4.7 Review

A REVIEW OF GLOBAL OCEAN TEMPERATURE OBSERVATIONS: IMPLICATIONS FOR OCEAN HEAT CONTENT ESTIMATES AND CLIMATE CHANGE

期刊

REVIEWS OF GEOPHYSICS
卷 51, 期 3, 页码 450-483

出版社

AMER GEOPHYSICAL UNION
DOI: 10.1002/rog.20022

关键词

global warming; ocean heat content; Argo float; thermosteric sea level rise; expendable bathythermograph; Earth energy balance

资金

  1. ARC Centre of Excellence for Climate Systems Science
  2. MOST project [2012CB417404]
  3. Australian Climate Change Science Program
  4. Australian Antarctic and Ecosystems Research Cooperative Centre
  5. NOAA [NA17RJ1231]
  6. DECC/Defra Met Office Hadley Centre Climate Programme [GA01101]
  7. Cluster of Excellence CLISAP, University of Hamburg [EXC177]
  8. German Science Foundation
  9. NOAA Climate Program Office
  10. NOAA Research
  11. Inter-American Institute for Global Change Research through the US National Science Foundation [GEO-0452325]
  12. NASA [NNX09AH89G]
  13. EC FP7 project MyOcean2
  14. Grants-in-Aid for Scientific Research [23540506] Funding Source: KAKEN
  15. Directorate For Geosciences [1138881] Funding Source: National Science Foundation
  16. Natural Environment Research Council [NE/K005480/1] Funding Source: researchfish
  17. NERC [NE/K005480/1] Funding Source: UKRI

向作者/读者索取更多资源

The evolution of ocean temperature measurement systems is presented with a focus on the development and accuracy of two critical devices in use today (expendable bathythermographs and conductivity-temperature-depth instruments used on Argo floats). A detailed discussion of the accuracy of these devices and a projection of the future of ocean temperature measurements are provided. The accuracy of ocean temperature measurements is discussed in detail in the context of ocean heat content, Earth's energy imbalance, and thermosteric sea level rise. Up-to-date estimates are provided for these three important quantities. The total energy imbalance at the top of atmosphere is best assessed by taking an inventory of changes in energy storage. The main storage is in the ocean, the latest values of which are presented. Furthermore, despite differences in measurement methods and analysis techniques, multiple studies show that there has been a multidecadal increase in the heat content of both the upper and deep ocean regions, which reflects the impact of anthropogenic warming. With respect to sea level rise, mutually reinforcing information from tide gauges and radar altimetry shows that presently, sea level is rising at approximately 3mmyr(-1) with contributions from both thermal expansion and mass accumulation from ice melt. The latest data for thermal expansion sea level rise are included here and analyzed.

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