印尼海域锋面的季节和年际变化及其对叶绿素 a 的影响

IF 2.8 2区 地球科学 Q1 OCEANOGRAPHY
Hao-Ran Zhang, Yi Yu, Zhibin Gao, Yanwei Zhang, Wentao Ma, Dezhou Yang, Baoshu Yin, Yuntao Wang
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引用次数: 0

摘要

利用高分辨率卫星观测资料,研究了印度尼西亚海域海洋锋的时空变化。该研究旨在了解驱动这些锋面的潜在机制及其对叶绿素-a变异性的影响。锋面概率在主要岛屿海岸附近较高,表现出明显的季节周期,高峰出现在南部冬季。叶绿素-a的分布变异性总体上与活跃锋面带的存在一致,但锋面与叶绿素-a的显著正相关仅局限于某些特定区域,如南爪哇岛和西里伯斯海。在爪哇上升流区,风驱动的上升流在锋面生成中起主要作用,锋面活动的增强可以促进浮游植物的生长,导致叶绿素-a的增加。此外,研究还表明,风型比锋面概率和叶绿素-a的变化早两个月左右。这种滞后表明该地区锋面和叶绿素a的时空变化主要受季风系统的影响。此外,海温对叶绿素-a的变化具有同步调节作用。大部分地区海温负异常与叶绿素-a锋概率正异常相关。值得注意的是,爪哇上升流区锋面和叶绿素a的年际变化非常明显。El Niño年,该地区季风增强,海温呈负距平,锋概率和叶绿素a呈正距平。本研究提供了印度尼西亚海域锋面活动的综合描述和潜在动力学。这些发现有助于描述叶绿素-a的变异,从而促进未来对当地初级生产和碳循环的理解。洋锋作为典型的中尺度过程,对边缘海的生物过程和渔业有着重要的影响。印度尼西亚海域锋面复杂的时空变异性及其对生物过程的影响仍然知之甚少。本研究旨在通过研究锋面的季节和年际变化及其对浮游植物生物量和初级生产力的关键指标叶绿素-a的影响来解决这一知识空白。该研究确定了南爪哇岛在南方冬季和厄尔尼诺Niño年的高锋面概率。研究发现,风驱动的上升流是浮游植物前缘生成和生长的主要因素。这项研究的结果将提高印度尼西亚海洋区域动态、当地初级生产和碳循环的理论知识,有利于渔业管理和生态系统保护工作。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Seasonal and Interannual Variability of Fronts and Their Impact on Chlorophyll-a in the Indonesian Seas
The spatiotemporal variability of oceanic fronts in the Indonesian seas was investigated using high-resolution satellite observations. The study aimed to understand the underlying mechanism driving these fronts and their impact on chlorophyll-a variability. A high value of frontal probability was found near the coasts of major islands, exhibiting a distinct seasonal cycle with peaks occurrences during austral winter. The distribution variability of chlorophyll-a was generally consistent with the presence of active frontal zones, although a significantly positive relationship between fronts and chlorophyll-a was limited to only some specific areas, e.g., south Java Island and the Celebes Sea. Wind-driven upwelling played a major role in front generation in the Java upwelling region and enhanced frontal activity can promote the growth of phytoplankton, leading to higher chlorophyll-a. Furthermore, the study demonstrated that wind patterns preceded variations in front probability and chlorophyll-a by approximately two months. This lag suggests that the spatiotemporal variability of fronts and chlorophyll-a in this region is primarily influenced by the monsoon system. In addition, the sea surface temperature (SST) simultaneously modulated the chlorophyll-a variability. Negative SST anomalies were typically associated with positive anomalies in front probability the chlorophyll-a in most areas. Notably, the interannual variability of fronts and chlorophyll-a are prominent in the Java upwelling region. During El Niño years, this region experienced an enhanced monsoon, resulting in a negative SST anomaly alongside positive anomalies in front probability and chlorophyll-a. A comprehensive description and underlying dynamics of frontal activity in the Indonesian seas are provided by this study. The findings are helpful to delineate the variability in chlorophyll-a, thereby facilitating the future understanding of local primary production and the carbon cycle. As typical mesoscale processes, oceanic fronts have significant impacts on biological processes and fisheries in marginal seas. The complex spatiotemporal variability of fronts and their effects on biological processes in the Indonesian seas remain poorly understood. This study aimed to address this knowledge gap by investigating the seasonal and interannual variability of fronts and their influence on chlorophyll-a, a key indicator of phytoplankton biomass and primary productivity. The study identified a high frontal probability in south Java Island during austral winter and El Niño years. Wind-driven upwelling was found to be a major factor in front generation and promoting phytoplankton growth. The findings of this study will improve the theoretical knowledge of regional dynamics, local primary production, and the carbon cycle in the Indonesian seas, benefiting fisheries management and ecosystem conservation efforts.
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来源期刊
CiteScore
2.40
自引率
20.00%
发文量
200
审稿时长
4.5 months
期刊介绍: The Journal of Physical Oceanography (JPO) (ISSN: 0022-3670; eISSN: 1520-0485) publishes research related to the physics of the ocean and to processes operating at its boundaries. Observational, theoretical, and modeling studies are all welcome, especially those that focus on elucidating specific physical processes. Papers that investigate interactions with other components of the Earth system (e.g., ocean–atmosphere, physical–biological, and physical–chemical interactions) as well as studies of other fluid systems (e.g., lakes and laboratory tanks) are also invited, as long as their focus is on understanding the ocean or its role in the Earth system.
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