Improved estimates of upper-ocean warming and multi-decadal sea-level rise

Edited: 2011-02-21
TitleImproved estimates of upper-ocean warming and multi-decadal sea-level rise
Publication TypeJournal Article
Year of Publication2008
AuthorsDomingues, C., J. Church, N. White, P. Gleckler, S. E. Wijffels, P. Barker, and J. Dunn
JournalNature
Volume453
Issue7198
Pagination1090
Date Published06/2008
Keywordsclimate, sea_level, steric
AbstractChanges in the climate system's energy budget are predominantly revealed in ocean temperatures1, 2 and the associated thermal expansion contribution to sea-level rise2. Climate models, however, do not reproduce the large decadal variability in globally averaged ocean heat content inferred from the sparse observational database3, 4, even when volcanic and other variable climate forcings are included. The sum of the observed contributions has also not adequately explained the overall multi-decadal rise2. Here we report improved estimates of near-global ocean heat content and thermal expansion for the upper 300 m and 700 m of the ocean for 1950–2003, using statistical techniques that allow for sparse data coverage5, 6, 7 and applying recent corrections8 to reduce systematic biases in the most common ocean temperature observations9. Our ocean warming and thermal expansion trends for 1961–2003 are about 50 per cent larger than earlier estimates but about 40 per cent smaller for 1993–2003, which is consistent with the recognition that previously estimated rates for the 1990s had a positive bias as a result of instrumental errors8, 9, 10. On average, the decadal variability of the climate models with volcanic forcing now agrees approximately with the observations, but the modelled multi-decadal trends are smaller than observed. We add our observational estimate of upper-ocean thermal expansion to other contributions to sea-level rise and find that the sum of contributions from 1961 to 2003 is about 1.5  0.4 mm yr-1, in good agreement with our updated estimate of near-global mean sea-level rise (using techniques established in earlier studies6, 7) of 1.6  0.2 mm yr-1.
DOI10.1038/nature07080