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Introduce namelist option for thermal conductivity of snow: Jordan vs. Sturm #2148
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| Original file line number | Diff line number | Diff line change |
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@@ -47,7 +47,7 @@ module SoilTemperatureMod | |
| ! o The thermal conductivity of soil is computed from | ||
| ! the algorithm of Johansen (as reported by Farouki 1981), and the | ||
| ! conductivity of snow is from the formulation used in | ||
| ! SNTHERM (Jordan 1991). | ||
| ! Sturm (1997). | ||
| ! o Boundary conditions: | ||
| ! F = Rnet - Hg - LEg (top), F= 0 (base of the soil column). | ||
| ! o Soil / snow temperature is predicted from heat conduction | ||
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@@ -100,7 +100,7 @@ subroutine SoilTemperature(bounds, num_urbanl, filter_urbanl, num_urbanc, filter | |
| ! o The thermal conductivity of soil is computed from | ||
| ! the algorithm of Johansen (as reported by Farouki 1981), and the | ||
| ! conductivity of snow is from the formulation used in | ||
| ! SNTHERM (Jordan 1991). | ||
| ! Sturm (1997). | ||
| ! o Boundary conditions: | ||
| ! F = Rnet - Hg - LEg (top), F= 0 (base of the soil column). | ||
| ! o Soil / snow temperature is predicted from heat conduction | ||
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@@ -611,7 +611,7 @@ subroutine SoilThermProp (bounds, num_urbanc, filter_urbanc, num_nolakec, filter | |
| ! | ||
| ! (2) The thermal conductivity of soil is computed from the algorithm of | ||
| ! Johansen (as reported by Farouki 1981), and of snow is from the | ||
| ! formulation used in SNTHERM (Jordan 1991). | ||
| ! formulation used in Sturm (1997). | ||
| ! The thermal conductivities at the interfaces between two neighboring | ||
| ! layers (j, j+1) are derived from an assumption that the flux across | ||
| ! the interface is equal to that from the node j to the interface and the | ||
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@@ -734,11 +734,16 @@ subroutine SoilThermProp (bounds, num_urbanc, filter_urbanc, num_nolakec, filter | |
| endif | ||
| endif | ||
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| ! Thermal conductivity of snow, which from Jordan (1991) pp. 18 | ||
| ! Thermal conductivity of snow, which from Sturm (1997) | ||
| ! Only examine levels from snl(c)+1 -> 0 where snl(c) < 1 | ||
| if (snl(c)+1 < 1 .AND. (j >= snl(c)+1) .AND. (j <= 0)) then | ||
| bw(c,j) = (h2osoi_ice(c,j)+h2osoi_liq(c,j))/(frac_sno(c)*dz(c,j)) | ||
| thk(c,j) = tkair + (7.75e-5_r8 *bw(c,j) + 1.105e-6_r8*bw(c,j)*bw(c,j))*(tkice-tkair) | ||
| bw(c,j) = ((h2osoi_ice(c,j)*1)+h2osoi_liq(c,j))/(frac_sno(c)*dz(c,j)) ! ==RHOS | ||
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Contributor
There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. This line is actually is the same for both approaches.
Contributor
There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. Returning line 740 to the original. Is the comment at the end |
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| ! thk(c,j) = tkair + (7.75e-5_r8 *bw(c,j) + 1.105e-6_r8*bw(c,j)*bw(c,j))*(tkice-tkair) ! Original (Jordan) Parameterisation | ||
| if (bw(c,j) <= 156) then !LMW or 0.156 ? | ||
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Contributor
There was a problem hiding this comment. Choose a reason for hiding this commentThe reason will be displayed to describe this comment to others. Learn more. Here is where I think we'll want to use a namelist option to chose between Jornand and Sturm formulations for |
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| thk(c,j) = 0.023 + 0.234*(bw(c,j)/1000) !LMW - units changed by VRD | ||
| else !LMW | ||
| thk(c,j) = 0.138 - 1.01*(bw(c,j)/1000) +(3.233*((bw(c,j)/1000)*(bw(c,j)/1000))) ! LMW Sturm I think | ||
| end if | ||
| end if | ||
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| end do | ||
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Why is there so much documentation in the code itself here? If we keep all the notes (here and below) snow conductivity should reference both Jordan and Sturm papers.
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Half of the notes here and below are about the thermal conductivity of soil, so I will keep them and reference both papers.