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…n-scheme' into next (PR #5974) In default, the infiltration rate is the same for the non-water surface and surface water storage within the grid cell. This assumption results in a significant underestimation of surface water because the infiltration in the surface water storage is not constrained. In this PR, we introduced a modified infiltration scheme to constrain the infiltration in the surface water storage. The infiltration rate in the surface water storage is smaller than the infiltration rate in the non-water surface. More details about this new scheme and corresponding evaluations can be found in the preprint: https://doi.org/10.21203/rs.3.rs-2733749/v1 The manuscript is still under review. The new infiltration scheme can be turned by adding use_modified_infil = .true. in user_nl_elm. We passed all the tests in e3sm_land_developer test suite. We also created a test for the simulation of surface water dynamics with the new infiltration scheme and calibrated parameter for NLDAS domain: surface_water_dynamics. This test was added into e3sm_land_developer test suite. [BFB] [STEALTH]
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components/elm/cime_config/testdefs/testmods_dirs/elm/surface_water_dynamics/shell_commands
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./xmlchange DATM_MODE=CLMMOSARTTEST | ||
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./xmlchange LND_DOMAIN_FILE=domain.lnd.nldas2_0224x0464_c110415.nc | ||
./xmlchange ATM_DOMAIN_FILE=domain.lnd.nldas2_0224x0464_c110415.nc | ||
./xmlchange LND_DOMAIN_PATH="\$DIN_LOC_ROOT/share/domains/domain.clm" | ||
./xmlchange ATM_DOMAIN_PATH="\$DIN_LOC_ROOT/share/domains/domain.clm" | ||
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./xmlchange -file env_run.xml -id DATM_CLMNCEP_YR_END -val 2000 | ||
./xmlchange -file env_run.xml -id DATM_CLMNCEP_YR_START -val 2000 | ||
./xmlchange -file env_run.xml -id DATM_CLMNCEP_YR_ALIGN -val 1 |
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components/elm/cime_config/testdefs/testmods_dirs/elm/surface_water_dynamics/user_nl_elm
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fsurdat = '$DIN_LOC_ROOT/lnd/clm2/surfdata_map/surfdata_nldas2_simyr2000_c181207_surfacewater.nc' | ||
use_modified_infil = .true. |
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