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<journal-meta>
<journal-id journal-id-type="publisher">EGUsphere</journal-id>
<journal-title-group>
<journal-title>EGUsphere</journal-title>
<abbrev-journal-title abbrev-type="publisher">EGUsphere</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">EGUsphere</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub"></issn>
<publisher><publisher-name>Copernicus Publications</publisher-name>
<publisher-loc>Göttingen, Germany</publisher-loc>
</publisher>
</journal-meta>
<article-meta>
<article-id pub-id-type="doi">10.5194/egusphere-2022-1067</article-id>
<title-group>
<article-title>Seasonal to interannual variabilities of sea&amp;ndash;air CO&lt;sub&gt;2&lt;/sub&gt; exchange across Tropical Maritime Continent indicated by eddy&amp;ndash;permitting coupled OGCM experiment</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Amri</surname>
<given-names>Faisal</given-names>
<ext-link>https://orcid.org/0000-0003-0881-6963</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nakamura</surname>
<given-names>Takashi</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Watanabe</surname>
<given-names>Atsushi</given-names>
</name>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Kartadikaria</surname>
<given-names>Aditiya R.</given-names>
</name>
<xref ref-type="aff" rid="aff3">
<sup>3</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nadaoka</surname>
<given-names>Kazuo</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Transdisciplinary Science and Engineering Department, Tokyo Institute of Technology, Tokyo, Japan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Ocean Policy Research Institute, The Sasakawa Peace Foundation, Japan</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Faculty of Earth Sciences and Technology, Oceanography Research Group, Institut Teknologi Bandung, Bandung, Indonesia</addr-line>
</aff>
<pub-date pub-type="epub">
<day>14</day>
<month>10</month>
<year>2022</year>
</pub-date>
<volume>2022</volume>
<fpage>1</fpage>
<lpage>25</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2022 Faisal Amri et al.</copyright-statement>
<copyright-year>2022</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 4.0 International License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/4.0/">https://creativecommons.org/licenses/by/4.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1067/">This article is available from https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1067/</self-uri>
<self-uri xlink:href="https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1067/egusphere-2022-1067.pdf">The full text article is available as a PDF file from https://egusphere.copernicus.org/preprints/2022/egusphere-2022-1067/egusphere-2022-1067.pdf</self-uri>
<abstract>
<p>&lt;p&gt;The lack of long&amp;ndash;term observational data has limited research on sea&amp;ndash;air CO&lt;sub&gt;2&lt;/sub&gt; exchange variabilities in the Tropical Maritime Continent (TMC). To address the issue, we utilized a three&amp;ndash;dimensional high&amp;ndash;resolution physical&amp;ndash;biogeochemical ocean numerical model and applied it to simulate sea&amp;ndash;air CO&lt;sub&gt;2&lt;/sub&gt; exchange in the region over the last decade (2010&amp;ndash;2019). Some key features like atmospheric CO&lt;sub&gt;2&lt;/sub&gt; source signature and high sea surface pCO&lt;sub&gt;2&lt;/sub&gt; environment inside the TMC were captured by the model. Within the TMC, model results indicated strong CO&lt;sub&gt;2&lt;/sub&gt; degassing along the south of Java associated with the seasonal cycle of the upwelling system. Abundant supply of inorganic carbon during upwelling season and strong wind speed results in CO&lt;sub&gt;2&lt;/sub&gt; degassing that could reach as high as 30 gC m&lt;sup&gt;&amp;ndash;2&lt;/sup&gt; year&lt;sup&gt;&amp;ndash;1&lt;/sup&gt; around the area. In addition to the region acting as a full&amp;ndash;year atmospheric CO&lt;sub&gt;2&lt;/sub&gt; source, the TMC also exhibited interannual modulation in both sea&amp;ndash;air CO&lt;sub&gt;2&lt;/sub&gt; flux and sea surface pCO&lt;sub&gt;2&lt;/sub&gt; which can be related to the El Ni&amp;ntilde;o&amp;ndash;Southern Oscillation (ENSO) and Indian Ocean Dipole (IOD). Large&amp;ndash;scale anomalous strong CO&lt;sub&gt;2&lt;/sub&gt; degassing and high sea surface pCO&lt;sub&gt;2&lt;/sub&gt; from 2015 to 2016 in response to the 2015/2016 El Ni&amp;ntilde;o evolution was observed and dominated by modulation within the TMC. It is further found that modulation of CO&lt;sub&gt;2&lt;/sub&gt; degassing related to IOD were confined along the west of south of Java with a higher magnitude compared with anomalies related to ENSO which shows larger spatial scale but lower in the magnitude. Study conducted here may provide insight about possible variabilities of sea&amp;ndash;air CO&lt;sub&gt;2&lt;/sub&gt; exchange in the area that still poorly represented in many global&amp;ndash;scale modelling and reconstruction efforts.&lt;/p&gt;</p>
</abstract>
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