<?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%">Moore, Willard S.</style></author><author><style face="normal" font="default" size="100%">Krest, James</style></author><author><style face="normal" font="default" size="100%">Taylor, Glenn</style></author><author><style face="normal" font="default" size="100%">Roggenstein, Edward</style></author><author><style face="normal" font="default" size="100%">Joye, Samantha B.</style></author><author><style face="normal" font="default" size="100%">Lee, Rosalynn Y.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Thermal evidence of water exchange through a coastal aquifer: implications for nutrient fluxes</style></title><secondary-title><style face="normal" font="default" size="100%">Geophysical Research Letters</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%">2002</style></year></dates><volume><style face="normal" font="default" size="100%">29</style></volume><pages><style face="normal" font="default" size="100%">1704</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">We report the discovery of a semi-confined, high permeability zone (HPZ) 2 meters below the sea bed where exchanges between coastal aquifers and the ocean occur. A temperature probe placed in the HPZ recorded a 1</style></abstract><issue><style face="normal" font="default" size="100%">14</style></issue><accession-num><style face="normal" font="default" size="100%">LTER.2002-93470</style></accession-num></record></records></xml>