subroutine gradients_kcm(profil_flag,rho_v,rho_n,T,dTdp,dPvdp,dPndp) use params_h use gases_h implicit none ! inputs integer profil_flag ! 0 = dry, 1 = moist, 2 = isothermal double precision rho_v,rho_n,T ! outputs double precision dTdp,dPndp,dPvdp double precision a_v ! internal !double precision cp_n,cp_v double precision cp_v double precision press, rho_plus, rho_minus, dVdT, rho_c double precision dlnr,dlna,dpsat,dsv double precision s_minus,s_plus double precision s_v,s_c,L double precision psat_plus,psat_minus,Pn double precision nul ! functions double precision cp_neutral !cp_n = cp_neutral(T) select case(profil_flag) case(2) ! isothermal dTdp = 0. a_v = rho_v/rho_n ! constant here dPndp = 1/(1d0+m_n/m_v*a_v) dPvdp = 1 - dPndp case(1) ! moist Pn = rho_n*T*rmn if(ngasmx.eq.1)then print*,'Cannot have moist adiabat with one gas...' stop endif if(gnom(ngasmx).eq.'H2O')then call psat_H2O(T-2d-1,psat_minus) call psat_H2O(T+2d-1,psat_plus) call psat_H2O(T,press) rho_minus = m_v*psat_minus*1d6/(Rc*(T-2d-1)) rho_plus = m_v*psat_plus*1d6/(Rc*(T+2d-1)) call therm(T-2d-1,rho_minus*1d-3,nul,nul,nul,nul,nul,nul,nul,& nul,nul,press,s_minus,nul) call therm(T+2d-1,rho_plus*1d-3,nul,nul,nul,nul,nul,nul,nul,& nul,nul,press,s_plus,nul) s_c = 2.06 * log(T/273.15) s_plus = s_plus * 1d3 s_minus = s_minus * 1d3 s_c = s_c * 1d3 ! convert to SI if(T.lt.280.0)then dpsat = press*1d6 * ( 1730.63*log(10.) / (T-39.714)**2 ) else call tdpsdt(T,dpsat) dpsat = dpsat * 1d6 / T endif elseif(gnom(ngasmx).eq.'NH3')then call psat_NH3(T-2d-1,psat_minus) call psat_NH3(T+2d-1,psat_plus) call psat_NH3(T,press) rho_minus = m_v*psat_minus*1d6/(Rc*(T-2d-1)) rho_plus = m_v*psat_plus*1d6/(Rc*(T+2d-1)) call latheat_NH3(T-2d-1,nul,s_minus) call latheat_NH3(T+2d-1,nul,s_plus) call latheat_NH3(T,s_c,nul) dpsat = press*1d6 * (-2*1.5609d-4*T + 0.1236) endif dsv = (s_plus-s_minus)/4d-1 ! dsv*T = ds / d ln[T] s_v = (s_plus+s_minus)/2d0 dlnr = T/rho_v * (rho_plus-rho_minus)/4d-1 ! d ln[rho_v] / d ln[T] if(rho_n/rho_v.lt.1e-5)then dlna = -T*dsv/(s_v-s_c) else a_v = rho_v/rho_n dlna = (rmn*dlnr - cp_n + rmn - a_v*T*dsv)/(a_v*(s_v-s_c)+rmn) ! d ln[alpha_v] / d ln[T] ! note cp_n + rmn = cv_n, which is what's required endif dTdp = 1d0 / (dpsat + rho_n*rmn*(1d0 + dlnr - dlna)) ! c.f. Marcq S2.2.2 dPvdp = dTdp * dpsat dPndp = 1d0 - dPvdp ! from p = p_v + p_n case(0) ! dry cp_v=0.0 if(gnom(ngasmx).eq.'H2O')then cp_v = (32.24+1.923d-3*T+1.055d-5*T**2-3.511d-9*T**3)/m_v elseif(gnom(ngasmx).eq.'NH3')then cp_v = 2.058d3 elseif(gnom(ngasmx).eq.'CH4')then cp_v = 2.226d3 endif dTdp = 1/(rho_n*cp_n+rho_v*cp_v) dPndp = 1/(1d0+m_n/m_v*rho_v/rho_n) dPvdp = 1/(1d0+m_v/m_n*rho_n/rho_v) end select end subroutine gradients_kcm