[1047] | 1 | subroutine getslopes(ngrid,geopot) |
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[900] | 2 | |
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[1543] | 3 | use geometry_mod, only: longitude, latitude ! in radians |
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[1047] | 4 | use slope_mod, only: theta_sl, psi_sl |
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[1528] | 5 | use comcstfi_h, only: g, rad, pi |
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| 6 | use mod_phys_lmdz_para, only: is_parallel |
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| 7 | use mod_grid_phy_lmdz, only: nbp_lon, nbp_lat |
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[900] | 8 | implicit none |
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| 9 | |
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| 10 | |
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| 11 | ! This routine computes slope inclination and orientation for the GCM (callslope=.true. in callphys.def) |
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| 12 | ! It works fine with a non-regular grid for zoomed simulations. |
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| 13 | ! slope inclination angle (deg) 0 == horizontal, 90 == vertical |
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| 14 | ! slope orientation angle (deg) 0 == Northward, 90 == Eastward, 180 == Southward, 270 == Westward |
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| 15 | ! TN 04/1013 |
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| 16 | |
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[1047] | 17 | integer,intent(in) :: ngrid ! nnumber of atmospheric columns |
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| 18 | real,intent(in) :: geopot(ngrid) ! geopotential on phy grid |
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[1528] | 19 | real topogrid(nbp_lon,nbp_lat) ! topography on lat/lon grid with poles and only one -180/180 point |
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| 20 | real latigrid(nbp_lon,nbp_lat),longgrid(nbp_lon,nbp_lat) ! meshgrid of latitude and longitude values (radians) |
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[900] | 21 | real theta_val ! slope inclination |
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| 22 | real psi_val ! slope orientation |
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[1528] | 23 | real gradx(nbp_lon,nbp_lat) ! x: latitude-wise topography gradient, increasing northward |
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| 24 | real grady(nbp_lon,nbp_lat) ! y: longitude-wise topography gradient, increasing westward |
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[900] | 25 | integer i,j,ig0 |
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[998] | 26 | integer id2,idm1 ! a trick to compile testphys1d with debug option |
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[900] | 27 | |
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[1528] | 28 | if (is_parallel) then |
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| 29 | ! This routine only works in serial mode so stop now. |
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| 30 | write(*,*) "getslopes Error: this routine is not designed to run in parallel" |
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| 31 | stop |
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| 32 | endif |
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| 33 | |
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[998] | 34 | id2 = 2 |
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[1528] | 35 | idm1 = nbp_lon-1 |
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[900] | 36 | |
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| 37 | ! rearrange topography on a 2d array |
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[1528] | 38 | do j=2,nbp_lat-1 |
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| 39 | ig0= 1+(j-2)*nbp_lon |
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| 40 | do i=1,nbp_lon |
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[900] | 41 | topogrid(i,j)=geopot(ig0+i)/g |
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[1541] | 42 | latigrid(i,j)=latitude(ig0+i) |
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| 43 | longgrid(i,j)=longitude(ig0+i) |
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[900] | 44 | enddo |
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| 45 | enddo |
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| 46 | !poles : |
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| 47 | topogrid(:,1) = geopot(1)/g |
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[1541] | 48 | latigrid(:,1) = latitude(1) |
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| 49 | longgrid(:,1) = longitude(1) |
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[1528] | 50 | topogrid(:,nbp_lat) = geopot(ngrid)/g |
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[1541] | 51 | latigrid(:,nbp_lat) = latitude(ngrid) |
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| 52 | longgrid(:,nbp_lat) = longitude(ngrid) |
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[900] | 53 | |
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| 54 | |
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| 55 | |
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| 56 | ! compute topography gradient |
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| 57 | ! topogrid and rad are both in meters |
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[1528] | 58 | do j=2,nbp_lat-1 |
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| 59 | do i=1,nbp_lon |
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[900] | 60 | gradx(i,j) = (topogrid(i,j+1) - topogrid(i,j-1)) / (latigrid(i,j+1)-latigrid(i,j-1)) |
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| 61 | gradx(i,j) = gradx(i,j) / rad |
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| 62 | enddo |
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[1528] | 63 | grady(1,j) = (topogrid(id2,j) - topogrid(nbp_lon,j)) / (2*pi+longgrid(id2,j)-longgrid(nbp_lon,j)) |
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[900] | 64 | grady(1,j) = grady(1,j) / rad |
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[1528] | 65 | grady(nbp_lon,j) = (topogrid(1,j) - topogrid(idm1,j)) / (2*pi+longgrid(1,j)-longgrid(idm1,j)) |
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| 66 | grady(nbp_lon,j) = grady(nbp_lon,j) / rad |
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| 67 | do i=2,nbp_lon-1 |
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[900] | 68 | grady(i,j) = (topogrid(i+1,j) - topogrid(i-1,j)) / (longgrid(i+1,j)-longgrid(i-1,j)) |
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| 69 | grady(i,j) = grady(i,j) / rad |
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| 70 | enddo |
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| 71 | enddo |
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| 72 | ! poles : |
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| 73 | gradx(:,1) = 0. |
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| 74 | grady(:,1) = 0. |
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[1528] | 75 | gradx(:,nbp_lat) = 0. |
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| 76 | grady(:,nbp_lat) = 0. |
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[900] | 77 | |
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| 78 | |
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| 79 | |
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| 80 | ! compute slope inclination and orientation : |
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| 81 | theta_sl(:) = 0. |
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| 82 | psi_sl(:) = 0. |
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[1528] | 83 | do j=2,nbp_lat-1 |
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| 84 | do i=1,nbp_lon |
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[900] | 85 | |
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[1528] | 86 | ig0= 1+(j-2)*nbp_lon |
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[900] | 87 | |
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| 88 | theta_val=atan(sqrt( (gradx(i,j))**2 + (grady(i,j))**2 )) |
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| 89 | |
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| 90 | psi_val=0. |
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| 91 | if (gradx(i,j) .ne. 0.) psi_val= -pi/2. - atan(grady(i,j)/gradx(i,j)) |
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| 92 | if (gradx(i,j) .ge. 0.) psi_val= psi_val - pi |
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| 93 | psi_val = 3*pi/2. - psi_val |
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| 94 | psi_val = psi_val*180./pi |
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| 95 | psi_val = MODULO(psi_val,360.) |
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| 96 | |
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| 97 | theta_sl(ig0+i) = theta_val |
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| 98 | psi_sl(ig0+i) = psi_val |
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| 99 | |
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| 100 | enddo |
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| 101 | enddo |
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| 102 | |
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| 103 | |
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| 104 | |
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| 105 | end subroutine getslopes |
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