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<front>
<journal-meta>
<journal-id journal-id-type="publisher">BG</journal-id>
<journal-title-group>
<journal-title>Biogeosciences</journal-title>
<abbrev-journal-title abbrev-type="publisher">BG</abbrev-journal-title>
<abbrev-journal-title abbrev-type="nlm-ta">Biogeosciences</abbrev-journal-title>
</journal-title-group>
<issn pub-type="epub">1726-4189</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/bg-10-7207-2013</article-id>
<title-group>
<article-title>Photobleaching as a factor controlling spectral characteristics of chromophoric dissolved organic matter in open ocean</article-title>
</title-group>
<contrib-group><contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Yamashita</surname>
<given-names>Y.</given-names>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Nosaka</surname>
<given-names>Y.</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>Suzuki</surname>
<given-names>K.</given-names>
<ext-link>https://orcid.org/0000-0001-5354-1044</ext-link>
</name>
<xref ref-type="aff" rid="aff1">
<sup>1</sup>
</xref>
<xref ref-type="aff" rid="aff2">
<sup>2</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Ogawa</surname>
<given-names>H.</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>Takahashi</surname>
<given-names>K.</given-names>
</name>
<xref ref-type="aff" rid="aff4">
<sup>4</sup>
</xref>
</contrib>
<contrib contrib-type="author" xlink:type="simple"><name name-style="western"><surname>Saito</surname>
<given-names>H.</given-names>
</name>
<xref ref-type="aff" rid="aff5">
<sup>5</sup>
</xref>
</contrib>
</contrib-group><aff id="aff1">
<label>1</label>
<addr-line>Faculty of Environmental and Earth Science, Hokkaido University, N10, W5, Kita-ku, Sapporo, Hokkaido 060-0810, Japan</addr-line>
</aff>
<aff id="aff2">
<label>2</label>
<addr-line>Graduate School of Environmental Science, Hokkaido University, N10, W5, Kita-ku, Sapporo, Hokkaido 060-0810, Japan</addr-line>
</aff>
<aff id="aff3">
<label>3</label>
<addr-line>Atmosphere and Ocean Research Institute, The University of Tokyo, 5-1-5, Kashiwanoha, Kashiwa-shi, Chiba 277-8564, Japan</addr-line>
</aff>
<aff id="aff4">
<label>4</label>
<addr-line>Graduate School of Agricultural and Life Sciences, The University of Tokyo, 1-1-1, Yayoi, Bunkyo-ku, Tokyo, 113-8657, Japan</addr-line>
</aff>
<aff id="aff5">
<label>5</label>
<addr-line>Tohoku National Fisheries Research Institute, Fisheries Research Agency, 3-27-5 Shinhama-cho, Shiogama 985-0001, Japan</addr-line>
</aff>
<pub-date pub-type="epub">
<day>12</day>
<month>11</month>
<year>2013</year>
</pub-date>
<volume>10</volume>
<issue>11</issue>
<fpage>7207</fpage>
<lpage>7217</lpage>
<permissions>
<copyright-statement>Copyright: &#x000a9; 2013 Y. Yamashita et al.</copyright-statement>
<copyright-year>2013</copyright-year>
<license license-type="open-access">
<license-p>This work is licensed under the Creative Commons Attribution 3.0 Unported License. To view a copy of this licence, visit <ext-link ext-link-type="uri"  xlink:href="https://creativecommons.org/licenses/by/3.0/">https://creativecommons.org/licenses/by/3.0/</ext-link></license-p>
</license>
</permissions>
<self-uri xlink:href="https://bg.copernicus.org/articles/10/7207/2013/bg-10-7207-2013.html">This article is available from https://bg.copernicus.org/articles/10/7207/2013/bg-10-7207-2013.html</self-uri>
<self-uri xlink:href="https://bg.copernicus.org/articles/10/7207/2013/bg-10-7207-2013.pdf">The full text article is available as a PDF file from https://bg.copernicus.org/articles/10/7207/2013/bg-10-7207-2013.pdf</self-uri>
<abstract>
<p>Chromophoric dissolved organic matter (CDOM) ubiquitously occurs in marine
environments and plays a significant role in the marine biogeochemical
cycles. Basin scale distributions of CDOM have recently been surveyed in the
global ocean and indicate that quantity and quality of oceanic CDOM are
mainly controlled by in situ production and photobleaching. However, factors
controlling the spectral parameters of CDOM in the UV region, i.e., spectral
slope of CDOM determined at 275–295 nm (&lt;i&gt;S&lt;/i&gt;&lt;sub&gt;275–295&lt;/sub&gt;) and the ratio of two
spectral slope parameters (&lt;i&gt;S&lt;/i&gt;&lt;sub&gt;R&lt;/sub&gt;); the ratio of &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;275–295&lt;/sub&gt; to
&lt;i&gt;S&lt;/i&gt;&lt;sub&gt;350–400&lt;/sub&gt;, have not been well documented. To evaluate the factor
controlling the spectral characteristics of CDOM in the UV region in the open
ocean, we determined the quantitative and qualitative characteristics of
CDOM in the subarctic and subtropical surface waters (5–300 m) of the
western North Pacific. Absorption coefficients at 320 nm in the subarctic
region were higher than those in the subtropical region throughout surface
waters, suggesting that magnitudes of photobleaching were different between
the two regions. The values of &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;275–295&lt;/sub&gt; and &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;R&lt;/sub&gt; were also higher in
the subtropical region than the subarctic region. The dark microbial
incubation showed biodegradation of DOM little affected &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;275–295&lt;/sub&gt;, but
slightly decreased &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;R&lt;/sub&gt;. On the other hand, increases in &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;275–295&lt;/sub&gt; and
relative stableness of &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;R&lt;/sub&gt; were observed during photo-irradiation
incubations respectively. These experimental results indicated that
photobleaching of CDOM mainly induced qualitative differences in CDOM at UV
region between the subarctic and subtropical surface waters. The results of
this study imply that &lt;i&gt;S&lt;/i&gt;&lt;sub&gt;275–295&lt;/sub&gt; can be used as a tracer of
photochemical history of CDOM in the open ocean.</p>
</abstract>
<counts><page-count count="11"/></counts>
</article-meta>
</front>
<body/>
<back>
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