{"refrec":{"BRefID":355381,"RR":"<b>Ouyang, Z.; Collins, A.; Li, Y.; Qi, D.; Arrigo, K.R.; Zhuang, Y.; Nishino, S.; Humphreys, M.P.; Kosugi, N.; Murata, A.; Kirchmann, D.L.; Chen, L.; Chen, J.; Cai, W.-J.</b> (2022). Seasonal water mass evolution and non‐redfield dynamics enhance CO<sub>2</sub> uptake in the Chukchi Sea. <i>JGR: Oceans 127(8)</i>: e2021JC018326. <a href=\"https://dx.doi.org/10.1029/2021jc018326\" target=\"_blank\">https://dx.doi.org/10.1029/2021jc018326</a>","BEntID":353094,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>JGR: Oceans 127(8)</i>: e2021JC018326. <a href=\"https://dx.doi.org/10.1029/2021jc018326\" target=\"_blank\">https://dx.doi.org/10.1029/2021jc018326</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Ouyang, Z.; Collins, A.; Li, Y.; Qi, D.; Arrigo, K.R.; Zhuang, Y.; Nishino, S.; Humphreys, M.P.; Kosugi, N.; Murata, A.; Kirchmann, D.L.; Chen, L.; Chen, J.; Cai, W.-J.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Ouyang, Z. <i>et al.</i>","Englishabstract":"<p>    The Chukchi Sea is an increasing CO<sub>2</sub> sink driven by rapidclimate changes. Understanding the seasonal variation of air-sea CO    <sub>2</sub> exchange and the underlying mechanisms of biogeochemical    dynamics is important for predicting impacts of climate change on and    feedbacks by the ocean. Here, we present a unique data set of underway sea    surface partial pressure of CO<sub>2</sub> (<em>p</em>CO<sub>2</sub>) and    discrete samples of biogeochemical properties collected in five consecutivecruises in 2014 and examine the seasonal variations in air-sea CO    <sub>2</sub> flux and net community production (NCP). We found that thermaland non-thermal effects have different impacts on sea surface <em>p</em>CO    <sub>2</sub> and thus the air-sea CO<sub>2</sub> flux in different water    masses. The Bering summer water combined with meltwater has a significantly    greater atmospheric CO<sub>2</sub> uptake potential than that of the    Alaskan Coastal Water in the southern Chukchi Sea in summer, due to    stronger biological CO<sub>2</sub> removal and a weaker thermal effect. By    analyzing the seasonal drawdown of dissolved inorganic carbon (DIC) and    nutrients, we found that DIC-based NCP was higher than nitrate-based NCP by    66%–84% and attributable to partially decoupled C and N uptake because of a    variable phytoplankton stoichiometry. A box model with a non-Redfield C:N    uptake ratio can adequately reproduce observed <em>p</em>CO<sub>2</sub> and    DIC, which reveals that, during the intensive growing season (late spring    to early summer), 30%–46% CO<sub>2</sub> uptake in the Chukchi Sea was    supported by a flexible stoichiometry of phytoplankton. These findings have    important ramification for forecasting the responses of CO<sub>2</sub>    uptake of the Chukchi ecosystem to climate change.</p>","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Seasonal water mass evolution and non‐redfield dynamics enhance CO<sub>2</sub> uptake in the Chukchi Sea","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-10 01:32:45.791943","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2022,"MonPub":null,"DateUpdate":"2022-09-13","DateCreate":"2022-09-13","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000837052800001","VABBcode":null,"OpenAcc":1,"DOI":"10.1029/2021jc018326"},"refs":null,"anarec":{"AnaID":355381,"PubliDate":2022,"Pagination":"e2021JC018326","XtraPublOfAnaID":null,"ISBN":null,"Volume":"127","Issue":"8","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":272092,"SerRR":"Journal of Geophysical Research-Oceans. 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