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Tropical storm-induced turbulent mixing and chlorophyll-a enhancement in the continental shelf southeast of Hainan Island

机译:热带风暴引起的湍流混合和海南岛东南大陆架的叶绿素增强

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摘要

Based on moored observations and remote sensing data in July and August 2005, energy sources for enhancing turbulent mixing and possible mechanisms of phytoplankton bloom in the continental shelf southeast of Hainan Island under the influence of Washi, a fast-moving and weak tropical storm, are analyzed in this paper. Observations show that strong near-inertial internal waves were generated by the rapidly changing wind stress and the near-inertial energy was dissipated quickly across the thermocline. The strong turbulent mixing associated with the near-inertial barodinic shear instability occurred with maximum eddy diffusivity above 3.2 x 10(-4) m(2) s(-1), and the surface chlorophyll-a (Chl-a) concentration after the storm increased by 22.2%. The Chl-a concentration augment was inferred to be an upper ocean biophysical response to the enhanced near-inertial turbulent mixing which could increase the upward nutrient flux into the surface low eutrophic zone during the passage of Washi. (C) 2013 The Authors. Published by Elsevier B.V. All rights reserved.
机译:基于2005年7月和2005年8月的停泊观测和遥感数据,在快速移动的热带风暴和弱热带风暴影响下,海南岛东南部大陆架上增加湍流混合的能量来源和浮游植物开花的可能机理是:本文进行了分析。观测结果表明,快速变化的风应力产生了强烈的近惯性内波,并且近惯性能量在整个温跃层上迅速消散。与近惯性二叠纪剪切不稳定性相关的强湍流混合发生,最大涡流扩散率高于3.2 x 10(-4)m(2)s(-1),且表面叶绿素a(Chl-a)浓度较高。风暴增加了22.2%。 Chl-a浓度的增加被认为是对近惯性湍流混合增强的上层海洋生物物理响应,这可能会增加在Washi通行期间向上营养流向表面低营养化区的通量。 (C)2013作者。由Elsevier B.V.发布。保留所有权利。

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