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! $Header$ |
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1920 |
SUBROUTINE ustarhb(knon, u, v, cd_m, ustar) |
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USE dimphy |
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IMPLICIT NONE |
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! ====================================================================== |
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! Laurent Li (LMD/CNRS), le 30 septembre 1998 |
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! Couche limite non-locale. Adaptation du code du CCM3. |
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! Code non teste, donc a ne pas utiliser. |
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! ====================================================================== |
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! Nonlocal scheme that determines eddy diffusivities based on a |
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! diagnosed boundary layer height and a turbulent velocity scale. |
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! Also countergradient effects for heat and moisture are included. |
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! For more information, see Holtslag, A.A.M., and B.A. Boville, 1993: |
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! Local versus nonlocal boundary-layer diffusion in a global climate |
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! model. J. of Climate, vol. 6, 1825-1842. |
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! ====================================================================== |
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include "YOMCST.h" |
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! Arguments: |
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INTEGER knon ! nombre de points a calculer |
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REAL u(klon, klev) ! vitesse U (m/s) |
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REAL v(klon, klev) ! vitesse V (m/s) |
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REAL cd_m(klon) ! coefficient de friction au sol pour vitesse |
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REAL ustar(klon) |
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INTEGER i, k |
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REAL zxt, zxq, zxu, zxv, zxmod, taux, tauy |
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REAL zx_alf1, zx_alf2 ! parametres pour extrapolation |
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LOGICAL unssrf(klon) ! unstb pbl w/lvls within srf pbl lyr |
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LOGICAL unsout(klon) ! unstb pbl w/lvls in outer pbl lyr |
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LOGICAL check(klon) ! True=>chk if Richardson no.>critcal |
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include "YOETHF.h" |
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include "FCTTRE.h" |
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2/2
✓ Branch 0 taken 788452 times.
✓ Branch 1 taken 1920 times.
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790372 |
DO i = 1, knon |
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zx_alf1 = 1.0 |
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zx_alf2 = 1.0 - zx_alf1 |
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zxu = u(i, 1)*zx_alf1 + u(i, 2)*zx_alf2 |
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zxv = v(i, 1)*zx_alf1 + v(i, 2)*zx_alf2 |
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zxmod = 1.0 + sqrt(zxu**2+zxv**2) |
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taux = zxu*zxmod*cd_m(i) |
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tauy = zxv*zxmod*cd_m(i) |
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ustar(i) = sqrt(taux**2+tauy**2) |
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! print*,'Ust ',zxu,zxmod,taux,ustar(i) |
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END DO |
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1920 |
RETURN |
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END SUBROUTINE ustarhb |
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