Rising surface ocean dissolved inorganic carbon at the Hawaii Ocean Time-series site
Surface ocean dissolved inorganic carbon (DIC) and titration alkalinity have been measured for 7 years as a part of the Hawaii Ocean Time-series (HOT) program. The time-series data set displays an interannual increase in the inventory of surface ocean DIC which we interpret as a response to increasi...
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| Veröffentlicht in: | Marine chemistry 1998, Vol.60 (1), p.33-47 |
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| container_title | Marine chemistry |
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| creator | Winn, Christopher D. Li, Yuan-Hui Mackenzie, Fred T. Karl, David M. |
| description | Surface ocean dissolved inorganic carbon (DIC) and titration alkalinity have been measured for 7 years as a part of the Hawaii Ocean Time-series (HOT) program. The time-series data set displays an interannual increase in the inventory of surface ocean DIC which we interpret as a response to increasing atmospheric carbon dioxide concentrations. The rate of increase in surface ocean DIC at the open ocean HOT site is approximately 1
μmol kg
−1 yr
−1 with a 95% confidence interval of 0.72 to 1.37
μmol kg
−1 yr
−1. This accumulation rate is consistent with the rate of increase predicted from the rise in boundary layer
p
CO
2
. |
| doi_str_mv | 10.1016/S0304-4203(97)00085-6 |
| format | Article |
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μmol kg
−1 yr
−1 with a 95% confidence interval of 0.72 to 1.37
μmol kg
−1 yr
−1. This accumulation rate is consistent with the rate of increase predicted from the rise in boundary layer
p
CO
2
.</description><identifier>ISSN: 0304-4203</identifier><identifier>EISSN: 1872-7581</identifier><identifier>DOI: 10.1016/S0304-4203(97)00085-6</identifier><identifier>CODEN: MRCHBD</identifier><language>eng</language><publisher>Amsterdam: Elsevier B.V</publisher><subject>carbon cycle ; dissolved inorganic carbon ; Earth sciences ; Earth, ocean, space ; Exact sciences and technology ; External geophysics ; Geochemistry ; Marine ; Mineralogy ; North Pacific subtropical gyre ; Physical and chemical properties of sea water ; Physics of the oceans ; Silicates ; Water geochemistry</subject><ispartof>Marine chemistry, 1998, Vol.60 (1), p.33-47</ispartof><rights>1998 Elsevier Science B.V.</rights><rights>1998 INIST-CNRS</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-a584t-9a9f9178384c8f42c4590a4354528ecde20b1b9104bfc19368167d356d7273683</citedby><cites>FETCH-LOGICAL-a584t-9a9f9178384c8f42c4590a4354528ecde20b1b9104bfc19368167d356d7273683</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktohtml>$$Uhttps://dx.doi.org/10.1016/S0304-4203(97)00085-6$$EHTML$$P50$$Gelsevier$$H</linktohtml><link.rule.ids>309,310,314,780,784,789,790,3550,4024,4050,4051,23930,23931,25140,27923,27924,27925,45995</link.rule.ids><backlink>$$Uhttp://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=2267867$$DView record in Pascal Francis$$Hfree_for_read</backlink></links><search><creatorcontrib>Winn, Christopher D.</creatorcontrib><creatorcontrib>Li, Yuan-Hui</creatorcontrib><creatorcontrib>Mackenzie, Fred T.</creatorcontrib><creatorcontrib>Karl, David M.</creatorcontrib><title>Rising surface ocean dissolved inorganic carbon at the Hawaii Ocean Time-series site</title><title>Marine chemistry</title><description>Surface ocean dissolved inorganic carbon (DIC) and titration alkalinity have been measured for 7 years as a part of the Hawaii Ocean Time-series (HOT) program. The time-series data set displays an interannual increase in the inventory of surface ocean DIC which we interpret as a response to increasing atmospheric carbon dioxide concentrations. The rate of increase in surface ocean DIC at the open ocean HOT site is approximately 1
μmol kg
−1 yr
−1 with a 95% confidence interval of 0.72 to 1.37
μmol kg
−1 yr
−1. This accumulation rate is consistent with the rate of increase predicted from the rise in boundary layer
p
CO
2
.</description><subject>carbon cycle</subject><subject>dissolved inorganic carbon</subject><subject>Earth sciences</subject><subject>Earth, ocean, space</subject><subject>Exact sciences and technology</subject><subject>External geophysics</subject><subject>Geochemistry</subject><subject>Marine</subject><subject>Mineralogy</subject><subject>North Pacific subtropical gyre</subject><subject>Physical and chemical properties of sea water</subject><subject>Physics of the oceans</subject><subject>Silicates</subject><subject>Water geochemistry</subject><issn>0304-4203</issn><issn>1872-7581</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>1998</creationdate><recordtype>article</recordtype><recordid>eNqFkMtKxEAQRRtRcHx8gtALEV1Eu5N-rkTEFwiCjuump1PRkkyiXRnFvzczI25dFQXn3qIOYwdSnEohzdmTqIQqVCmqY29PhBBOF2aDTaSzZWG1k5ts8odssx2itxEylfYTNn1Ewu6F0yI3MQHvE8SO10jUt59Qc-z6_BI7TDzFPOs7Hgc-vAK_jV8RkT-s8CnOoSDICMQJB9hjW01sCfZ_5y57vr6aXt4W9w83d5cX90XUTg2Fj77x0rrKqeQaVSalvYiq0kqXDlINpZjJmZdCzZokfWWcNLautKltacet2mVH69733H8sgIYwR0rQtrGDfkFBGmWFVXYE9RpMuSfK0IT3jPOYv4MUYekwrByGpaDgbVg5DGbMHf4eiJRi2-TYJaS_cFka68yy_nyNwfjsJ0IOlBC6BDVmSEOoe_zn0A-XT4Qn</recordid><startdate>1998</startdate><enddate>1998</enddate><creator>Winn, Christopher D.</creator><creator>Li, Yuan-Hui</creator><creator>Mackenzie, Fred T.</creator><creator>Karl, David M.</creator><general>Elsevier B.V</general><general>Elsevier Science</general><scope>IQODW</scope><scope>AAYXX</scope><scope>CITATION</scope><scope>7TN</scope><scope>F1W</scope><scope>H96</scope><scope>L.G</scope></search><sort><creationdate>1998</creationdate><title>Rising surface ocean dissolved inorganic carbon at the Hawaii Ocean Time-series site</title><author>Winn, Christopher D. ; Li, Yuan-Hui ; Mackenzie, Fred T. ; Karl, David M.</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-a584t-9a9f9178384c8f42c4590a4354528ecde20b1b9104bfc19368167d356d7273683</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>1998</creationdate><topic>carbon cycle</topic><topic>dissolved inorganic carbon</topic><topic>Earth sciences</topic><topic>Earth, ocean, space</topic><topic>Exact sciences and technology</topic><topic>External geophysics</topic><topic>Geochemistry</topic><topic>Marine</topic><topic>Mineralogy</topic><topic>North Pacific subtropical gyre</topic><topic>Physical and chemical properties of sea water</topic><topic>Physics of the oceans</topic><topic>Silicates</topic><topic>Water geochemistry</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Winn, Christopher D.</creatorcontrib><creatorcontrib>Li, Yuan-Hui</creatorcontrib><creatorcontrib>Mackenzie, Fred T.</creatorcontrib><creatorcontrib>Karl, David M.</creatorcontrib><collection>Pascal-Francis</collection><collection>CrossRef</collection><collection>Oceanic Abstracts</collection><collection>ASFA: Aquatic Sciences and Fisheries Abstracts</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources</collection><collection>Aquatic Science & Fisheries Abstracts (ASFA) Professional</collection><jtitle>Marine chemistry</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Winn, Christopher D.</au><au>Li, Yuan-Hui</au><au>Mackenzie, Fred T.</au><au>Karl, David M.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Rising surface ocean dissolved inorganic carbon at the Hawaii Ocean Time-series site</atitle><jtitle>Marine chemistry</jtitle><date>1998</date><risdate>1998</risdate><volume>60</volume><issue>1</issue><spage>33</spage><epage>47</epage><pages>33-47</pages><issn>0304-4203</issn><eissn>1872-7581</eissn><coden>MRCHBD</coden><abstract>Surface ocean dissolved inorganic carbon (DIC) and titration alkalinity have been measured for 7 years as a part of the Hawaii Ocean Time-series (HOT) program. The time-series data set displays an interannual increase in the inventory of surface ocean DIC which we interpret as a response to increasing atmospheric carbon dioxide concentrations. The rate of increase in surface ocean DIC at the open ocean HOT site is approximately 1
μmol kg
−1 yr
−1 with a 95% confidence interval of 0.72 to 1.37
μmol kg
−1 yr
−1. This accumulation rate is consistent with the rate of increase predicted from the rise in boundary layer
p
CO
2
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| ispartof | Marine chemistry, 1998, Vol.60 (1), p.33-47 |
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| language | eng |
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| source | Access via ScienceDirect (Elsevier) |
| subjects | carbon cycle dissolved inorganic carbon Earth sciences Earth, ocean, space Exact sciences and technology External geophysics Geochemistry Marine Mineralogy North Pacific subtropical gyre Physical and chemical properties of sea water Physics of the oceans Silicates Water geochemistry |
| title | Rising surface ocean dissolved inorganic carbon at the Hawaii Ocean Time-series site |
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