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Merge pull request #1228 from CliMA/js/soil_bc_bug
fix soil boundary var construction with coupled atmos
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.buildkite/Manifest-v1.11.toml

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deps = ["ClimaComms", "ClimaCore", "ClimaDiagnostics", "ClimaTimeSteppers", "ClimaUtilities", "Dates", "DocStringExtensions", "Insolation", "Interpolations", "LazyArtifacts", "LazyBroadcast", "LinearAlgebra", "NCDatasets", "SciMLBase", "StaticArrays", "SurfaceFluxes", "Thermodynamics"]
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path = ".."
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uuid = "08f4d4ce-cf43-44bb-ad95-9d2d5f413532"
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version = "0.17.0"
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version = "0.17.1"
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weakdeps = ["BSON", "CSV", "ClimaParams", "DataFrames", "Flux", "HTTP", "StatsBase"]
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[deps.ClimaLand.extensions]

.buildkite/Manifest.toml

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deps = ["ClimaComms", "ClimaCore", "ClimaDiagnostics", "ClimaTimeSteppers", "ClimaUtilities", "Dates", "DocStringExtensions", "Insolation", "Interpolations", "LazyArtifacts", "LazyBroadcast", "LinearAlgebra", "NCDatasets", "SciMLBase", "StaticArrays", "SurfaceFluxes", "Thermodynamics"]
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path = ".."
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uuid = "08f4d4ce-cf43-44bb-ad95-9d2d5f413532"
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version = "0.17.0"
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version = "0.17.1"
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weakdeps = ["BSON", "CSV", "ClimaParams", "DataFrames", "Flux", "HTTP", "StatsBase"]
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[deps.ClimaLand.extensions]

NEWS.md

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main
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-------
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v0.17.1
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-------
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- Fix bug in soil boundary var types for coupled atmos PR[#1228](https://github.com/CliMA/ClimaLand.jl/pull/1228)
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v0.17.0
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-------
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- Fix texure norm bug (soil composition) PR[#1217](https://github.com/CliMA/ClimaLand.jl/pull/1217)

Project.toml

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name = "ClimaLand"
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uuid = "08f4d4ce-cf43-44bb-ad95-9d2d5f413532"
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authors = ["Clima Land Team"]
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version = "0.17.0"
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version = "0.17.1"
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[deps]
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ClimaComms = "3a4d1b5c-c61d-41fd-a00a-5873ba7a1b0d"

docs/Manifest-v1.11.toml

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deps = ["ClimaComms", "ClimaCore", "ClimaDiagnostics", "ClimaTimeSteppers", "ClimaUtilities", "Dates", "DocStringExtensions", "Insolation", "Interpolations", "LazyArtifacts", "LazyBroadcast", "LinearAlgebra", "NCDatasets", "SciMLBase", "StaticArrays", "SurfaceFluxes", "Thermodynamics"]
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path = ".."
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uuid = "08f4d4ce-cf43-44bb-ad95-9d2d5f413532"
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version = "0.17.0"
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version = "0.17.1"
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weakdeps = ["BSON", "CSV", "ClimaParams", "DataFrames", "Flux", "HTTP", "StatsBase"]
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docs/Manifest.toml

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deps = ["ClimaComms", "ClimaCore", "ClimaDiagnostics", "ClimaTimeSteppers", "ClimaUtilities", "Dates", "DocStringExtensions", "Insolation", "Interpolations", "LazyArtifacts", "LazyBroadcast", "LinearAlgebra", "NCDatasets", "SciMLBase", "StaticArrays", "SurfaceFluxes", "Thermodynamics"]
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path = ".."
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uuid = "08f4d4ce-cf43-44bb-ad95-9d2d5f413532"
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version = "0.17.0"
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version = "0.17.1"
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weakdeps = ["BSON", "CSV", "ClimaParams", "DataFrames", "Flux", "HTTP", "StatsBase"]
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src/standalone/Soil/boundary_conditions.jl

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A concrete type of soil boundary condition, for use at
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the BottomBoundary only, where the flux is set to be
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`F = -K∇h = -K`.
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`F = -K∇h = -K`.
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This is not tied to any boundary condition for the heat equation.
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This is not tied to any boundary condition for the heat equation.
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To account for the energy flux resulting from free drainage of liquid
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water, please see `EnergyWaterFreeDrainage`.
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"""
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FT,
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FT,
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FT,
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FT,
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Runoff.runoff_var_types(bc.runoff, FT)...,
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)
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of the soil domain.
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Here, the soil boundary fluxes are computed as if the soil is run
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in standalone mode, indicated by the value of
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in standalone mode, indicated by the value of
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`prognostic_land_components`.
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"""
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function soil_boundary_fluxes!(
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compute_liquid_influx(p,
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model,
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prognostic_land_components::Val{(:soil,)},
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)
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)
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Returns the liquid water volume flux at the surface of the soil; this
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will then be partitioned into surface runoff and infiltration:
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we approximate the volumetric internal energy with the volumetric
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internal energy of liquid water at the air temperature at the surface.
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Future runoff parameterizations may require allowing for exfiltration of
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Future runoff parameterizations may require allowing for exfiltration of
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liquid water from the soil, which would have a different energy. To accomodate
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this, the runoff is passed as an argument and this can be used for dispatch in the
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this, the runoff is passed as an argument and this can be used for dispatch in the
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future.
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Furthermore, in coupled simulations, the energy flux may be provided directly,

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