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The introduction of CaMa-Flood in the IFS permit to consider a tighter coupling between the inundated areas and the atmosphere, as well as the soil below. A set experiments has been prepare to support the development of the 2-way coupling, starting from re-evaporating from temporarily inundated areas. CAMA-Coupling of lakes and inundation require alignment with the Hydro branches. Here work in progress experiments:
| 1 | Surface | ivkr | TCo399 | 1980-2025 | pad_CY49R1_control_50R1_esuite | CONTROL | 4 Layers as in 49r1 Oper. |
| 2 | Surface | ivk9 | TCo399 | 1980-2025 | pad_CY49R1_control_50R1_esuite | CAMA2WAY | CAMA-Flood is coupled 2way with impact on Evaporation |
| 3 | Surface | iw03 | TCo399 | 1980-2025 | pad_CY49R1_control_50R1_esuite | CAMA2WAY | CAMA-Flood is coupled 2way with impact on Evaporation, and with water extracted from rivers (LWEVAP=.true.) |
A set of case studies is identified and the plan is to compare with the operational runs and the Atos DestinE Extremes DT run. The control TEST: Run ecLand/CaMa-Flood with SDFOR instead of SDOR can provide the starting point from both 9 and 4km coupled testing. Offline DestinE new experiments are also providing a useful batch.