Estimation of systematic error in an equ
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M. J. Martin; M. J. Bell; N. K. Nichols
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Article
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2002
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John Wiley and Sons
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English
โ 224 KB
## 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