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. Springer Berlin Heidelberg, 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. p. с.121-139.
