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|a Observations |h [electronic resource] |b Oceanic Climate Change and Sea Level |y French. |
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|a [S.l.] : |b Intergovernmental Panel on Climate Change, |c 2007. |
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|a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights. |
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|a The oceans are warming. Over the period 1961 to 2003, global ocean temperature has risen by 0.10°C from the surface to a depth of 700 m. Consistent with the Third Assessment Report (TAR), global ocean heat content (0–3,000 m) has increased during the same period, equivalent to absorbing energy at a rate of 0.21 ± 0.04 W m–2 globally averaged over the Earth’s surface. Two-thirds of this energy is absorbed between the surface and a depth of 700 m. Global ocean heat content observations show considerable interannual and inter-decadal variability superimposed on the longer-term trend. Relative to 1961 to 2003, the period 1993 to 2003 has high rates of warming but since 2003 there has been some cooling. |
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|a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software. |
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|a Bindoff, Nathaniel L.. |
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|a dpSobek |c Sea Level Rise |
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|u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15062038/00001 |y Click here for full text |
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|3 Host material |u https://www.ipcc.ch/publications_and_data/ar4/wg1/en/ch5s5-es.html |y Observations |
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|a http://dpanther.fiu.edu/sobek/content/FI/15/06/20/38/00001/FI15062038thm.jpg |