<?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%">Levitus, S.</style></author><author><style face="normal" font="default" size="100%">Antonov, J. I.</style></author><author><style face="normal" font="default" size="100%">Boyer, T. P.</style></author><author><style face="normal" font="default" size="100%">Stephens, C.</style></author></authors></contributors><titles><title><style face="normal" font="default" size="100%">Warming of the world ocean</style></title><secondary-title><style face="normal" font="default" size="100%">Science</style></secondary-title></titles><keywords><keyword><style  face="normal" font="default" size="100%">Atlantic Ocean</style></keyword><keyword><style  face="normal" font="default" size="100%">Northern Hemisphere</style></keyword><keyword><style  face="normal" font="default" size="100%">sea surface temperature</style></keyword><keyword><style  face="normal" font="default" size="100%">stratospheric circulation</style></keyword><keyword><style  face="normal" font="default" size="100%">variability</style></keyword><keyword><style  face="normal" font="default" size="100%">winter</style></keyword></keywords><dates><year><style  face="normal" font="default" size="100%">2000</style></year></dates><number><style face="normal" font="default" size="100%">5461</style></number><volume><style face="normal" font="default" size="100%">287</style></volume><pages><style face="normal" font="default" size="100%">2225-2229</style></pages><language><style face="normal" font="default" size="100%">eng</style></language><abstract><style face="normal" font="default" size="100%">&lt;p&gt;We quantify the interannual-to-decadal variability of the heat content (mean temperature) of the world ocean from the surface through 3000-meter depth for the period 1948 to 1998. The heat content of the world ocean increased by similar to 2 X 10(23) joules between the mid-1950s and mid-1990s, representing a volume mean warming of 0.06 degrees C. This corresponds to a warming rate of 0.3 watt per meter squared (per unit area of faith's surface). Substantial changes in heat content occurred in the 300- to 1000-meter layers of each ocean and in depths greater than 1000 meters of the North Atlantic. The global volume mean temperature increase for the 0- to 300-meter layer was 0.31 degrees C, corresponding to an increase in heat content for this Layer of similar to 10(23) joules between the mid-1950s and mid-1990s. The Atlantic and Pacific Oceans have undergone a net warming since the 1950s and the Indian Ocean has warmed since the mid-1960s, although the warming is not monotonic.&lt;/p&gt;</style></abstract></record></records></xml>
