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Science 28 August 1998:
Vol. 281. no. 5381, pp. 1327 - 1332
DOI: 10.1126/science.281.5381.1327

Research Articles

Ocean Climate Change: Comparison of Acoustic Tomography, Satellite Altimetry, and Modeling

The ATOC Consortium

Comparisons of gyre-scale acoustic and direct thermal measurements of heat content in the Pacific Ocean, satellite altimeter measurements of sea surface height, and results from a general circulation model show that only about half of the seasonal and year-to-year changes in sea level are attributable to thermal expansion. Interpreting climate change signals from fluctuations in sea level is therefore complicated. The annual cycle of heat flux is 150 ± 25 watts per square meter (peak-to-peak, corresponding to a 0.2°C vertically averaged temperature cycle); an interannual change of similar magnitude is also detected. Meteorological estimates of surface heat flux, if accurate, require a large seasonal cycle in the advective heat flux.

The ATOC Consortium: A. B. Baggeroer, T. G. Birdsall, C. Clark, J. A. Colosi, B. D. Cornuelle, D. Costa, B. D. Dushaw, M. Dzieciuch, A. M. G. Forbes, C. Hill, B. M. Howe, J. Marshall, D. Menemenlis, J. A. Mercer, K. Metzger, W. Munk, R. C. Spindel, D. Stammer, P. F. Worcester, and C. Wunsch.* A. B. Baggeroer is in the Department of Ocean Engineering, Massachusetts Institute of Technology (MIT), Cambridge, MA 02139, USA. T. G. Birdsall and K. Metzger are in the Department of Electrical Engineering and Computer Sciences, University of Michigan, Ann Arbor, MI 48109, USA. C. Clark is in the Laboratory of Ornithology, Cornell University, Ithaca, NY 14853, USA. J. A. Colosi is in the Department of Applied Ocean Physics and Engineering, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA. B. D. Cornuelle, M. Dzieciuch, W. Munk, and P. F. Worcester are at Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093, USA. D. Costa is in the Biology Department, University of California, Santa Cruz, CA 95064, USA. B. D. Dushaw, B. M. Howe, J. A. Mercer, and R. C. Spindel are at the Applied Physics Laboratory, University of Washington, Seattle, WA 98105, USA. A. M. G. Forbes is at the Division of Oceanography, CSIRO, Hobart, Tasmania 7001, Australia. C. Hill, J. Marshall, D. Menemenlis, D. Stammer, and C. Wunsch are in the Department of Earth, Atmospheric and Planetary Sciences, MIT, Cambridge, MA 02139, USA.


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THIS ARTICLE HAS BEEN CITED BY OTHER ARTICLES:
The Late Cambrian Spice ({delta}13C) Event and the Sauk II-SAUK III Regression: New Evidence from Laurentian Basins in Utah, Iowa, and Newfoundland.
(2004)
Journal of Sedimentary Research 74, 366-377
Heat Content Changes in the Pacific Ocean.
K. A. Kelly, L. Thompson, F. Vivier;, and ATOC Consortium (3); (1999)
Science 284, 1735a-1735
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