subroutine radar_simulator( & hp, & nprof,ngate, & undef, & hgt_matrix,hm_matrix,re_matrix,Np_matrix, & p_matrix,t_matrix,rh_matrix, & Ze_non,Ze_ray,a_to_vol,g_to_vol,dBZe, & g_to_vol_in,g_to_vol_out) use m_mrgrnk use array_lib use math_lib use optics_lib use radar_simulator_types use scale_LUTs_io implicit none ! Purpose: ! Simulates a vertical profile of radar reflectivity ! Originally Part of QuickBeam v1.04 by John Haynes & Roger Marchand. ! but has been substantially modified since that time by ! Laura Fowler and Roger Marchand (see modifications below). ! Inputs: ! [hp] structure that defines hydrometeor types and other radar properties ! [nprof] number of hydrometeor profiles ! [ngate] number of vertical layers ! [undef] missing data value ! (The following 5 arrays must be in order from closest to the radar ! to farthest...) ! [hgt_matrix] height of hydrometeors (km) ! [p_matrix] pressure profile (hPa) ! [t_matrix] temperature profile (K) ! [rh_matrix] relative humidity profile (%) -- only needed if gaseous aborption calculated. ! [hm_matrix] table of hydrometeor mixing rations (g/kg) ! [re_matrix] table of hydrometeor effective radii. 0 ==> use defaults. (units=microns) ! [Np_matrix] table of hydrometeor number concentration. 0 ==> use defaults. (units = 1/kg) ! Outputs: ! [Ze_non] radar reflectivity without attenuation (dBZ) ! [Ze_ray] Rayleigh reflectivity (dBZ) ! [h_atten_to_vol] attenuation by hydromets, radar to vol (dB) ! [g_atten_to_vol] gaseous atteunation, radar to vol (dB) ! [dBZe] effective radar reflectivity factor (dBZ) ! Optional: ! [g_to_vol_in] integrated atten due to gases, r>v (dB). ! If present then is used as gaseous absorption, independently of the ! value in use_gas_abs ! [g_to_vol_out] integrated atten due to gases, r>v (dB). ! If present then gaseous absorption for each profile is returned here. ! Created: ! 11/28/2005 John Haynes (haynes@atmos.colostate.edu) ! Modified: ! 09/2006 placed into subroutine form (Roger Marchand,JMH) ! 08/2007 added equivalent volume spheres, Z and N scalling most distrubtion types (Roger Marchand) ! 01/2008 'Do while' to determine if hydrometeor(s) present in volume ! changed for vectorization purposes (A. Bodas-Salcedo) ! 07/2010 V3.0 ... Modified to load or save scale factors to disk as a Look-Up Table (LUT) ! ... All hydrometeor and radar simulator properties now included in hp structure ! ... hp structure should be initialized by call to radar_simulator_init prior ! ... to calling this subroutine. ! Also ... Support of Morrison 2-moment style microphyscis (Np_matrix) added ! ... Changes implement by Roj Marchand following work by Laura Fowler ! 10/2011 Modified ngate loop to go in either direction depending on flag ! hp%radar_at_layer_one. This affects the direction in which attenuation is summed. ! Also removed called to AVINT for gas and hydrometeor attenuation and replaced with simple ! summation. (Roger Marchand) ! ----- INPUTS ----- logical, parameter :: DO_LUT_TEST = .false. logical, parameter :: DO_NP_TEST = .false. type(class_param), intent(inout) :: hp integer, intent(in) :: nprof,ngate real undef real*8, dimension(nprof,ngate), intent(in) :: & hgt_matrix, p_matrix,t_matrix,rh_matrix real*8, dimension(hp%nhclass,nprof,ngate), intent(in) :: hm_matrix real*8, dimension(hp%nhclass,nprof,ngate), intent(inout) :: re_matrix real*8, dimension(hp%nhclass,nprof,ngate), intent(inout) :: Np_matrix ! ----- OUTPUTS ----- real*8, dimension(nprof,ngate), intent(out) :: Ze_non,Ze_ray, & g_to_vol,dBZe,a_to_vol ! ----- OPTIONAL ----- real*8, optional, dimension(nprof,ngate) :: & g_to_vol_in,g_to_vol_out ! integrated atten due to gases, r>v (dB). This allows to output and then input ! the same gaseous absorption in different calls. Optional to allow compatibility ! with original version. A. Bodas April 2008. ! real*8, dimension(nprof,ngate) :: kr_matrix ! ----- INTERNAL ----- real, parameter :: one_third = 1.0/3.0 real*8 :: t_kelvin integer :: & phase, & ! 0=liquid, 1=ice ns ! number of discrete drop sizes logical :: hydro ! true=hydrometeor in vol, false=none real*8 :: & rho_a, & ! air density (kg m^-3) gases ! function: 2-way gas atten (dB/km) real*8, dimension(:), allocatable :: & Di, Deq, & ! discrete drop sizes (um) Ni, & ! discrete concentrations (cm^-3 um^-1) rhoi ! discrete densities (kg m^-3) real*8, dimension(nprof, ngate) :: & z_vol, & ! effective reflectivity factor (mm^6/m^3) z_ray, & ! reflectivity factor, Rayleigh only (mm^6/m^3) kr_vol, & ! attenuation coefficient hydro (dB/km) g_vol ! attenuation coefficient gases (dB/km) integer,parameter :: KR8 = selected_real_kind(15,300) real*8, parameter :: xx = -1.0_KR8 real*8, dimension(:), allocatable :: xxa real*8 :: kr, ze, zr, pi, scale_factor, tc, Re, ld, tmp1, ze2, kr2, apm, bpm real*8 :: half_a_atten_current,half_a_atten_above real*8 :: half_g_atten_current,half_g_atten_above integer*4 :: tp, i, j, k, pr, itt, iff real*8 step,base, Np integer*4 iRe_type,n,max_bin integer start_gate,end_gate,d_gate logical :: g_to_vol_in_present, g_to_vol_out_present ! Logicals to avoid calling present within the loops g_to_vol_in_present = present(g_to_vol_in) g_to_vol_out_present = present(g_to_vol_out) ! load scaling matricies from disk -- but only the first time this subroutine is called if(hp%load_scale_LUTs) then call load_scale_LUTs(hp) hp%load_scale_LUTs=.false. hp%Z_scale_added_flag = .false. ! will be set true if scaling Look Up Tables are modified during run endif pi = acos(-1.0) ! ----- Initialisation ----- g_to_vol = 0.0 a_to_vol = 0.0 z_vol = 0.0 z_ray = 0.0 kr_vol = 0.0 ! // loop over each range gate (ngate) ... starting with layer closest to the radar ! if(hp%radar_at_layer_one) then start_gate=1 end_gate=ngate d_gate=1 else start_gate=ngate end_gate=1 d_gate=-1 endif DO k=start_gate,end_gate,d_gate ! // loop over each profile (nprof) DO pr=1,nprof t_kelvin = t_matrix(pr,k) ! :: determine if hydrometeor(s) present in volume hydro = .false. DO j=1,hp%nhclass if ((hm_matrix(j,pr,k) > 1E-12) .AND. (hp%dtype(j) > 0)) then hydro = .true. exit endif enddo ! :: if there is hydrometeor in the volume if (hydro) then rho_a = (p_matrix(pr,k)*100.)/(287.0*(t_kelvin)) ! :: loop over hydrometeor type DO tp=1,hp%nhclass if (hm_matrix(tp,pr,k) <= 1E-12) cycle phase = hp%phase(tp) if (phase==0) then itt = infind(hp%mt_ttl,t_kelvin) else itt = infind(hp%mt_tti,t_kelvin) endif if (re_matrix(tp,pr,k).eq.0) then call calc_Re(hm_matrix(tp,pr,k),Np_matrix(tp,pr,k),rho_a, & hp%dtype(tp),hp%dmin(tp),hp%dmax(tp),hp%apm(tp),hp%bpm(tp), & hp%rho(tp),hp%p1(tp),hp%p2(tp),hp%p3(tp),Re) re_matrix(tp,pr,k)=Re else if (Np_matrix(tp,pr,k)>0) then PRINT *, 'Warning: Re and Np set for the same ', & 'volume & hydrometeor type. Np is being ignored.' endif Re = re_matrix(tp,pr,k) endif iRe_type=1 if(Re.gt.0) then ! determine index in to scale LUT ! distance between Re points (defined by "base" and "step") for ! each interval of size Re_BIN_LENGTH ! Integer asignment, avoids calling floor intrinsic n=Re/Re_BIN_LENGTH if (n>=Re_MAX_BIN) n=Re_MAX_BIN-1 step=hp%step_list(n+1) base=hp%base_list(n+1) iRe_type=Re/step if (iRe_type.lt.1) iRe_type=1 Re=step*(iRe_type+0.5) ! set value of Re to closest value allowed in LUT. iRe_type=iRe_type+base-int(n*Re_BIN_LENGTH/step) ! make sure iRe_type is within bounds if (iRe_type.ge.nRe_types) then ! write(*,*) 'Warning: size of Re exceed value permitted ', & ! 'in Look-Up Table (LUT). Will calculate. ' ! no scaling allowed iRe_type=nRe_types hp%Z_scale_flag(tp,itt,iRe_type)=.false. else ! set value in re_matrix to closest values in LUT if (.not. DO_LUT_TEST) re_matrix(tp,pr,k)=Re endif endif ! use Ze_scaled, Zr_scaled, and kr_scaled ... if know them ! if not we will calculate Ze, Zr, and Kr from the distribution parameters if( (.not. hp%Z_scale_flag(tp,itt,iRe_type)) .or. DO_LUT_TEST) then ! :: create a distribution of hydrometeors within volume select case(hp%dtype(tp)) case(4) ns = 1 allocate(Di(ns),Ni(ns),rhoi(ns),xxa(ns),Deq(ns)) Di = hp%p1(tp) Ni = 0. case default ns = nd ! constant defined in radar_simulator_types.f90 allocate(Di(ns),Ni(ns),rhoi(ns),xxa(ns),Deq(ns)) Di = hp%D Ni = 0. end select call dsd(hm_matrix(tp,pr,k),re_matrix(tp,pr,k),Np_matrix(tp,pr,k), & Di,Ni,ns,hp%dtype(tp),rho_a,t_kelvin, & hp%dmin(tp),hp%dmax(tp),hp%apm(tp),hp%bpm(tp), & hp%rho(tp),hp%p1(tp),hp%p2(tp),hp%p3(tp)) ! calculate particle density if (phase == 1) then if (hp%rho(tp) < 0) then ! Use equivalent volume spheres. hp%rho_eff(tp,1:ns,iRe_type) = 917 ! solid ice == equivalent volume approach Deq = ( ( 6/pi*hp%apm(tp)/917 ) ** (1.0/3.0) ) * ( (Di*1E-6) ** (hp%bpm(tp)/3.0) ) * 1E6 ! alternative is to comment out above two lines and use the following block ! MG Mie approach - adjust density of sphere with D = D_characteristic to match particle density ! hp%rho_eff(tp,1:ns,iRe_type) = (6/pi)*hp%apm(tp)*(Di*1E-6)**(hp%bpm(tp)-3) !MG Mie approach ! as the particle size gets small it is possible that the mass to size relationship of ! (given by power law in hclass.data) can produce impossible results ! where the mass is larger than a solid sphere of ice. ! This loop ensures that no ice particle can have more mass/density larger than an ice sphere. ! do i=1,ns ! if(hp%rho_eff(tp,i,iRe_type) > 917 ) then ! hp%rho_eff(tp,i,iRe_type) = 917 ! endif ! enddo else ! Equivalent volume sphere (solid ice rho_ice=917 kg/m^3). hp%rho_eff(tp,1:ns,iRe_type) = 917 Deq=Di * ((hp%rho(tp)/917)**(1.0/3.0)) ! alternative ... coment out above two lines and use the following for MG-Mie ! hp%rho_eff(tp,1:ns,iRe_type) = hp%rho(tp) !MG Mie approach endif else ! I assume here that water phase droplets are spheres. ! hp%rho should be ~ 1000 or hp%apm=524 .AND. hp%bpm=3 Deq = Di endif ! calculate effective reflectivity factor of volume xxa = -9.9 rhoi = hp%rho_eff(tp,1:ns,iRe_type) call zeff(hp%freq,Deq,Ni,ns,hp%k2,t_kelvin,phase,hp%do_ray, & ze,zr,kr,xxa,xxa,rhoi) ! test code ... compare Np value input to routine with sum of DSD ! NOTE: if .not. DO_LUT_TEST, then you are checking the LUT approximation ! not just the DSD representation given by Ni if(Np_matrix(tp,pr,k)>0 .AND. DO_NP_TEST ) then Np = path_integral(Ni,Di,1,ns-1)/rho_a*1E6 ! Note: Representation is not great or small Re < 2 if( (Np_matrix(tp,pr,k)-Np)/Np_matrix(tp,pr,k)>0.1 ) then write(*,*) 'Error: Np input does not match sum(N)' write(*,*) tp,pr,k,Re,Ni(1),Ni(ns),10*log10(ze) write(*,*) Np_matrix(tp,pr,k),Np,(Np_matrix(tp,pr,k)-Np)/Np_matrix(tp,pr,k) write(*,*) endif endif deallocate(Di,Ni,rhoi,xxa,Deq) ! LUT test code ! This segment of code compares full calculation to scaling result if ( hp%Z_scale_flag(tp,itt,iRe_type) .AND. DO_LUT_TEST ) then scale_factor=rho_a*hm_matrix(tp,pr,k) ! if more than 2 dBZe difference print error message/parameters. if ( abs(10*log10(ze) - 10*log10(hp%Ze_scaled(tp,itt,iRe_type) * & scale_factor)) > 2 ) then write(*,*) 'Roj Error: ',tp,itt,iRe_type,hp%Z_scale_flag(tp,itt,iRe_type),n,step,base write(*,*) 10*log10(ze),10*log10(hp%Ze_scaled(tp,itt,iRe_type) * scale_factor) write(*,*) hp%Ze_scaled(tp,itt,iRe_type),scale_factor write(*,*) re_matrix(tp,pr,k),Re write(*,*) endif endif else ! can use z scaling scale_factor=rho_a*hm_matrix(tp,pr,k) zr = hp%Zr_scaled(tp,itt,iRe_type) * scale_factor ze = hp%Ze_scaled(tp,itt,iRe_type) * scale_factor kr = hp%kr_scaled(tp,itt,iRe_type) * scale_factor endif ! end z_scaling kr_vol(pr,k) = kr_vol(pr,k) + kr z_vol(pr,k) = z_vol(pr,k) + ze z_ray(pr,k) = z_ray(pr,k) + zr ! construct Ze_scaled, Zr_scaled, and kr_scaled ... if we can if ( .not. hp%Z_scale_flag(tp,itt,iRe_type) ) then if (iRe_type>1) then scale_factor=rho_a*hm_matrix(tp,pr,k) hp%Ze_scaled(tp,itt,iRe_type) = ze/ scale_factor hp%Zr_scaled(tp,itt,iRe_type) = zr/ scale_factor hp%kr_scaled(tp,itt,iRe_type) = kr/ scale_factor hp%Z_scale_flag(tp,itt,iRe_type) = .true. hp%Z_scale_added_flag(tp,itt,iRe_type)=.true. endif endif enddo ! end loop of tp (hydrometeor type) else ! :: volume is hydrometeor-free kr_vol(pr,k) = 0 z_vol(pr,k) = undef z_ray(pr,k) = undef endif ! :: attenuation due to hydrometeors between radar and volume ! NOTE old scheme integrates attenuation only for the layers ABOVE ! the current layer ... i.e. 1 to k-1 rather than 1 to k ... ! which may be a problem. ROJ ! in the new scheme I assign half the attenuation to the current layer if(d_gate==1) then ! dheight calcuations assumes hgt_matrix points are the cell mid-points. if (k>2) then ! add to previous value to half of above layer + half of current layer a_to_vol(pr,k)= a_to_vol(pr,k-1) + & (kr_vol(pr,k-1)+kr_vol(pr,k))*(hgt_matrix(pr,k-1)-hgt_matrix(pr,k)) else a_to_vol(pr,k)= kr_vol(pr,k)*(hgt_matrix(pr,k)-hgt_matrix(pr,k+1)) endif else ! d_gate==-1 if(k1) then ! add to previous value to half of above layer + half of current layer g_to_vol(pr,k) = g_to_vol(pr,k-1) + & 0.5*(g_vol(pr,k-1)+g_vol(pr,k))*(hgt_matrix(pr,k-1)-hgt_matrix(pr,k)) else g_to_vol(pr,k)= 0.5*g_vol(pr,k)*(hgt_matrix(pr,k)-hgt_matrix(pr,k+1)) endif else ! d_gate==-1 if (k 0)) then Ze_ray(pr,k) = 10*log10(z_ray(pr,k)) else Ze_ray(pr,k) = undef endif if (z_vol(pr,k) > 0) then Ze_non(pr,k) = 10*log10(z_vol(pr,k)) dBZe(pr,k) = Ze_non(pr,k)-a_to_vol(pr,k)-g_to_vol(pr,k) else dBZe(pr,k) = undef Ze_non(pr,k) = undef endif enddo ! end loop over pr (profile) enddo ! end loop of k (range gate) ! Output array with gaseous absorption if (g_to_vol_out_present) g_to_vol_out = g_to_vol ! save any updates made if (hp%update_scale_LUTs) call save_scale_LUTs(hp) end subroutine radar_simulator