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<shortName>Thermal IR</shortName>
<title>Thermal IR imagery analysis of the Duplin River, Georgia</title>
<creator>
<individualName>
<salutation>Dr.</salutation>
<givenName>Samantha</givenName>
<givenName>B.</givenName>
<surName>Joye</surName>
</individualName>
<organizationName>University of Georgia</organizationName>
<address>
<deliveryPoint>Dept. of Marine Sciences</deliveryPoint>
<deliveryPoint>University of Georgia</deliveryPoint>
<city>Athens</city>
<administrativeArea>Georgia</administrativeArea>
<postalCode>30602-3636</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>mjoye@uga.edu</electronicMailAddress>
<onlineUrl>http://www.marsci.uga.edu/directory/samantha-b-joye</onlineUrl>
</creator>
<metadataProvider><organizationName>Georgia Coastal Ecosystems LTER Project</organizationName>
<address>
<deliveryPoint>Dept. of Marine Sciences</deliveryPoint>
<deliveryPoint>University of Georgia</deliveryPoint>
<city>Athens</city>
<administrativeArea>Georgia</administrativeArea>
<postalCode>30602-3636</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>gcelter@uga.edu</electronicMailAddress>
<onlineUrl>https://gce-lter.marsci.uga.edu/</onlineUrl>
</metadataProvider>
<associatedParty>
<individualName>
<salutation>Dr.</salutation>
<givenName>Samantha</givenName>
<givenName>B.</givenName>
<surName>Joye</surName>
</individualName>
<organizationName>University of Georgia</organizationName>
<address>
<deliveryPoint>Dept. of Marine Sciences</deliveryPoint>
<deliveryPoint>University of Georgia</deliveryPoint>
<city>Athens</city>
<administrativeArea>Georgia</administrativeArea>
<postalCode>30602-3636</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>mjoye@uga.edu</electronicMailAddress>
<onlineUrl>http://www.marsci.uga.edu/directory/samantha-b-joye</onlineUrl>
<role>Principal investigator</role>
<temporalCoverage>
<rangeOfDates>
<beginDate>
<calendarDate>2006-01-01</calendarDate>
</beginDate>
<endDate>
<calendarDate>2006-12-31</calendarDate>
</endDate>
</rangeOfDates>
</temporalCoverage>
</associatedParty>
<pubDate>2026</pubDate>
<abstract>
<section>
<title>Overview</title>
<para>Thermal IR imaging can be used to provide visual identifications and a geospatial location of sites where groundwater discharges into the marsh.  This technique is most successful in summer when temperature differences between warm surface water and colder groundwater are at their maximum (Portnoy et al. 1998).  In 2001, we collected 20 thermal IR images focused on GCE site 10 (Moses Hammock).  Those data clearly showed multiple sites of significant groundwater inflow in the vicinity of this site (Fig. 5).  During the summer of 2006, we acquired a more complete set of thermal IR images of the Duplin River watershed.  The georeferenced images allow us to select sampling sites along the Duplin River with more or less freshwater input to evaluate the effect of differential freshwater input on a variety of marsh processes.</para>
</section>
<section>
<title>Associated GCE LTER research questions</title>
<para>Question 2: How do the spatial and temporal patterns of biogeochemical processes, primary production, community dynamics, decomposition, and disturbance vary across the estuarine landscape, and how do they relate to environmental gradients? (<ulink url="http://gce-lter.marsci.uga.edu/public/research/gce2_q2.asp">more information</ulink>)</para>
</section>
</abstract>
<keywordSet name="organization">
<keyword>LTER</keyword>
<keyword>NSF</keyword>
</keywordSet>
<keywordSet name="place">
<keyword>Duplin River</keyword>
<keyword>Georgia</keyword>
</keywordSet>
<keywordSet name="site">
<keyword>GCE</keyword>
</keywordSet>
<keywordSet name="theme">
<keyword>discharge</keyword>
<keyword>groundwater</keyword>
<keyword>hyperspectral</keyword>
<keyword>remote sensing</keyword>
<keyword>thermal IR</keyword>
</keywordSet>
<coverage>
<geographicCoverage>
<geographicDescription>Overall geographic extent of the research project</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.299522</westBoundingCoordinate>
<eastBoundingCoordinate>-81.195661</eastBoundingCoordinate>
<northBoundingCoordinate>31.546868</northBoundingCoordinate>
<southBoundingCoordinate>31.371003</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<temporalCoverage>
<rangeOfDates>
<beginDate>
<calendarDate>2006-01-01</calendarDate>
</beginDate>
<endDate>
<calendarDate>2006-12-31</calendarDate>
</endDate>
</rangeOfDates>
</temporalCoverage>
</coverage>
<funding>
<section>
<para>National Science Foundation grant number OCE-9982133</para>
</section>
</funding>
<studyAreaDescription>
<descriptor name="hydrology" citableClassificationSystem="false">
<descriptorValue>estuary marsh complex</descriptorValue>
</descriptor>
<coverage>
<geographicCoverage>
<geographicDescription>Hunt Camp - Barrier island/marsh site on western Sapelo Island.  This site is located at the upper reaches of the Duplin River, and is within the Sapelo Island National Estuarine Research Reserve. Existing well fields border small marsh area to northwest, some wells have been installed to south end of hammock where marsh is more extensive and permanent plots are located. Two existing hydrographic sondes and weather stations within this site are operated by SINERR (Hunt Camp dock) and UGAMI (flume dock).</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.295506</westBoundingCoordinate>
<eastBoundingCoordinate>-81.258908</eastBoundingCoordinate>
<northBoundingCoordinate>31.497026</northBoundingCoordinate>
<southBoundingCoordinate>31.462320</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>North Sapelo - High salinity marsh/Sapelo Sound site.  Few or no small creeks, but one large creek is easily accessed. Further upstream upland drainage is affected by culvert at Reynolds' duck pond. Upland is heavily forested. Hydrographic sonde is deployed adjacent to this site attached to a channel marker (under U.S. Coast Guard permit). A huge mud flat is present at the northern tip of Sapelo Island.</geographicDescription>
<boundingCoordinates>
<westBoundingCoordinate>-81.233249</westBoundingCoordinate>
<eastBoundingCoordinate>-81.195661</eastBoundingCoordinate>
<northBoundingCoordinate>31.546868</northBoundingCoordinate>
<southBoundingCoordinate>31.515188</southBoundingCoordinate>
</boundingCoordinates>
</geographicCoverage>
<geographicCoverage>
<geographicDescription>Dean Creek - Doboy Sound/salt marsh site at the southern end of Sapelo Island near Dean Creek and the Sapelo lighthouse.  A few small creeks are present, but a large creek (Dean Creek) is easily accessed. Upland is composed of small hammocks and some constructed causeways, with sand dune complexes east of Dean Creek and extending to the beach. Upper end of the watershed is affected by a culvert at Beach Road and heavy student use of marsh immediately adjacent to culvert. A hydrographic sonde is deployed in Doboy Sound near Commodore Island approximately 1.5km from this site. GCE6 is also the focus of Sapelo Island Microbial Observatory research on microbial diversity  and  genomics (http://simo.marsci.uga.edu)</geographicDescription>
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<westBoundingCoordinate>-81.299522</westBoundingCoordinate>
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<northBoundingCoordinate>31.394072</northBoundingCoordinate>
<southBoundingCoordinate>31.371003</southBoundingCoordinate>
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</coverage>
</studyAreaDescription>
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