{"id":34862,"date":"2024-11-19T10:11:28","date_gmt":"2024-11-19T02:11:28","guid":{"rendered":"https:\/\/www.oc.ntu.edu.tw\/?p=34862"},"modified":"2024-11-20T09:37:16","modified_gmt":"2024-11-20T01:37:16","slug":"seasonal-variation-of-co2-air-sea-flux-and-effects-of-warming-in-the-kuroshio-current-of-the-east-china-sea","status":"publish","type":"post","link":"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/34862\/","title":{"rendered":"Seasonal Variation of CO2 air-sea flux and Effects of Warming in the Kuroshio Current of the East China Sea"},"content":{"rendered":"\n<p><a><strong>Shou-En Tsao, Po-Yen Shen, Chun-Mao Tseng<sup>*<\/sup><\/strong><\/a><\/p>\n\n\n\n<p>The partial pressure of CO<sub>2<\/sub> (pCO<sub>2<\/sub>) and CO<sub>2<\/sub> air-sea flux exhibit marked spatial and temporal variability across ocean margins, reflecting the complex interplay of regional environmental processes. Understanding these variations is fundamental to comprehending the global carbon cycle and predicting how oceans may respond to climate change.<\/p>\n\n\n\n<p>A recent study published in Marine Chemistry documented seasonal CO<sub>2<\/sub> flux dynamics within the Kuroshio Current of the East China Sea (ECS), particularly in the context of warming oceans. The research reveals that the Kuroshio functions as a net CO<sub>2<\/sub> sink, with an annual uptake of approximately 1.3 mol C m<sup>\u22122<\/sup> yr<sup>\u22121<\/sup>\u2014less than the ECS shelf\u2019s higher rate of ~1.8 mol C m<sup>\u22122<\/sup> yr<sup>\u22121<\/sup>. Seasonal fluxes are thermally driven, making the Kuroshio a strong CO<sub>2<\/sub> sink in winter and transitioning to a weak source or net-neutral state in summer, contrasting with the biologically and physically driven fluxes of the ECS shelf. This highlights the contrasting controls on carbon dynamics within marginal seas, with tropical and subtropical regions, like the Kuroshio, being particularly vulnerable to the effects of climate warming.<\/p>\n\n\n\n<p>Looking forward, ongoing warming trends could disrupt the seasonal balance of CO<sub>2<\/sub> fluxes, leading to shifts in interannual carbon dynamics. and impacting carbon storage potential and removal feasibilitiess in marginal seas. Long-term monitoring of dynamic systems like the Kuroshio Current is essential to understanding their evolving role in the global carbon cycle under climate change.<\/p>\n\n\n\n<p>Share Link: <a href=\"https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0304420324001208 \">https:\/\/www.sciencedirect.com\/science\/article\/pii\/S0304420324001208 <\/a><\/p>\n\n\n\n<p>S.-E. Tsao, P.-Y. Shen, <strong><u>C.-M. Tseng*<\/u><\/strong><em> <\/em>(2024) Seasonal variation of CO<sub>2<\/sub> air-sea flux and effects of warming in the Kuroshio Current of the East China Sea, Marine Chemistry, 267, 104469, https:\/\/doi.org\/10.1016\/j.marchem.2024.104469.<\/p>\n\n\n\n<figure class=\"wp-block-image size-full\"><img fetchpriority=\"high\" decoding=\"async\" width=\"884\" height=\"489\" src=\"https:\/\/www.oc.ntu.edu.tw\/wp-content\/uploads\/2024\/11\/image001.png\" alt=\"\" class=\"wp-image-34864\" srcset=\"https:\/\/www.oc.ntu.edu.tw\/wp-content\/uploads\/2024\/11\/image001.png 884w, https:\/\/www.oc.ntu.edu.tw\/wp-content\/uploads\/2024\/11\/image001-768x425.png 768w\" sizes=\"(max-width: 884px) 100vw, 884px\" \/><\/figure>\n\n\n\n<p>A conceptual comparison of seasonal mean pCO<sub>2<\/sub>, CO fluxes, and their controlling mechanisms between (a) the East China Sea (ECS) shelf and (b) the Kuroshio.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Shou-En Tsao, Po-Yen Shen, Chun-Mao Tseng* The partial pressure of CO2 (pCO2) and CO2 air-sea flux exhibit marked spatial and temporal variability across ocean margins, reflecting the complex interplay of regional environmental processes. Understanding these variations is fundamental to comprehending the global carbon cycle and predicting how oceans may respond to climate change. A recent [&hellip;]<\/p>\n","protected":false},"author":15,"featured_media":34865,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_acf_changed":false,"footnotes":""},"categories":[95,119],"tags":[],"class_list":["post-34862","post","type-post","status-publish","format-standard","has-post-thumbnail","hentry","category-news-en","category-research-highlights"],"acf":[],"yoast_head":"<!-- This site is optimized with the Yoast SEO plugin v25.3 - https:\/\/yoast.com\/wordpress\/plugins\/seo\/ -->\n<title>Seasonal Variation of CO2 air-sea flux and Effects of Warming in the Kuroshio Current of the East China Sea - Institute of Oceanography, NTU<\/title>\n<meta name=\"robots\" content=\"index, follow, max-snippet:-1, max-image-preview:large, max-video-preview:-1\" \/>\n<link rel=\"canonical\" href=\"https:\/\/www.oc.ntu.edu.tw\/en\/research-highlights\/34862\/\" \/>\n<meta property=\"og:locale\" content=\"en_US\" \/>\n<meta property=\"og:type\" content=\"article\" \/>\n<meta property=\"og:title\" content=\"Seasonal Variation of CO2 air-sea flux and Effects of Warming in the Kuroshio Current of the East China Sea - Institute of Oceanography, NTU\" \/>\n<meta property=\"og:description\" content=\"Shou-En Tsao, Po-Yen Shen, Chun-Mao Tseng* The partial pressure of CO2 (pCO2) and CO2 air-sea flux exhibit marked spatial and temporal variability across ocean margins, reflecting the complex interplay of regional environmental processes. Understanding these variations is fundamental to comprehending the global carbon cycle and predicting how oceans may respond to climate change. 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