven upwelling, shoaling the upper thermocline in the SAE, and thus turning it into an ITE. Among the 71 anticyclonic eddies detected by Argo profiles around Preparis Channel from 2003 to 2018, approximately 60% were ITEs, indicating that Preparis Channel could be the main source for ITE generation in Bay of Bengal.https://doi.org/10.1029/2022GL099201intrathermocline eddyKelvin waveBay of Bengalmonsoon
spellingShingle Xiwu Zhou
Yun Qiu
Xinyu Lin
Hui Teng
Cherry Aung
An Intrathermocline Eddy Observed in the Northeastern Bay of Bengal
Geophysical Research Letters
intrathermocline eddy
Kelvin wave
Bay of Bengal
monsoon
title An Intrathermocline Eddy Observed in the Northeastern Bay of Bengal
title_full An Intrathermocline Eddy Observed in the Northeastern Bay of Bengal
title_fullStr An Intrathermocline Eddy Observed in the Northeastern Bay of Bengal
title_full_unstemmed An Intrathermocline Eddy Observed in the Northeastern Bay of Bengal
title_short An Intrathermocline Eddy Observed in the Northeastern Bay of Bengal
title_sort intrathermocline eddy observed in the northeastern bay of bengal
topic intrathermocline eddy
Kelvin wave
Bay of Bengal
monsoon
url https://doi.org/10.1029/2022GL099201
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