<?xml version="1.0" encoding="UTF-8"?><xml><records><record><source-app name="Biblio" version="6.x">Drupal-Biblio</source-app><ref-type>10</ref-type><contributors><authors><author><style face="normal" font="default" size="100%">Lygre, Kjetil</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Carbon uptake by the ocean, subject to biological feedback</style></title><secondary-title><style face="normal" font="default" size="100%">Arctic Science Summit Week</style></secondary-title></titles><dates><year><style  face="normal" font="default" size="100%">2009</style></year></dates><publisher><style face="normal" font="default" size="100%">Talk at: The Role of the Arctic in the Global Change process</style></publisher><pub-location><style face="normal" font="default" size="100%">Bergen 23-28 March 2009</style></pub-location><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">The World oceans - especially the Arctic - are projected to undergo large changes in physical state, such as temperature, light (shrinking ice cover) and mixing climate. The ocean stores carbon by the joint effect of solubility (temperature, wind) and downward particulate transport of biogenic material. A simple box model is constructed to examine how changes in physical parameters (mainly temperature and light) alter carbon storage and the partitioning between downward transport of sinking particles and dissolved organic matter.</style></abstract><auth-address><style face="normal" font="default" size="100%">NERSC</style></auth-address></record></records></xml>