Changeset 1276 for LMDZ4/branches/LMDZ4-dev/libf/phylmd/cv3_routines.F
- Timestamp:
- Dec 7, 2009, 3:30:39 PM (15 years ago)
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LMDZ4/branches/LMDZ4-dev/libf/phylmd/cv3_routines.F
r1139 r1276 72 72 c tau = 3000. 73 73 cc tau = 1800. 74 c tau= 2800. 74 75 tau=8000. 75 76 beta = 1.0 - delt/tau … … 2086 2087 cc---end jyg--- 2087 2088 c 2088 c--------retour à la formulation originale d' Emanuel.2089 c--------retour à la formulation originale d''Emanuel. 2089 2090 b6=bfac*50.*sigd(il)*(ph(il,i)-ph(il,i+1))*sigt*afac 2090 2091 c6=water(il,i+1)+bfac*wdtrain(il) … … 2092 2093 if(c6.gt.0.0)then 2093 2094 revap=0.5*(-b6+sqrt(b6*b6+4.*c6)) 2094 evap(il,i)=sigt*afac*revap 2095 water(il,i)=revap*revap 2095 water(il,i)=revap*revap !equation de conservation 2096 2096 else 2097 water(il,i) = 0. 2098 endif 2097 2099 cJYG/IM : ci-dessous formulation originale de KE 2098 2100 c evap(il,i)=-evap(il,i+1) … … 2104 2106 c lorsqu'il y a evaporation totale de la pluie 2105 2107 c 2106 evap(il,i)= +(wdtrain(il)+sigd(il)*wt(il,i)*water(il,i+1)) 2108 c evap(il,i)= +(wdtrain(il)+sigd(il)*wt(il,i)*water(il,i+1)) !itlmd(jyg) 2109 c : /(sigd(il)*(ph(il,i)-ph(il,i+1))*100.) 2110 c end if !itlmd(jyg) 2111 cjyg--- Dans tous les cas, evaporation = [tt ce qui entre dans la couche i] 2112 c moins [tt ce qui sort de la couche i] 2113 evap(il,i)= 2114 : (wdtrain(il)+sigd(il)*wt(il,i)*(water(il,i+1)-water(il,i))) 2107 2115 : /(sigd(il)*(ph(il,i)-ph(il,i+1))*100.) 2108 end if 2116 c 2109 2117 ccc 2110 2118 c *** calculate precipitating downdraft mass flux under ***
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