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| N | Type | Experiment | Resolution | Time | Branch | Label | Comments |
|---|---|---|---|---|---|---|---|
| 1 | Surface | iv3q (copy of iluo) | TCo399 | 1980-2024 | pad_CY49R1.1_control | CONTROL | 4 Layers as in 49r1 Oper. Minimum lake depth 2.0m |
| 2 | Surface | iv6b | TCo399 | 1980-2024 | pad_CY49R1.1_shallow_water | SHALLOW WATER | Minimum lake depth 0.5m |
| 3 | Surface | iv74 | TCo399 | 1980-2024 | pad_CY49R1.1_shallow_water_1 | SHALLOW WATER | Minimum lake depth 1.0m |
| 4 | Surface | iv8v | TCo399 | 1980-2024 | pad_CY49R1.1_shallow_water_15 | SHALLOW WATER | Minimum lake depth 1.5m |
Results file:///perm/pad/climsfc/49r1_shallow_lakes/plots/eval_mon.html indicate neutral impact from changing the minimum lake depth.
Lake mean depth correction/upgrade details the recently updated lake depth (i.e. new bathymetry for Caspian Sea, Azov Sea, Titicaca Lake, how we recognize lakes to map mean depth.
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| N | Type | Experiment | Resolution | Time | Branch | Label | Comments |
|---|---|---|---|---|---|---|---|
| 1 | Surface | ivd5 | TCo399 | 1980-2024 | pad_CY49R1.1_runoff_frozen_soil | RUNOFF_FROZEN_SOIL | revised permeability limiting freezing shutdown to 50% of soil |
| 2 | Surface | ivgk | TCo399 | 1980-2024 | pad_CY49R1.1_runoff_frozen_soil_20 | RUNOFF_FROZEN_SOIL | revised permeability limiting freezing shutdown to 20% of soil |
Results file:///perm/pad/climsfc/49r1_shallow_lakes/plots/eval_mon.html indicate that 50% permeability in frozen soil condition can increase the overall soil water storage.
A new soil discretisation (control experiment iv3r) and new climate fields version (climate.v023) will be tested in parallel and the CAMA-Coupling of lakes and inundation require alignment with the Hydro branches. Here 2 work in progress experiment (not yet completing):
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