1 | #-------------------------------------------------------------------------------------------------- |
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2 | # Parameter file for forcing |
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3 | # LIM1D, version source_3.04 - ISPOL forcing |
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4 | #-------------------------------------------------------------------------------------------------- |
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5 | # ts_forc time step of the forcing |
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6 | 86400.0 |
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7 | # n0_forc number of the first time step in forcing file wrt XXXX ???? |
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8 | 263 |
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9 | # n1_forc number of the forcing.nc last time step relative to XXXX ???? |
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10 | 340 |
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11 | #-------------------------------------------------------------------------------------------------- |
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12 | # forc_swi 0=read in nc, 1-N=computed, 99=prescribed |
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13 | # forc_uni multiplication factor compared to SI units |
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14 | # forc_val constant value in case of prescribed value (forc_swi = 99) |
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15 | #-------------------------------------------------------------------------------------------------- |
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16 | # forc_swi forc_uni forc_val |
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17 | # shortwave radiation (W/m2) ; 1=Shine; 2=Zillmann |
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18 | 0 1.0 0.0 |
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19 | # longwave radiation (W/m2); 1=Efimova; 2=Berliand |
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20 | 0 1.0 0.0 |
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21 | # incident PAR (muE/m2/s); 1=Computed from shortwave |
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22 | 1 1.0 0.0 |
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23 | # air temperature (K) |
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24 | 0 1.0 0.0 |
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25 | # atmospheric pressure (Pa) |
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26 | 0 1.0 0.0 |
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27 | # specific humidity (kg/kg) ! there is a bias at ISPOL |
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28 | 0 1.00 0.0 |
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29 | # wind speed (m/s) |
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30 | 0 1.0 0.0 |
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31 | # cloudiness (0-1) |
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32 | 99 1.0 1.0 |
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33 | # oceanic heat flux (W/m2) ; 5. is the ref |
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34 | 99 1.0 4. |
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35 | # snowfall (dimensions=length/timestep) 0.012 - 1h |
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36 | 99 1.0 0.0 |
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37 | # albedo (0-1); 1=Shine & Henderson-Sellers, 2=parameterized using obs from ISPOL |
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38 | 1 1.0 0.00 |
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39 | #-------------------------------------------------------------------------------------------------- |
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40 | # Some parameters |
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41 | #-------------------------------------------------------------------------------------------------- |
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42 | # opt_dept : optical depth (m) in Efimova 1961 parameterization; SIMBA - 16.297; ISPOL - ; BARROW - WHY 30. ? |
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43 | 12.0 |
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