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wet canopy fraction is incorrectly a function of vegetation fraction #91
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weiwangncar
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Jan 13, 2024
TYPE: bug fix KEYWORDS: Noah-MP, snow combine, vegetation fraction scaling, urban ground heat flux SOURCE: Cenlin He (NCAR/RAL) DESCRIPTION OF CHANGES: There are a few bug fixes for Noah-MP related processes: (1) the snow layer index in snow COMBINE module was wrong, causing model crash when snow layer changes by more than 1 layer within one timestep; This has been fixed by using the correct layer index. (2) the ground heat flux sign in Noah-MP column model (positive: downward) is inconsistent with that in urban canopy model (positive: upward), leading to wrong diagnostic grid-mean ground heat flux calculation for urban grid. This only affects the diagnostic value for output. See this issue: #1921 and NCAR/hrldas#114 (3) there is a bug in vegetation fraction (FVEG) scaling for stomata resistance calculation (NCAR/noahmp#92) and canopy interception calculation (NCAR/noahmp#91). LIST OF MODIFIED FILES: list of changed files (use `git diff --name-status master` to get formatted list): phys/noahmp/src/module_sf_noahmplsm.F phys/noahmp/src/module_sf_noahmpdrv.F TESTS CONDUCTED: 1. Tested successfully in NCAR Cheyenne HPC for 13-km run over the entire CONUS region 2. The Jenkins tests are all passing. RELEASE NOTE: Noah-MP bug fix for snow combination, vegetation fraction scaling, and urban ground heat flux sign.
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The partitioning of precipitation in precip_heat/CanopyWaterIntercept is scaled by fveg/VegFrac early in the module, but maxliq/CanopyLiqWaterMax (and similar for snow) are not scaled by fveg/VegFrac. This causes a dependence of fwet/CanopyWetFrac on vegetation fraction. I see two possible solutions:
I like solution 2 better since it is clearer to understand and the canopy water would be a physical value that is actually on the leaf and not spread across the grid.
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