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8 - The Dynamic Ocean

from Flows of Energy

Published online by Cambridge University Press:  25 February 2022

Kevin E. Trenberth
Affiliation:
National Center for Atmospheric Research
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Summary

The oceans are wet, and play a major role in the hydrological cycle. They also have a high heat capacity. Section 6.2 provided the basic character of sea water and ocean structure. Figures 5.2 and 5.3 presented maps and the annual cycle of the mean surface air temperatures, and Fig. 5.4 gave the sea surface temperatures (SSTs). The latter are closely related to water vapor and precipitation in the atmosphere over the oceans. The SSTs are supported by the upper ocean temperatures and especially the mixed layer, which is the part of the ocean in direct contact with the surface through wind effects and heating from both radiation and temperatures in the atmosphere (see Fig. 8.8).

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Publisher: Cambridge University Press
Print publication year: 2022

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References

References and Further Reading

Bronseleiaer, B., and Zanna, L., 2020: Heat and carbon coupling reveals ocean warming due to circulation changes. Nature, 584, 227233. doi: 10.1038/s41586-020-2573-5.CrossRefGoogle Scholar
Cheng, L., Trenberth, K., Fasullo, J., Boyer, T., Abraham, J., and Zhu, J., 2017: Improved estimates of ocean heat content from 1960–2015. Science Advances, 3(3), e1601545. doi: 10.1126/sciadv.1601545. http://advances.sciencemag.org/content/3/3/e1601545.CrossRefGoogle Scholar
Cheng, L., Trenberth, K. E., Gruber, N., et al., 2020: Improved estimates of changes in upper ocean salinity and the hydrological cycle. Journal of Climate, 33. https://doi.org/10.1175/JCLI-D-20-0366.1.CrossRefGoogle Scholar
Cornwall, W., 2019: In hot water. Science, 363, 442445. doi: 10.1126/science.363.6426.442.CrossRefGoogle Scholar
Ezer, T., Atkinson, L. P., Corlett, W. B., and Blanco, J. L., 2013: Gulf Stream’s induced sea level rise and variability along the U.S. mid-Atlantic coast. Journal of Geophysical Research: Oceans, 118, 685697. doi: 10.1002/jgrc.20091.Google Scholar
Lumpkin, R., and Johnson, G. C., 2013: Global ocean surface velocities from drifters: mean, variance, El Nino–Southern Oscillation response, and seasonal cycle. Journal of Geophysical Research: Oceans, 118, 29923006, doi: 10.1002/jgrc.20210.CrossRefGoogle Scholar
Trenberth, K. E., Zhang, Y., Fasullo, J. T., and Cheng, L., 2019: Observation-based estimates of global and basin ocean meridional heat transport time series. Journal of Climate, 32, 45674583. doi: 10.1175/JCLI-D-18-0872.1.CrossRefGoogle Scholar

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  • The Dynamic Ocean
  • Kevin E. Trenberth
  • Book: The Changing Flow of Energy Through the Climate System
  • Online publication: 25 February 2022
  • Chapter DOI: https://doi.org/10.1017/9781108979030.011
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  • The Dynamic Ocean
  • Kevin E. Trenberth
  • Book: The Changing Flow of Energy Through the Climate System
  • Online publication: 25 February 2022
  • Chapter DOI: https://doi.org/10.1017/9781108979030.011
Available formats
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Save book to Google Drive

To save content items to your account, please confirm that you agree to abide by our usage policies. If this is the first time you use this feature, you will be asked to authorise Cambridge Core to connect with your account. Find out more about saving content to Google Drive.

  • The Dynamic Ocean
  • Kevin E. Trenberth
  • Book: The Changing Flow of Energy Through the Climate System
  • Online publication: 25 February 2022
  • Chapter DOI: https://doi.org/10.1017/9781108979030.011
Available formats
×