A Generalized Inverse Model of the Equatorial Pacific Ocean

将发展赤道太平洋的广义逆同化或四维变分同化方案。一个时间相关的，多层次的，非线性的原始方程模型将是一个弱约束。初始条件和强迫将会改变，以适应来自TOGA TAO阵列、地面漂移器、潮汐计和高度计的数据。生产油田将允许详细解释TOGA TAO数据，并为预测模型提供更准确和动态一致的初始条件。

9520956 Bennett A generalized inverse, or four-dimensional variational assimilation scheme for the Equatorial Pacific ocean will be developed. A time-dependent, multi-level, non-linear primitive equation model will be a weak constraint. Initial conditions and forcing will be varied in order to fit data from the TOGA TAO Array, surface drifters, tidegauges and altimetry. The produced fields will allow detailed interpretation of the TOGA TAO data and provide more accurate and dynamically consistent initial conditions for forecast models.