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<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:contributor>A. H. Barnard</dc:contributor>
  <dc:contributor>G. Aiken</dc:contributor>
  <dc:contributor>Thomas G. Huntington</dc:contributor>
  <dc:contributor>W. B. Balch</dc:contributor>
  <dc:contributor>H. Xue</dc:contributor>
  <dc:creator>C. S. Roesler</dc:creator>
  <dc:date>2006</dc:date>
  <dc:description>&lt;p&gt;Coastal waters are physically, biogeochemically, and therefore optically complex as a result of the&amp;nbsp;commingling of waters arising from terrestrial, freshwater and marine ecosystems. Separating the&amp;nbsp;influences of these three ecosystems on the optical properties of the resulting mixture is challenging,&amp;nbsp;particularly given the variability within each. The longterm goals of this project are twofold: (1) to&amp;nbsp;investigate the feasibility of identifying landuse changes using inwater optical observations, (2) to&amp;nbsp;quantify the input of terrestrial organic carbon into the coastal marine environment. Our approach is to&amp;nbsp;study the Penobscot River Watershed in Maine, from its many tributaries and subwatersheds into the&amp;nbsp;main branch of the Penobscot River, Penobscot Bay and ultimately into the coastal waters of the&amp;nbsp;Eastern Maine Coastal Current. The first step towards this goal is to define optical signatures&amp;nbsp;associated with specific watershed land coverages measured at the source (optical proxies). The next&amp;nbsp;step is to track those proxies from their respective sources to the coast, characterizing the dilution and&amp;nbsp;transformative processes. Using analyses of discrete samples collected monthly from the&amp;nbsp;subwatersheds, we have quantified optical proxies for both dissolved and particulate organic carbon,&amp;nbsp;particulate carbon to nitrogen ratios and fluorophores unique to certain land coverages (e.g. wetlands,&amp;nbsp;residence ponds, lumber mills, agriculture). We apply these proxies to in situ optical observations&amp;nbsp;retrieved from sensors moored within the lower river and upper estuary to quantify the temporal&amp;nbsp;patterns in the biogeochemical properties. To date we have approximately 2 years of observations,&amp;nbsp;including the wettest year on record for the last century in this region. The proxies associated with the&amp;nbsp;dissolved fraction are the most robust and provide signatures for both land coverage and for organic&amp;nbsp;carbon concentration. Those associated with particles are robust proxies for carbon but are less&amp;nbsp;informative about land coverage. &lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:language>en</dc:language>
  <dc:publisher>The Oceanography Society</dc:publisher>
  <dc:title>Using optical proxies for biogeochemical properties to study land coverage and terrestrial inputs of organic carbon into coastal waters from the Penobscot Watershed to the Gulf of Maine </dc:title>
  <dc:type>text</dc:type>
</oai_dc:dc>