To study the sub-seasonal distribution and generation of ocean mass anomalies, Gravity Recovery and Climate Experiment (GRACE) observations of daily and monthly resolution are assimilated into a global ocean circulation model with an ensemble-based Kalman-Filter technique. The improvements are caused by assimilation-induced changes in the atmospheric wind forcing, i.e., quantities not directly observed by GRACE.
Saynisch, J., Bergmann-Wolf, I., Thomas, M. Assimilation of GRACE-derived oceanic mass distributions with a global ocean circulation model,
Springer Berlin Heidelberg, 2015, с.121-139.
Saynisch, J., Bergmann-Wolf, I., Thomas, M. .
Assimilation of GRACE-derived oceanic mass distributions with a global ocean circulation model.
: Springer Berlin Heidelberg, 2015, с.121-139.
Saynisch, J., Bergmann-Wolf, I., Thomas, M. (2015)
Assimilation of GRACE-derived oceanic mass distributions with a global ocean circulation model,
: Springer Berlin Heidelberg, с.121-139
Saynisch, J.,
Bergmann-Wolf, I., &
Thomas, M.
(2015).
Assimilation of GRACE-derived oceanic mass distributions with a global ocean circulation model. Journal of Geodesy. Springer Berlin Heidelberg 89 (2), с.121-139.
