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北印度洋大气输入和初级生产力的近期变化。

Recent changes in atmospheric input and primary productivity in the north Indian Ocean.

作者信息

Kuttippurath J, Maishal S, Anjaneyan P, Sunanda N, Chakraborty Kunal

机构信息

CORAL, Indian Institute of Technology Kharagpur, Kharagpur 721302, India.

Indian National Centre for Ocean Information Services, Ministry of Earth Sciences, Hyderabad 500090, India.

出版信息

Heliyon. 2023 Jul 5;9(7):e17940. doi: 10.1016/j.heliyon.2023.e17940. eCollection 2023 Jul.

DOI:10.1016/j.heliyon.2023.e17940
PMID:37483689
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC10362137/
Abstract

Global oceanic regions are rapidly changing in terms of their temperature, oxygen, heat content, salinity and biogeochemistry. Since the biogeochemistry of the oceans is important and pivotal for global food production, and a major part of the world population relies on marine resources for their daily life and livelihood, it is imperative to monitor and find the spatio-temporal changes in the primary productivity of oceans. Here, we estimate the changes in Chlorophyll-a (Chl-a) and Net Primary Productivity (NPP) in the north Indian Ocean (NIO) basins of Bay of Bengal and Arabian Sea for the period 1998-2019. We find a substantial reduction of NPP in NIO since 1998 (-0.048 mg m day yr) and the increase in sea surface temperature (SST) (+0.02 °C yr) is the primary driver of this change. Furthermore, there is a significant (10-20%) change in the air mass or dust transport to NIO from the period Decade 1 (1998-2008) to Decade 2 (2009-2019). This change in air mass trajectories has also altered NPP in both basins through the changes in nutrient input and associated biogeochemistry. Henceforth, this study cautions the changes in primary productivity of NIO, and suggests regular assessments and continuous monitoring of the physical and biological processes from a perspective of food security and ecosystem dynamics.

摘要

全球海洋区域在温度、氧气、热量含量、盐度和生物地球化学方面正在迅速变化。由于海洋的生物地球化学对全球粮食生产至关重要且具有关键作用,并且世界上很大一部分人口的日常生活和生计依赖海洋资源,因此监测并找出海洋初级生产力的时空变化势在必行。在此,我们估算了1998 - 2019年期间孟加拉湾和阿拉伯海的北印度洋(NIO)盆地中叶绿素a(Chl-a)和净初级生产力(NPP)的变化。我们发现自1998年以来北印度洋的净初级生产力大幅下降(-0.048毫克·米⁻²·天⁻¹·年⁻¹),而海面温度的升高(+0.02℃·年⁻¹)是这一变化的主要驱动因素。此外,从十年1(1998 - 2008年)到十年2(2009 - 2019年),输送到北印度洋的气团或沙尘传输发生了显著(10 - 20%)变化。气团轨迹的这种变化也通过营养物质输入和相关生物地球化学的变化改变了两个盆地的净初级生产力。因此,本研究警示了北印度洋初级生产力的变化,并建议从粮食安全和生态系统动态的角度对物理和生物过程进行定期评估和持续监测。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2df1/10362137/401716d85077/gr9.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2df1/10362137/401716d85077/gr9.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2df1/10362137/9c3776c362c3/gr1.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2df1/10362137/a61bb76cea2f/gr2.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2df1/10362137/3b918001d3a8/gr3.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2df1/10362137/04196b16fa69/gr4.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2df1/10362137/715fb634793e/gr5.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2df1/10362137/776689fbabe7/gr6.jpg
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https://cdn.ncbi.nlm.nih.gov/pmc/blobs/2df1/10362137/401716d85077/gr9.jpg

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本文引用的文献

1
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2
Spatio-temporal changes of winter and spring phytoplankton blooms in Arabian sea during the period 1997-2020.1997-2020 年期间阿拉伯海冬春季节浮游植物水华的时空变化。
J Environ Manage. 2023 Apr 15;332:117435. doi: 10.1016/j.jenvman.2023.117435. Epub 2023 Feb 4.
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Ecosystem state change in the Arabian Sea fuelled by the recent loss of snow over the Himalayan-Tibetan Plateau region.
由于喜马拉雅-青藏高原地区近年来积雪消融,阿拉伯海的生态系统状态发生了变化。
Sci Rep. 2020 May 4;10(1):7422. doi: 10.1038/s41598-020-64360-2.
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Nature. 2006 Dec 7;444(7120):752-5. doi: 10.1038/nature05317.
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Global iron connections between desert dust, ocean biogeochemistry, and climate.沙漠尘埃、海洋生物地球化学与气候之间的全球铁联系。
Science. 2005 Apr 1;308(5718):67-71. doi: 10.1126/science.1105959.