Phytoplankton Blooms Triggered by Anticyclonic Eddy and Cyclonic Eddy during Tropical Cyclone Nada

Tropical cyclone (TC) Nada occurred in the southwestern Bay of Bengal (BOB) in the winter of 2016. With high photosynthetically available radiation (PAR) and minimal precipitation, phytoplankton blooms occurred from offshore to nearshore respectively. In this study, there was an pre-existed ocean ed...

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Main Authors: Xueting Xing, Shengzhe Luo, Honghua Zhang, Jianqing Shi, Haibin Lü
Format: Article
Language:English
Published: Stockholm University Press 2023-01-01
Series:Tellus: Series A, Dynamic Meteorology and Oceanography
Online Access:https://a.tellusjournals.se/articles/147
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author Xueting Xing
Shengzhe Luo
Honghua Zhang
Jianqing Shi
Haibin Lü
author_facet Xueting Xing
Shengzhe Luo
Honghua Zhang
Jianqing Shi
Haibin Lü
author_sort Xueting Xing
collection DOAJ
description Tropical cyclone (TC) Nada occurred in the southwestern Bay of Bengal (BOB) in the winter of 2016. With high photosynthetically available radiation (PAR) and minimal precipitation, phytoplankton blooms occurred from offshore to nearshore respectively. In this study, there was an pre-existed ocean eddy pair on the left and right sides of Nada’s path before its passage, we studied the different mechanisms of phytoplankton blooms caused by TC Nada and the ocean eddy pair with satellite observation, multisource reanalysis products, and Argo float data. An anticyclonic eddy near Sri Lanka was weakened during Nada and horizontal transport of chlorophyll-a (Chl-a) balanced the inhibition effect of anticyclone on Chl-a. Near the anticyclonic eddy’s periphery, an upwelling above the thermocline was enhanced by Nada which promoted the uplift of nutrient-rich deep-water. Meanwhile, the large cyclonic eddy in the northern Bay of Bengal was strengthened by Nada, with the vorticity increasing from 0.19 s–1 to 0.28 s–1. Significant inertial oscillation (~2 days period) happened in the subsurface layer, leading to strong vertical mixing and upwelling and subsequently causing the offshore surface Chl-a bloom. This study provides new insights to evaluate typhoons and ocean eddies that induce biological responses in the future.
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spelling doaj.art-df3e59c5fe1f4b8d84188810173537c72023-02-03T14:17:59ZengStockholm University PressTellus: Series A, Dynamic Meteorology and Oceanography1600-08702023-01-0175110.16993/tellusa.1473191Phytoplankton Blooms Triggered by Anticyclonic Eddy and Cyclonic Eddy during Tropical Cyclone NadaXueting Xing0Shengzhe Luo1Honghua Zhang2Jianqing Shi3Haibin Lü4Jiangsu Key Laboratory of Marine Bioresources and Environment /Jiangsu Key Laboratory of Marine Biotechnology, Jiangsu Ocean University, Lianyungang, Jiangsu province; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu province; Lianyungang Meteorological Bureau, Lianyungang, Jiangsu provinceSchool of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu provinceLianyungang Meteorological Bureau, Lianyungang, Jiangsu provinceJiangsu Key Laboratory of Marine Bioresources and Environment /Jiangsu Key Laboratory of Marine Biotechnology, Jiangsu Ocean University, Lianyungang, Jiangsu province; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu provinceJiangsu Key Laboratory of Marine Bioresources and Environment /Jiangsu Key Laboratory of Marine Biotechnology, Jiangsu Ocean University, Lianyungang, Jiangsu province; Co-Innovation Center of Jiangsu Marine Bio-industry Technology, Jiangsu Ocean University, Lianyungang, Jiangsu province; School of Marine Technology and Geomatics, Jiangsu Ocean University, Lianyungang, Jiangsu provinceTropical cyclone (TC) Nada occurred in the southwestern Bay of Bengal (BOB) in the winter of 2016. With high photosynthetically available radiation (PAR) and minimal precipitation, phytoplankton blooms occurred from offshore to nearshore respectively. In this study, there was an pre-existed ocean eddy pair on the left and right sides of Nada’s path before its passage, we studied the different mechanisms of phytoplankton blooms caused by TC Nada and the ocean eddy pair with satellite observation, multisource reanalysis products, and Argo float data. An anticyclonic eddy near Sri Lanka was weakened during Nada and horizontal transport of chlorophyll-a (Chl-a) balanced the inhibition effect of anticyclone on Chl-a. Near the anticyclonic eddy’s periphery, an upwelling above the thermocline was enhanced by Nada which promoted the uplift of nutrient-rich deep-water. Meanwhile, the large cyclonic eddy in the northern Bay of Bengal was strengthened by Nada, with the vorticity increasing from 0.19 s–1 to 0.28 s–1. Significant inertial oscillation (~2 days period) happened in the subsurface layer, leading to strong vertical mixing and upwelling and subsequently causing the offshore surface Chl-a bloom. This study provides new insights to evaluate typhoons and ocean eddies that induce biological responses in the future.https://a.tellusjournals.se/articles/147
spellingShingle Xueting Xing
Shengzhe Luo
Honghua Zhang
Jianqing Shi
Haibin Lü
Phytoplankton Blooms Triggered by Anticyclonic Eddy and Cyclonic Eddy during Tropical Cyclone Nada
Tellus: Series A, Dynamic Meteorology and Oceanography
title Phytoplankton Blooms Triggered by Anticyclonic Eddy and Cyclonic Eddy during Tropical Cyclone Nada
title_full Phytoplankton Blooms Triggered by Anticyclonic Eddy and Cyclonic Eddy during Tropical Cyclone Nada
title_fullStr Phytoplankton Blooms Triggered by Anticyclonic Eddy and Cyclonic Eddy during Tropical Cyclone Nada
title_full_unstemmed Phytoplankton Blooms Triggered by Anticyclonic Eddy and Cyclonic Eddy during Tropical Cyclone Nada
title_short Phytoplankton Blooms Triggered by Anticyclonic Eddy and Cyclonic Eddy during Tropical Cyclone Nada
title_sort phytoplankton blooms triggered by anticyclonic eddy and cyclonic eddy during tropical cyclone nada
url https://a.tellusjournals.se/articles/147
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