南海海洋浮游生物生态系统对夏季马登-朱利安涛动的季内响应:模型研究

IF 3.8 3区 地球科学 Q1 OCEANOGRAPHY
Hengye Ren , Wenfang Lu , Wupeng Xiao , Qing Zhu , Canbo Xiao , Zhigang Lai
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引用次数: 0

摘要

在夏季,马登-朱利安涛动(MJO)对中国南海(SCS)的季内变化有很大影响。以往的研究揭示了 MJO 对表层叶绿素(Chl)浓度的影响,但 MJO 对生态系统结构和功能的影响仍有待探索。在此,我们通过分析 2010 年至 2014 年巡航收集的浮游植物色素数据,研究了海洋生态系统对 MJO 的响应。结果表明,多云涛动对南中国海海盆上层 50 米浮游植物尺度等级(PSCs)结构的影响很大。为了进一步探讨生态系统对 MJO 的响应,我们利用经过良好校准的南中国海物理-生物地球化学模式(ROMS-CoSiNE),在有 MJO 胁迫和无 MJO 胁迫的情况下进行了数值实验。我们的模型表明,MJO 诱导的深层混合和上升流增加了上层的营养物质,提高了 Chl 浓度,纳米浮游植物的比例较高(15%),而微浮游植物的比例较低(-20%)。此外,MJO 强制模式实验显示初级生产量(56%)和出口生产量(23%)大幅增加,导致 e 比率明显下降。e-比率的下降不能归因于 PSCs 的变化,而可以用初级生产和出口生产之间的时滞来解释。上升流和混合等物理过程延长了这一滞后期,从而减缓了颗粒的下沉。我们的研究结果强调了 MJO 在调节季内尺度生态系统中的重要作用,从而提高了我们对 SCS 生态系统非稳定动态的理解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Intraseasonal response of marine planktonic ecosystem to summertime Madden-Julian Oscillation in the South China Sea: A model study

In summer, the Madden-Julian Oscillation (MJO) greatly influences the intraseasonal variability of the South China Sea (SCS). Previous studies have revealed MJO effects on surface chlorophyll (Chl) concentration, but the impact of the MJO on the ecosystem's structure and functionality remains unexplored. Here, we investigated the marine ecosystem response to the MJO by analyzing phytoplankton pigment data collected in cruises from 2010 to 2014. The results indicated the strong influence of the MJO on the structure of phytoplankton size classes (PSCs) in the upper 50 m of the SCS basin. To further explore the ecosystem's response to MJO, we utilized a well-calibrated physical-biogeochemical model (ROMS-CoSiNE) of the SCS to conduct numerical experiments with and without MJO forcings. Our model demonstrated that MJO-induced deep mixing and upwelling increased nutrients in the upper layer, increasing the Chl concentration with a higher proportion of nanophytoplankton (15 %) and a lower proportion of picophytoplankton (−20 %). Moreover, The MJO-forced model experiment exhibited a substantial enhancement in primary production (56 %) and export production (23 %), resulting in a notable decrease in the e-ratio. This reduction in the e-ratio cannot be attributed to changes in PSCs but can be explained by the time lag between primary and export production. This lag was prolonged by the physical processes of upwelling and mixing, which slows down the particle sinking. Our results emphasize the important role of MJO in regulating the ecosystem at intraseasonal scale, thus improving our comprehension of the nonsteady dynamics of ecosystems in the SCS.

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来源期刊
Progress in Oceanography
Progress in Oceanography 地学-海洋学
CiteScore
7.20
自引率
4.90%
发文量
138
审稿时长
3 months
期刊介绍: Progress in Oceanography publishes the longer, more comprehensive papers that most oceanographers feel are necessary, on occasion, to do justice to their work. Contributions are generally either a review of an aspect of oceanography or a treatise on an expanding oceanographic subject. The articles cover the entire spectrum of disciplines within the science of oceanography. Occasionally volumes are devoted to collections of papers and conference proceedings of exceptional interest. Essential reading for all oceanographers.
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