Continuity of NASA Earth Observations from Space A Value Framework (2015) / Chapter Skim
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Appendix E: Full Framework Example: Determining the Change in Ocean Heat Storage
Appendix E: Full Framework Example: Determining the Change in Ocean Heat Storage
Pages 83-85
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From page 83... ...
The ocean heat is estimated from the total steric change calculated as the altimetry sea level-GRACE determined mass component. The comparison of the space determined steric sea level to Argo estimated value for the upper 2000 m is consistent within measurement errors of both systems.
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From page 84... ...
and GRACE (from the glacial isostatic adjustment correction) have time scales much longer than a decade, the 1-s error in the full-depth steric sea level rate, computed from the difference between altimetry and GRACE observations over a decade (in which the calibration errors cancel out)
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From page 85... ...
2010. Warming of global abyssal and deep southern ocean waters between the 1990s and 2000s: contributions to global heat and sea level rise budgets.
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