<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Sheldon, Joan E.</style></author><author><style face="normal" font="default" size="100%">Griffith, Peter C.</style></author><author><style face="normal" font="default" size="100%">Peters, Francesc</style></author><author><style face="normal" font="default" size="100%">Sheldon, Wade M.</style></author><author><style face="normal" font="default" size="100%">Blanton, Jackson O.</style></author><author><style face="normal" font="default" size="100%">Amft, Julie</style></author><author><style face="normal" font="default" size="100%">Pomeroy, Lawrence R.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Southeastern U.S.A. continental shelf respiratory rates revisited</style></title><secondary-title><style face="normal" font="default" size="100%">Biogeochemistry</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">GCE</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2012</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.springerlink.com/openurl.asp?genre=article&amp;id=doi:10.1007/s10533-010-9552-0</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">107</style></volume><pages><style face="normal" font="default" size="100%">501-506</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Respiratory rates on the U. S. southeastern continental shelf have been estimated several times by different investigators, most recently by Jiang et al. (Biogeochemistry 98:101</style></abstract><accession-num><style face="normal" font="default" size="100%">LTER.2012-93228</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Blanton, Jackson O.</style></author><author><style face="normal" font="default" size="100%">Garrett, A.</style></author><author><style face="normal" font="default" size="100%">Bollinger, J.</style></author><author><style face="normal" font="default" size="100%">Hayes, D.</style></author><author><style face="normal" font="default" size="100%">Koffman, L.</style></author><author><style face="normal" font="default" size="100%">Amft, Julie</style></author><author><style face="normal" font="default" size="100%">Moore, Trent C.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Transport and retention of a conservative tracer in an isolated creek</style></title><secondary-title><style face="normal" font="default" size="100%">Estuarine, Coastal and Shelf Science</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">GCE</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2010</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://dx.doi.org/10.1016/j.ecss.2010.01.010</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">87</style></volume><pages><style face="normal" font="default" size="100%">333-345</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">A study of tracer transport and retention in a small tidal creek and marsh system located in the southeastern US was conducted using a three-dimensional hydrodynamic model and data from a dye tracer release. The model simulated tidally driven flow, including inundation and drying out of the marshes and the dispersal of the dye tracer. Flow measurements in the tidal creek showed that the simulations appeared to generally duplicate the tidally driven flow into and out of the tidal creeks and marshes. The dye tracer experiment was conducted to test the hydrodynamic model</style></abstract><accession-num><style face="normal" font="default" size="100%">LTER.2010-93267</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Blanton, Jackson O.</style></author><author><style face="normal" font="default" size="100%">Garrett, A.</style></author><author><style face="normal" font="default" size="100%">Bollinger, J.</style></author><author><style face="normal" font="default" size="100%">Hayes, D.</style></author><author><style face="normal" font="default" size="100%">Koffman, L.</style></author><author><style face="normal" font="default" size="100%">Amft, Julie</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Transport and dispersion of a conservative tracer in coastal waters with large intertidal areas</style></title><secondary-title><style face="normal" font="default" size="100%">Estuaries and Coasts</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">GCE</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.springerlink.com/content/772817k644w71071/</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">32</style></volume><pages><style face="normal" font="default" size="100%">573-592</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">In late December 1991, an accidental release of 5,700 CI of tritiated water (HTO) from the Savannah River Site was transported via site streams into the Savannah River where it was carried downstream to the coastal zone. HTO released into a semitropical Georgia estuary was forced into the tidal marshes surrounding the estuary as well as discharged directly into the Atlantic Ocean. The spreading of HTO was studied with a 3D hydrodynamic model (ALGE) that includes flooding and draining of intertidal areas. Comparisons of model simulations to measured HTO concentration showed that ALGE simulated well the general increase and decrease of HTO as its plume passed a given area. The</style></abstract><accession-num><style face="normal" font="default" size="100%">LTER.2009-93296</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Wenner, E.</style></author><author><style face="normal" font="default" size="100%">Knott, D.</style></author><author><style face="normal" font="default" size="100%">Barans, Charles</style></author><author><style face="normal" font="default" size="100%">Wilde, S.</style></author><author><style face="normal" font="default" size="100%">Blanton, Jackson O.</style></author><author><style face="normal" font="default" size="100%">Amft, Julie</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Key factors influencing the transport of white shrimp (Litopenaeus setiferus) post-larvae into the Ossabaw Sound System, Georgia, USA</style></title><secondary-title><style face="normal" font="default" size="100%">Fisheries Oceanography</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">GCE</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2005</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.blackwell-synergy.com/doi/full/10.1111/j.1365-2419.2005.00328.x</style></url></web-urls></urls><volume><style face="normal" font="default" size="100%">14</style></volume><pages><style face="normal" font="default" size="100%">175-194</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">We examined conditions under which white shrimp (Litopenaeus setiferus) post-larvae enter an estuarine channel receiving high freshwater discharge and one receiving negligible discharge in the Ossabaw Sound system of Georgia, USA, during 1997 and 1998. We used surface nets to collect plankton over several 14-day periods, during which consecutive tows were made at night against the flooding current at stations in the inlet channels. During these sampling periods, additional intensive periods of around-the-clock surface and near-bottom (using a bottom sled) plankton tows were made. Data on oceanographic conditions were obtained from moored instrument arrays and shipboard sampling. We identified three key factors that influenced the densities of post-larval white shrimp in time and space within the Ossabaw inlet system. The first factor was a critical minimum temperature of coastal waters of 27</style></abstract><accession-num><style face="normal" font="default" size="100%">LTER.2005-93422</style></accession-num></record><record><source-app name="Biblio" version="7.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Blanton, Jackson O.</style></author><author><style face="normal" font="default" size="100%">Seim, Harvey E.</style></author><author><style face="normal" font="default" size="100%">Alexander, Clark R</style></author><author><style face="normal" font="default" size="100%">Amft, Julie</style></author><author><style face="normal" font="default" size="100%">Kineke, Gayle</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Transport of salt and suspended sediments in a curving channel of a coastal plain estuary: Satilla River, GA</style></title><secondary-title><style face="normal" font="default" size="100%">Estuarine, Coastal and Shelf Science</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">GCE</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2003</style></year></dates><volume><style face="normal" font="default" size="100%">57</style></volume><pages><style face="normal" font="default" size="100%">993-1006</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">This study describes the transport of salt and suspended sediment in a curving reach of a shallow mesotidal coastal plain estuary. Circulation data revealed a subtidal upstream bottom flow during neap tide, indicating the presence of a gravitational circulation mode throughout the channel. During spring tide, landward bottom flow weakened considerably at the upstream end of the channel and changed to seaward in the middle and downstream areas of the reach, suggesting the importance of tidal pumping. Salt flux near-bottom was landward at both ends of the channel during neap tide. At spring, however, the salt flux diverged along the bottom of the thalweg suggesting that tidal pumping caused a transfer of salt vertically and laterally into the intertidal zone. Thus, landward flux of salt is maintained even in the presence of subtidal seaward flow along the bottom at the downstream end of the channel. Landward bottom stress is greater than seaward stress, preferentially transporting suspended sediments upstream. Compared with salt, however, the weight of the suspended sediments causes less upward transfer of sediments into the intertidal zone. Flood flow carried more suspended sediments landward at the upstream end compared with the downstream end. We speculate that secondary flow in the curving channel picks up increasing amounts of suspended sediments along the sides during flood and adds them to the axial flow in the thalweg. Since the landward flow along the bottom of the thalweg weakens and even reverses during spring tide, there appears to be a complex re-circulation system for sediments re-suspended in curving channels that complicates the picture of a net transport of sediments landward.</style></abstract><accession-num><style face="normal" font="default" size="100%">LTER.2003-93446</style></accession-num></record></records></xml>