Baroclinic instability-induced intensification of phytoplankton blooms at submesoscales in eutrophic frontal regions

IF 3.8 1区 地球科学 Q1 LIMNOLOGY
Zhonghua Zhao, Lie-Yauw Oey, Zhaoyun Chen, Bangqin Huang, Huijie Xue, Shuh-Ji Kao, Feng Cai, Yuwu Jiang
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Abstract

Off-coast phytoplankton blooms occur frequently in the frontal region of the eutrophic Taiwan Strait during the northeasterly monsoon relaxation period, as consistently revealed by extensive cruise and satellite observations. Realistic model simulations have shown that restratification by frontal baroclinic instability (BCI) plays a crucial role in triggering blooms under nutrient-rich conditions. This study deciphered the distinct contributions of submesoscale and mesoscale BCIs to bloom development using sensitivity tests of an idealized model of the Taiwan Strait featuring an intense alongshore front with ample nutrients. In three-dimensional fine simulations with both submesoscale and mesoscale BCIs present, blooms were triggered by the cessation of a down-front wind. Chlorophyll a was higher in submesoscale front regions than in mesoscale regions, primarily because of the higher upper-ocean stability resulting from more effective restratification by submesoscale BCI. In three-dimensional coarse simulations, mesoscale BCI led to relatively lower upper-ocean stability and weaker blooms following wind relaxation, consistent with those in mesoscale regions in corresponding three-dimensional fine simulations. In two-dimensional simulations without submesoscale and mesoscale BCIs, blooms could not be triggered despite the cessation of a down-front wind, primarily because of the absence of significant near-surface restratification by BCIs. Furthermore, although symmetric instability was present in two-dimensional fine simulations, its contribution to blooms was limited because of its minimal restratification effect. These results show that BCIs play the predominant role in triggering off-coast blooms in eutrophic coastal front regions such as the Taiwan Strait.

斜压不稳定导致富营养化额区亚中尺度浮游植物华的加剧
在东北季风弛豫期,富营养化的台湾海峡锋面区经常发生近海浮游植物大量繁殖,这是广泛的巡航和卫星观测所一致揭示的。现实的模型模拟表明,在营养丰富的条件下,锋斜压不稳定性(BCI)的重新强化在触发华花中起着至关重要的作用。本研究利用台湾海峡理想化模型的敏感性测试,揭示了亚中尺度和中尺度bci对水华发展的独特贡献,该模型具有强烈的沿岸锋和充足的营养物质。在亚中尺度和中尺度bci同时存在的三维精细模拟中,华花是由一个下风的停止引发的。叶绿素a在亚中尺度锋区高于中尺度锋区,这主要是由于亚中尺度BCI更有效的复冰作用导致了更高的上层海洋稳定性。在三维粗糙模拟中,中尺度BCI导致了相对较低的上层海洋稳定性和较弱的风松弛后华花,这与相应的三维精细模拟中中尺度区域的结果一致。在没有亚中尺度和中尺度bci的二维模拟中,尽管停止了下风,但仍不能触发华花,这主要是因为bci没有显著的近地面再冰作用。此外,尽管在二维精细模拟中存在对称不稳定性,但由于其最小的再固化效应,其对华花的贡献有限。这些结果表明,在台湾海峡等富营养化沿海地区,bci在引发近海水华中起主导作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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来源期刊
Limnology and Oceanography
Limnology and Oceanography 地学-海洋学
CiteScore
8.80
自引率
6.70%
发文量
254
审稿时长
3 months
期刊介绍: Limnology and Oceanography (L&O; print ISSN 0024-3590, online ISSN 1939-5590) publishes original articles, including scholarly reviews, about all aspects of limnology and oceanography. The journal''s unifying theme is the understanding of aquatic systems. Submissions are judged on the originality of their data, interpretations, and ideas, and on the degree to which they can be generalized beyond the particular aquatic system examined. Laboratory and modeling studies must demonstrate relevance to field environments; typically this means that they are bolstered by substantial "real-world" data. Few purely theoretical or purely empirical papers are accepted for review.
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