1 | |
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2 | ! $Header$ |
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3 | |
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4 | MODULE icefrac_lsc_mod |
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5 | |
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6 | IMPLICIT NONE |
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7 | |
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8 | CONTAINS |
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9 | !******************************************************************* |
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10 | |
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11 | SUBROUTINE icefrac_lsc(np,temp, sig, icefrac) |
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12 | |
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13 | ! Compute the ice fraction 1-xliq (see e.g. |
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14 | ! Doutriaux-Boucher & Quaas 2004, section 2.2.) |
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15 | |
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16 | ! (JBM 3/14 8/14 5/16) |
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17 | |
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18 | USE print_control_mod, ONLY: lunout, prt_level |
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19 | USE lmdz_lscp_ini, ONLY: t_glace_min, t_glace_max, exposant_glace, iflag_t_glace |
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20 | ! lscp_ini contains: |
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21 | ! t_glace_min: if T < Tmin, the cloud is only made of water ice |
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22 | ! t_glace_max: if T > Tmax, the cloud is only made of liquid water |
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23 | ! exposant_glace: controls the sharpness of the transition |
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24 | INTEGER :: np |
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25 | REAL, DIMENSION(np), INTENT(IN) :: temp ! temperature |
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26 | REAL, DIMENSION(np), INTENT(IN) :: sig |
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27 | REAL, DIMENSION(np), INTENT(OUT) :: icefrac |
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28 | |
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29 | REAL :: sig0,www,tmin_tmp,liqfrac_tmp |
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30 | INTEGER :: ip |
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31 | |
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32 | sig0=0.8 |
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33 | |
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34 | DO ip=1,np |
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35 | IF (iflag_t_glace==1) THEN |
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36 | ! Transition to ice close to surface for T<Tmax |
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37 | ! w=1 at the surface and 0 for sig < sig0 |
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38 | www=(max(sig(ip)-sig0,0.))/(1.-sig0) |
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39 | ELSEIF (iflag_t_glace>=2) THEN |
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40 | ! No convertion to ice close to surface |
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41 | www = 0. |
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42 | ENDIF |
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43 | tmin_tmp=www*t_glace_max+(1.-www)*t_glace_min |
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44 | liqfrac_tmp= (temp(ip)-tmin_tmp) / (t_glace_max-tmin_tmp) |
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45 | liqfrac_tmp = MIN(MAX(liqfrac_tmp,0.0),1.0) |
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46 | IF (iflag_t_glace>=3) THEN |
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47 | icefrac(ip) = 1.0-liqfrac_tmp**exposant_glace |
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48 | ELSE |
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49 | icefrac(ip) = (1.0-liqfrac_tmp)**exposant_glace |
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50 | ENDIF |
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51 | ENDDO |
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52 | |
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53 | RETURN |
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54 | END SUBROUTINE icefrac_lsc |
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55 | |
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56 | !******************************************************************* |
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57 | |
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58 | END MODULE icefrac_lsc_mod |
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