- 1Universidad de Alicante, Escuela Politécnica Superior, Applies Mathematics Department, Alicante, Spain
- 2Universidad de Alicante, Facultad de Ciencias, Mathematics Department, Alicante, Spain
In the ocean, horizontal water fluxes can be estimated from a variety of in situ measurements and ocean general circulation models. However, the study of such fluxes with remote measurements has been elusive for decades. In recent years, a technique has been developed that allows the calculation of net ocean water transports between basins from: (1) temporal gravity measurements made by the GRACE and GRACE-FO missions; (2) global precipitation and evaporation such as those from the ERA5 atmospheric reanalysis model. In this work, we show a compilation of the results obtained with this technique, such as the net water exchange between ocean basins and between semi-enclosed seas (Black, Mediterranean and Baltic Seas, and the Arabian Gulf) and the open ocean. Such results are useful for understanding ocean dynamics and providing constraints for numerical ocean models.
How to cite: Garcia-Garcia, D., Boulahia, A. K., Trottini, M., Vargas‐Alemañy, J. A., Sayol, J., and Vigo, M. I.: Estimates of net horizontal water fluxes in the ocean from GRACE/GRACE-FO and ERA5, EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-15595, https://doi.org/10.5194/egusphere-egu25-15595, 2025.