source:
NEMO/trunk/doc/latex/SI3/namelists/namsbc
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15720
Last change on this file since 15720 was 14176, checked in by nicolasmartin, 4 years ago | |
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[11015] | 1 | !------------------------------------------------------------------------------ |
2 | &namsbc ! Ice surface boundary conditions | |
3 | !------------------------------------------------------------------------------ | |
4 | rn_cio = 5.0e-03 ! ice-ocean drag coefficient (-) | |
[14176] | 5 | nn_snwfra = 2 ! calculate the fraction of ice covered by snow (for zdf and albedo) |
6 | ! = 0 fraction = 1 (if snow) or 0 (if no snow) | |
7 | ! = 1 fraction = 1-exp(-0.2*rhos*hsnw) [MetO formulation] | |
8 | ! = 2 fraction = hsnw / (hsnw+0.02) [CICE formulation] | |
9 | rn_snwblow = 0.66 ! mesure of snow blowing into the leads | |
[11015] | 10 | ! = 1 => no snow blowing, < 1 => some snow blowing |
11 | nn_flxdist = -1 ! Redistribute heat flux over ice categories | |
12 | ! =-1 Do nothing (needs N(cat) fluxes) | |
13 | ! = 0 Average N(cat) fluxes then apply the average over the N(cat) ice | |
14 | ! = 1 Average N(cat) fluxes then redistribute over the N(cat) ice using T-ice and albedo sensitivity | |
15 | ! = 2 Redistribute a single flux over categories | |
16 | ln_cndflx = .false. ! Use conduction flux as surface boundary conditions (i.e. for Jules coupling) | |
17 | ln_cndemulate = .false. ! emulate conduction flux (if not provided in the inputs) | |
[14176] | 18 | nn_qtrice = 1 ! Solar flux transmitted thru the surface scattering layer: |
19 | ! = 0 Grenfell and Maykut 1977 (depends on cloudiness and is 0 when there is snow) | |
20 | ! = 1 Lebrun 2019 (equals 0.3 anytime with different melting/dry snw conductivities) | |
[11015] | 21 | / |
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