Net Community Production Variability in Response to Changing Upwelling Intensity Before and After a Typhoon in the Southern East China Sea

IF 3.4 2区 地球科学 Q1 OCEANOGRAPHY
Kai-Jung Kao, Wei-Jen Huang, Yonghui Gao, Hsiao-Chun Tseng, Veran Weerathunga, Fei-Ling Yuan, Gwo-Ching Gong, Wen-Chen Chou
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引用次数: 0

Abstract

Continental shelves contribute approximately 30% of the ocean's net community production (NCP), significantly influencing the global oceanic carbon cycle. However, the regulation of NCP variability on continental shelves by physical processes, such as upwelling remains poorly understood. High spatial resolution mixed-layer O2/Ar-NCP measurements were conducted using equilibrator inlet mass spectrometry in the southern East China Sea (ECS) before (6–9 July 2018) and after (13–17 July 2018) Typhoon “Maria.” The relationship between biological N2O and O2 in the water column was used to correct for the impact of upwelling and vertical mixing on O2/Ar-NCP measurements (refined NCP, RNCP). Our study revealed that the periodic upwelling in the southern ECS relaxed before the typhoon and intensified afterward. This change in upwelling conditions corresponded to an increase in RNCP at the southern ECS from an average of 17 ± 11 mmol C m−2 d−1 to 99 ± 25 mmol C m−2 d−1. The N2O-based correction improved the estimation of O2/Ar-NCP measurements in upwelling regions. Without this correction, NCP values were underestimated, with the degree of underestimation increasing from 18 ± 9 to 80 ± 17 mmol C m−2 d−1 as upwelling intensified during our study period. We suggest that the upwelling regions within the mixed layer were net autotrophic before and after the typhoon, yielding valuable information for refining fishery models.

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台风前后东海净群落生产变率对上升流强度变化的响应
大陆架贡献了大约30%的海洋净群落产量(NCP),显著影响着全球海洋碳循环。然而,物理过程(如上升流)对大陆架上NCP变率的调节仍然知之甚少。在台风“玛丽亚”之前(2018年7月6日至9日)和之后(2018年7月13日至17日),利用平衡器入口质谱法在东海南部(ECS)进行了高空间分辨率混合层O2/Ar-NCP测量。利用水柱中生物N2O和O2的关系来校正上升流和垂直混合对O2/Ar-NCP测量(精制NCP, RNCP)的影响。研究结果表明,台风前东太平洋南部的周期性上升流有所减弱,台风后则有所增强。这种上升流条件的变化对应于南部ECS的RNCP从平均17±11 mmol C m−2 d−1增加到99±25 mmol C m−2 d−1。基于n2o的校正改进了上升流区O2/Ar-NCP测量值的估计。如果没有这种校正,NCP值被低估了,在我们的研究期间,随着上升流的加剧,NCP值的低估程度从18±9增加到80±17 mmol C m - 2 d - 1。我们认为,在台风前后,混合层内的上升流区域是净自养的,为完善渔业模型提供了有价值的信息。
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来源期刊
Journal of Geophysical Research-Oceans
Journal of Geophysical Research-Oceans Earth and Planetary Sciences-Oceanography
CiteScore
7.00
自引率
13.90%
发文量
429
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