Bottom water warming along the pathway of lower circumpolar deep water in the Pacific Ocean
Geophysical Research Letters, Vol. 33 (14 December 2006), L23613.
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This article has been bookmarked 5 times, initially on 2006-12-23.
| 2007-07-25 |
User zan
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| 2006-12-23 |
User kmcolo
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Repeat trans-Pacific hydrographic observations along the pathway of Lower Circumpolar Deep Water (LCDW) reveal that bottom water has warmed by about 0.005 to 0.01°C in recent decades. The warming is probably not from direct heating of LCDW, but is manifest as a decrease of the coldest component of LCDW evident at each hydrographic section. This result is consistent with numerical model results of warming associated with decreased bottom water formation rates around Antarctica.
2006-12-23 21:15:20
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