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<shortName>Salinity variations across the GCE domain</shortName>
<title>Salinity variations across the GCE domain</title>
<creator>
<individualName>
<salutation>Dr.</salutation>
<givenName>Daniela</givenName>
<surName>Di Iorio</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>
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<electronicMailAddress>daniela@uga.edu</electronicMailAddress>
<onlineUrl>http://www.marsci.uga.edu/directory/daniela-di-iorio</onlineUrl>
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<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>
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<individualName>
<salutation>Dr.</salutation>
<givenName>Daniela</givenName>
<surName>Di Iorio</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>daniela@uga.edu</electronicMailAddress>
<onlineUrl>http://www.marsci.uga.edu/directory/daniela-di-iorio</onlineUrl>
<role>Principal investigator</role>
</associatedParty>
<associatedParty>
<individualName>
<salutation>Dr.</salutation>
<givenName>Jackson</givenName>
<givenName>O.</givenName>
<surName>Blanton</surName>
</individualName>
<organizationName>Skidaway Institute of Oceanography</organizationName>
<address>
<deliveryPoint>10 Ocean Science Circle</deliveryPoint>
<city>Savannah</city>
<administrativeArea>Georgia</administrativeArea>
<postalCode>31411</postalCode>
<country>USA</country>
</address>
<electronicMailAddress>jack.blanton@skio.uga.edu</electronicMailAddress>
<onlineUrl>http://www.skio.peachnet.edu/faculty/blanton.html</onlineUrl>
<role>Co-investigator</role>
</associatedParty>
<pubDate>2026</pubDate>
<abstract>
<section>
<title>Overview</title>
<para>Salinity data collected over the GCE domain were averaged into daily mean quantities for each of the long term monitoring sites. GCE1 in head waters of Sapelo Sound has large changes in salinity that is predominately due to local rain and possibly some groundwater input.  GCE7 located approximately 20 km upstream from GCE9 is almost always fresh except for times of drought conditions.  The remaining stations are strongly influence by freshwater and oceanic input.</para>
<para>River discharge shows a change from a wet period (2003-2005) to drought conditions (2006-2008) with a recovery in spring 2009.  Coastal precipitation is not indicative of river discharge as coastal precipitation is more frequent in summer when river discharge is weaker.  Sea surface height is positively correlated with the along shore winds (Uas) and shows that a 0.4 m rise or fall of oceanic input can occur during the fall and summer season when Nor-easters and southwesterly winds dominate respectively.  Cross-shore winds are not correlated with SSH.</para>
<para>Empirical orthogonal function (EOF) analysis (Figure 1) is used to study the salinity variability using 6 spatially separated measurements (GCE1 and GCE7 are excluded from the analysis).  Two modes explain 94.3% of the salinity variability of which the first mode explains 85.6%.  The temporal variability for this 1st mode is negatively correlated with river discharge with time lags increasing from 1-3 d to 6-8 d as one moved from the Altamaha to the Doboy and Sapelo Sounds respectively.  The coherence shows that variability over yearly time scales dominate.  </para>
<para>For the 2nd mode there is a correlation with the SSH but there is a phase difference between the salinity variations observed in Doboy and Sapelo to those observed in the Altamaha River.  For the Altamaha River, the results indicate that when SSH increases the salinity increases, whereas for Doboy and Sapelo when the SSH increases the salinity decreases.  The coherence seems to show more seasonal time scales for the variability.</para>
<para>The spatial pattern of the station’s eigenvectors, illustrate the degree to which the two modes influence the 6 sites (see Table 1).  The first mode (Figure 2) is uniformly distributed over the whole domain implying that the seasonal discharge is the primary mode of the salinity variability throughout the domain.  For the second mode (Figure 3) Sapelo and Doboy are out of phase with the Altamaha River.  Over these seasonal time scales when SSH increases during Nor’easter storms, the Altamaha river water may be forced through the Intracoastal Waterway or other channels moving freshwater north or may recirculate back in through the Sounds from the ocean.  Further investigation is needed to test this hypothesis.</para>
</section>
<section>
<title>Associated GCE LTER research questions</title>
<para>Area 2: Patterns within the Domain (<ulink url="http://gce-lter.marsci.uga.edu/public/research/gce3_area2.asp">more information</ulink>)</para>
<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="measurement">
<keyword>salinity</keyword>
</keywordSet>
<keywordSet name="organization">
<keyword>LTER</keyword>
<keyword>NSF</keyword>
</keywordSet>
<keywordSet name="place">
<keyword>Altamaha River</keyword>
<keyword>Doboy Sound</keyword>
<keyword>Georgia</keyword>
<keyword>Sapelo Sound</keyword>
</keywordSet>
<keywordSet name="site">
<keyword>GCE</keyword>
</keywordSet>
<keywordSet name="theme">
<keyword>discharge</keyword>
<keyword>precipitation</keyword>
</keywordSet>
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<temporalCoverage>
<ongoing>
<beginDate>
<calendarDate>2006-01-01</calendarDate>
</beginDate>
</ongoing>
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</coverage>
<funding>
<section>
<para>National Science Foundation grant number OCE-0620959</para>
</section>
</funding>
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<descriptor name="hydrology" citableClassificationSystem="false">
<descriptorValue>estuary marsh complex</descriptorValue>
</descriptor>
<coverage>
<geographicCoverage>
<geographicDescription>Eulonia - Transitional salt marsh/upland forest site at the upper reach of the Sapelo River near Eulonia, Georgia. The main marsh area is to the north of the channel where the upland is controlled by DNR. Several small creeks lie within the study area.  Residential development is increasing on the upland areas south of the channel. A hydrographic sonde is deployed within this site attached to a private dock to the south of the main channel near the HW-17 bridge. The sonde is accessed from a dock on a private residence off of highway 17. As of late 2017 the property is owned by Linda Hornby. She asks that we notify her by text about an hour before arriving to service the sondes. There is no reason to go to this property other than for sonde work.</geographicDescription>
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<geographicDescription>Four Mile Island - Low salt marsh/estuary site encompassing the southwestern end of Four Mile Island and the Sapelo River near Sapelo Sound. The large island is totally marsh, with no upland, and no development. Nearby areas, like "Sutherland Bluff", are developing with golf courses. A hydrographic sonde is deployed within this site attached to channel marker 4 (under U.S. Coast Guard permit). Salinity regime is similar to seawater.</geographicDescription>
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<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>
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<geographicDescription>Meridian - Inland marsh and tidal creek site near Meridian, Georgia. The primary marsh site is to the south of the dock in front of the Sapelo Island Visitor Center. Some small creeks and one large creek (Hudson Creek) are present. Upland is heavily forested. Marsh to the north of the dock can be used for additional studies if larger areas are required. Upland to the North is being developed for residential use, so future access is uncertain. The USGS super station site (weather station plus multiple-sensor sonde) is deployed off the ferry dock. Salinity is similar to seawater because there is little freshwater input from the upland.</geographicDescription>
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<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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<geographicDescription>Carrs Island - Freshwater marsh site along the northern bank of Hammersmith Creek at the south end of Carrs Island. Upland area is heavily forested. Northern 3/4 of the island was diked for rice agriculture, but the southern 1/4 is undisturbed. A hydrographic sonde is deployed in the Altamaha River near Hammersmith Creek, adjacent to this site.</geographicDescription>
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<geographicDescription>Alligator Creek - Mid-estuary/salt marsh site on the west side of Friday Cap Creek along the Altamaha River. This is a brackish marsh with salinities around 14 PSU during drought, less than 5 PSU normally. A hydrographic sonde is deployed adjacent to this site in the Altamaha River near Alligator Creek, attached to the US Coast Guard Daymarker 2 pilings.</geographicDescription>
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<geographicDescription>Rockdedundy Island - Lower estuary tidal creek and marsh site at Rockdedundy Island west of Wolf Island. A hydrographic sonde is deployed approximately 2km from this site in the Altamaha River near Rockdedundy Island, attached to the US Coast Guard Daymarker 201 pilings.</geographicDescription>
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