diff --git a/physics/PBL/MYNN_EDMF/module_bl_mynn.F90 b/physics/PBL/MYNN_EDMF/module_bl_mynn.F90 index 79b9522c5..a0f647083 100644 --- a/physics/PBL/MYNN_EDMF/module_bl_mynn.F90 +++ b/physics/PBL/MYNN_EDMF/module_bl_mynn.F90 @@ -302,7 +302,7 @@ MODULE module_bl_mynn ! Note that the following mixing-length constants are now specified in mym_length ! &cns=3.5, alp1=0.23, alp2=0.3, alp3=3.0, alp4=10.0, alp5=0.2 - real(kind_phys), parameter :: gpw=5./3., qcgmin=1.e-8, qkemin=1.e-12 + real(kind_phys), parameter :: qkemin=1.e-4 real(kind_phys), parameter :: tliq = 269. !all hydrometeors are liquid when T > tliq ! Constants for cloud PDF (mym_condensation) @@ -1932,11 +1932,11 @@ SUBROUTINE mym_length ( & h1=MIN(h1,maxdz) ! 1/2 transition layer depth h2=h1/2.0 ! 1/4 transition layer depth - qkw(kts) = SQRT(MAX(qke(kts),1.0e-10)) + qkw(kts) = SQRT(MAX(qke(kts), qkemin)) DO k = kts+1,kte afk = dz(k)/( dz(k)+dz(k-1) ) abk = 1.0 -afk - qkw(k) = SQRT(MAX(qke(k)*abk+qke(k-1)*afk,1.0e-3)) + qkw(k) = SQRT(MAX(qke(k)*abk+qke(k-1)*afk, qkemin)) END DO elt = 1.0e-5 @@ -1956,7 +1956,7 @@ SUBROUTINE mym_length ( & elt = alp1*elt/vsc vflx = ( vt(kts)+1.0 )*flt +( vq(kts)+tv0 )*flq - vsc = ( gtr*elt*MAX( vflx, 0.0 ) )**(1.0/3.0) + vsc = ( gtr*elt*MAX( vflx, 0.0 ) )**onethird ! ** Strictly, el(i,k=1) is not zero. ** el(kts) = 0.0 @@ -2014,14 +2014,14 @@ SUBROUTINE mym_length ( & h1=MIN(h1,600.) ! 1/2 transition layer depth h2=h1/2.0 ! 1/4 transition layer depth - qtke(kts)=MAX(0.5*qke(kts), 0.01) !tke at full sigma levels + qtke(kts)=MAX(0.5*qke(kts), 0.5*qkemin) !tke at full sigma levels thetaw(kts)=theta(kts) !theta at full-sigma levels - qkw(kts) = SQRT(MAX(qke(kts),1.0e-10)) + qkw(kts) = SQRT(MAX(qke(kts), qkemin)) DO k = kts+1,kte afk = dz(k)/( dz(k)+dz(k-1) ) abk = 1.0 -afk - qkw(k) = SQRT(MAX(qke(k)*abk+qke(k-1)*afk,1.0e-3)) + qkw(k) = SQRT(MAX(qke(k)*abk+qke(k-1)*afk, qkemin)) qtke(k) = 0.5*(qkw(k)**2) ! q -> TKE thetaw(k)= theta(k)*abk + theta(k-1)*afk END DO @@ -2034,14 +2034,14 @@ SUBROUTINE mym_length ( & zwk = zw(k) DO WHILE (zwk .LE. zi2+h1) dzk = 0.5*( dz(k)+dz(k-1) ) - qdz = min(max( qkw(k)-qmin, 0.02 ), 30.0)*dzk + qdz = min(max( qkw(k)-qmin, 0.01 ), 30.0)*dzk elt = elt +qdz*zwk vsc = vsc +qdz k = k+1 zwk = zw(k) END DO - elt = MIN( MAX( alp1*elt/vsc, 10.), 400.) + elt = MIN( MAX( alp1*elt/vsc, 8.), 400.) !avoid use of buoyancy flux functions which are ill-defined at the surface !vflx = ( vt(kts)+1.0 )*flt + ( vq(kts)+tv0 )*flq vflx = fltv @@ -2117,13 +2117,13 @@ SUBROUTINE mym_length ( & h1=MIN(h1,600.) h2=h1*0.5 ! 1/4 transition layer depth - qtke(kts)=MAX(0.5*qke(kts),0.01) !tke at full sigma levels - qkw(kts) = SQRT(MAX(qke(kts),1.0e-4)) + qtke(kts)=MAX(0.5*qke(kts), 0.5*qkemin) !tke at full sigma levels + qkw(kts) = SQRT(MAX(qke(kts), qkemin)) DO k = kts+1,kte afk = dz(k)/( dz(k)+dz(k-1) ) abk = 1.0 -afk - qkw(k) = SQRT(MAX(qke(k)*abk+qke(k-1)*afk,1.0e-3)) + qkw(k) = SQRT(MAX(qke(k)*abk+qke(k-1)*afk, qkemin)) qtke(k) = 0.5*qkw(k)**2 ! qkw -> TKE END DO @@ -3356,8 +3356,8 @@ SUBROUTINE mym_predict (kts,kte, & CALL tridiag2(kte,a,b,c,d,x) DO k=kts,kte -! qke(k)=max(d(k-kts+1), 1.e-4) - qke(k)=max(x(k), 1.e-4) +! qke(k)=max(d(k-kts+1), qkemin) + qke(k)=max(x(k), qkemin) qke(k)=min(qke(k), 150.) ENDDO @@ -6504,11 +6504,11 @@ SUBROUTINE DMP_mf( & do k=kts,kte-1 do I=1,nup edmf_a(K) =edmf_a(K) +UPA(K,i) - edmf_w(K) =edmf_w(K) +rhoz(k)*UPA(K,i)*UPW(K,i) - edmf_qt(K) =edmf_qt(K) +rhoz(k)*UPA(K,i)*UPQT(K,i) - edmf_thl(K)=edmf_thl(K)+rhoz(k)*UPA(K,i)*UPTHL(K,i) - edmf_ent(K)=edmf_ent(K)+rhoz(k)*UPA(K,i)*ENT(K,i) - edmf_qc(K) =edmf_qc(K) +rhoz(k)*UPA(K,i)*UPQC(K,i) + edmf_w(K) =edmf_w(K) +UPA(K,i)*UPW(K,i) + edmf_qt(K) =edmf_qt(K) +UPA(K,i)*UPQT(K,i) + edmf_thl(K)=edmf_thl(K)+UPA(K,i)*UPTHL(K,i) + edmf_ent(K)=edmf_ent(K)+UPA(K,i)*ENT(K,i) + edmf_qc(K) =edmf_qc(K) +UPA(K,i)*UPQC(K,i) enddo enddo do k=kts,kte-1