<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>17</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Nilsen, Jan Even Øie</style></author><author><style face="normal" font="default" size="100%">Nilsen, F.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">The Atlantic Water flow along the Vøring Plateau: Detecting frontal structures in the ocean station time series</style></title><secondary-title><style face="normal" font="default" size="100%">Deep-Sea Research</style></secondary-title><tertiary-title><style face="normal" font="default" size="100%">Part I: Oceanographic Research Papers</style></tertiary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">15</style></keyword><keyword><style  face="normal" font="default" size="100%">Atlantic Water</style></keyword><keyword><style  face="normal" font="default" size="100%">Baroclinic motion</style></keyword><keyword><style  face="normal" font="default" size="100%">Fronts</style></keyword><keyword><style  face="normal" font="default" size="100%">Nordic Seas</style></keyword><keyword><style  face="normal" font="default" size="100%">Ocean Weather Station M</style></keyword><keyword><style  face="normal" font="default" size="100%">Topographic effects</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2007</style></year></dates><urls><web-urls><url><style face="normal" font="default" size="100%">http://www.elsevier.com/wps/find/journaldescription.cws_home/601265/description#description</style></url></web-urls><related-urls><url><style face="normal" font="default" size="100%">http://www.nersc.no/sites/www.nersc.no/files/nilsen_mfront.pdf</style></url></related-urls></urls><number><style face="normal" font="default" size="100%">3</style></number><publisher><style face="normal" font="default" size="100%">Elsevier Science</style></publisher><volume><style face="normal" font="default" size="100%">54</style></volume><pages><style face="normal" font="default" size="100%">297-319</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The topographic steering of the baroclinic western branch of the Norwegian Atlantic Current (NwAC) determines the extent of Atlantic Water and location of the Arctic Front in the Nordic Seas. In this paper the geographical spread of hydrographic measurements at the Ocean Weather Station M (OWSM, 66</style></abstract><auth-address><style face="normal" font="default" size="100%">NERSC</style></auth-address></record></records></xml>