## Abstract Assimilation of temperature observations into an ocean model near the equator often results in a dynamically unbalanced state with unrealistic overturning circulations. The way in which these circulations arise from systematic errors in the model or its forcing is discussed. A scheme is
β¦ LIBER β¦
Error estimates for assimilation of satellite sea surface temperature data in ocean climate models
β Scribed by Richman, James G.; Miller, Robert N.; Spitz, Yvette H.
- Book ID
- 119666547
- Publisher
- American Geophysical Union
- Year
- 2005
- Tongue
- English
- Weight
- 649 KB
- Volume
- 32
- Category
- Article
- ISSN
- 1944-8007
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