Modeling ocean heat content changes during the last millennium

Details Modeling ocean heat content changes during the last millennium Modeling ocean heat content changes during the last millennium

Sep 2003

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2003georl..30rclm3c&link_type=abstract

Geophysical Research Letters, Volume 30, Issue 18, pp. CLM 3-1, CiteID 1932, DOI 10.1029/2003GL017801

Mathematics

Logic

31

Atmospheric Composition And Structure: Volcanic Effects (8409), Global Change: Climate Dynamics (3309), Global Change: Oceans (4203), Oceanography: Physical: Sea Level Variations

Scientific paper

Observational studies show a significant increase in ocean heat content over the last half century. Herein we estimate heat content changes during the last millennium with a climate model whose forcing terms have been best-fit to surface proxy data. The model simulates the observed late 20th century ocean heat content increase and a comparable Little Ice Age minimum. When glacial advances are factored in, these results imply a sea level fall after the Middle Ages that is consistent with some geologic data. The present ocean heat content increase can be traced back to the mid-19th century, with a near-linear rate of change during the 20th century.

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