The amount of water stored on continents is an important constraint for water mass and energy exchanges in the Earth system and exhibits large inter-annual variability at both local and continental scales. From 2002 to 2017, the satellites of the Gravity Recovery and Climate Experiment (GRACE) mission have observed changes in terrestrial water storage (TWS) with an unprecedented level of accuracy. In this paper, we use a statistical model trained with GRACE observations to reconstruct past climate-driven changes in TWS from historical and near-real-time meteorological datasets at daily and monthly scales. Unlike most hydrological models which represent water reservoirs individually (e.g., snow, soil moisture) and usually provide a single mo...
The Gravity Recovery and Climate Experiment (GRACE) mission ended its operation in October 2017, and...
International audienceBy delivering monthly maps of the gravity field, the GRACE project allows the ...
A land surface model’s ability to simulate states (e.g., soil moisture) and fluxes (e.g., runoff) is...
The amount of water stored on continents is an important constraint for water mass and energy exchan...
Notes for the 13.10.2019 update- The months of January 2019 to July 2019 were added to the ERA5 reco...
This research data is associated with the manuscript entitled "Long-term (1979-present) Total Water ...
Hydrological models and the data derived from the Gravity Recovery and Climate Experiment (GRACE) sa...
Terrestrial water storage (TWS) includes all forms of water stored on and below the land surface, an...
For 15 years, the Gravity Recovery and Climate Experiment (GRACE) mission have monitored total water...
Since 2002, the GRACE satellite mission provides estimates of the Earth's dynamic gravity field with...
Coupled climate models participating in the CMIP5 (Coupled Model Intercomparison Project Phase 5) ex...
Abstract. Estimates of terrestrial water storage (TWS) variations from the Gravity Recovery and Cli...
The Gravity Recovery and Climate Experiment (GRACE) mission has provided unprecedented observations ...
Since March 2002, the Gravity Recovery and Climate Experiment (GRACE) has provided first estimates o...
Estimates of terrestrial water storage (TWS) variations from the Gravity Recovery and Climate Experi...
The Gravity Recovery and Climate Experiment (GRACE) mission ended its operation in October 2017, and...
International audienceBy delivering monthly maps of the gravity field, the GRACE project allows the ...
A land surface model’s ability to simulate states (e.g., soil moisture) and fluxes (e.g., runoff) is...
The amount of water stored on continents is an important constraint for water mass and energy exchan...
Notes for the 13.10.2019 update- The months of January 2019 to July 2019 were added to the ERA5 reco...
This research data is associated with the manuscript entitled "Long-term (1979-present) Total Water ...
Hydrological models and the data derived from the Gravity Recovery and Climate Experiment (GRACE) sa...
Terrestrial water storage (TWS) includes all forms of water stored on and below the land surface, an...
For 15 years, the Gravity Recovery and Climate Experiment (GRACE) mission have monitored total water...
Since 2002, the GRACE satellite mission provides estimates of the Earth's dynamic gravity field with...
Coupled climate models participating in the CMIP5 (Coupled Model Intercomparison Project Phase 5) ex...
Abstract. Estimates of terrestrial water storage (TWS) variations from the Gravity Recovery and Cli...
The Gravity Recovery and Climate Experiment (GRACE) mission has provided unprecedented observations ...
Since March 2002, the Gravity Recovery and Climate Experiment (GRACE) has provided first estimates o...
Estimates of terrestrial water storage (TWS) variations from the Gravity Recovery and Climate Experi...
The Gravity Recovery and Climate Experiment (GRACE) mission ended its operation in October 2017, and...
International audienceBy delivering monthly maps of the gravity field, the GRACE project allows the ...
A land surface model’s ability to simulate states (e.g., soil moisture) and fluxes (e.g., runoff) is...