<?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%">Swift, L.W.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Climatology and hydrology.</style></title><secondary-title><style face="normal" font="default" size="100%">Pages 35-55 in W</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">CWT</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">1988</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://cwt33.ecology.uga.edu/publications/393.pdf</style></url></web-urls></urls><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">Streamflow from an undisturbed forested watershed is the net result of the physiography of the catchment and its climate.  In early reports on the research in the southern Appalachian Mountains, Hursh championed studies to describe and develop understanding of climate, precipitation, soils, and topography of these mountains and how they interact with forest vegetation to produce streamflow.The state of knowledge of climate and streamflow in the Coweeta Basin and understanding of interactions with topography and vegetation are subjects of this chapter.</style></abstract><accession-num><style face="normal" font="default" size="100%">LTER.1988-80971</style></accession-num></record></records></xml>