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| 1 | +# LoTmpDnsTruncatedAnderson1976 |
| 2 | +""" |
| 3 | + snow_density(Ta::Float64, U10::Float64=NaN; tfrz=0.0, method="LoTmpDnsSlater2017") |
| 4 | +
|
| 5 | +Calculate the density of new snow |
| 6 | +
|
| 7 | +"Snow fraction depends on the density of snow in CLM4. A 10 cm snowpack has f_snow=1 when density is low |
| 8 | +(50–100 kg m–3), such as may be found in fresh snow, and a smaller snow fraction (f_snow = 0.76) |
| 9 | +when density is high (400 kg m–3)" -- Bonan 2019, P148 |
| 10 | +
|
| 11 | +Snow compacts over time, increasing to a density of 100–500 kg m–3. |
| 12 | +
|
| 13 | +# Reference |
| 14 | +
|
| 15 | +- van Kampenhout et al. 2017 |
| 16 | +
|
| 17 | +- CLM5, <https://github.com/ESCOMP/CTSM/blob/07051e3758addf2f9753d520823be9ebcbfec0aa/src/biogeophys/SnowHydrologyMod.F90#L3729-L3747> |
| 18 | +
|
| 19 | +# Examples |
| 20 | +```julia |
| 21 | +Ta = -100.:50 |
| 22 | +ρ_snow = snow_density.(Ta, 2.0) |
| 23 | +ρ_snow_chen = @. 67.9 + 51.3 * exp(Ta / 2.6) |
| 24 | +
|
| 25 | +# using Plots |
| 26 | +# plot(Ta, ρ_snow) |
| 27 | +# plot!(Ta, ρ_snow_chen) |
| 28 | +``` |
| 29 | +""" |
| 30 | +function cal_snow_density(Ta::Float64, U10::Float64=NaN; tfrz=0.0, method="LoTmpDnsSlater2017") |
| 31 | + if Ta > tfrz + 2.0 |
| 32 | + ρ_snow = 50.0 + 1.7 * (17.0)^1.5 |
| 33 | + elseif Ta > tfrz - 15.0 |
| 34 | + ρ_snow = 50.0 + 1.7 * (Ta - tfrz + 15.0)^1.5 |
| 35 | + else |
| 36 | + if method == "LoTmpDnsTruncatedAnderson1976" |
| 37 | + ρ_snow = 50.0 |
| 38 | + elseif method == "LoTmpDnsSlater2017" |
| 39 | + # ρ_snow = -3.833 * (Ta - tfrz) - 0.0333 * (Ta - tfrz)^2 |
| 40 | + t_for_bifall_degC = Ta > tfrz - 57.55 ? (Ta - tfrz) : -57.55 |
| 41 | + ρ_snow = -(50.0 / 15.0 + 0.0333 * 15.0) * t_for_bifall_degC - 0.0333 * t_for_bifall_degC^2 |
| 42 | + end |
| 43 | + end |
| 44 | + |
| 45 | + if U10 > 0.1 |
| 46 | + ρ_snow = ρ_snow + (266.861 * ((1.0 + tanh(U10 / 2)) / 2.0)^8.8) |
| 47 | + end |
| 48 | + ρ_snow |
| 49 | +end |
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