Abstract
Bottom water warming along the pathway of lower circumpolar deep water in the Pacific Ocean
Institute of Observational Research for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Institute of Observational Research for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Institute of Observational Research for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Institute of Observational Research for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Institute of Observational Research for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Institute of Observational Research for Global Change, Japan Agency for Marine-Earth Science and Technology, Yokosuka, Japan
Geochemical Research Department, Meteorological Research Institute, Tsukuba, Japan
Departamento de Oceanografía and Centro de Investigación Oceanográfica en el Pacifico Sur-Oriental, Universidad de Concepción, Concepcion, Chile
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.
Received 21 August 2006; accepted 8 November 2006; published 14 December 2006.
Citation: (2006), Bottom water warming along the pathway of lower circumpolar deep water in the Pacific Ocean, Geophys. Res. Lett., 33, L23613, doi:10.1029/2006GL027933.
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