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Functions/Subroutines | |
| subroutine | cvtrvf_nerd (F, FN, FSCEXP, H, HN, HPROP, UDEL, VDEL, DM1, ZCONV, SOLSYS, SM, SMH, YASMH, SMI, YASMI, FBOR, MASKTR, MESH, T1, T2, T3, T4, T5, T6, T7, HT, DT, ENTET, MSK, MASKEL, OPTSOU, LIMTRA, KDIR, KDDL, NPTFR, FLBOR, YAFLBOR, UNSV2D, IOPT, FLBORTRA, GLOSEG1, GLOSEG2, NBOR, FLULIM, YAFLULIM, RAIN, PLUIE, TRAIN, GIVEN_FLUX, FLUX_GIVEN, NITMAX) |
Function/Subroutine Documentation
◆ cvtrvf_nerd()
| subroutine cvtrvf_nerd | ( | type(bief_obj), intent(inout) | F, |
| type(bief_obj), intent(in) | FN, | ||
| type(bief_obj), intent(in) | FSCEXP, | ||
| type(bief_obj), intent(in) | H, | ||
| type(bief_obj), intent(in) | HN, | ||
| type(bief_obj), intent(in) | HPROP, | ||
| type(bief_obj), intent(in) | UDEL, | ||
| type(bief_obj), intent(in) | VDEL, | ||
| type(bief_obj), intent(in) | DM1, | ||
| type(bief_obj), intent(in) | ZCONV, | ||
| integer, intent(in) | SOLSYS, | ||
| type(bief_obj), intent(inout) | SM, | ||
| type(bief_obj), intent(in) | SMH, | ||
| logical, intent(in) | YASMH, | ||
| type(bief_obj), intent(in) | SMI, | ||
| logical, intent(in) | YASMI, | ||
| type(bief_obj), intent(inout) | FBOR, | ||
| type(bief_obj), intent(in) | MASKTR, | ||
| type(bief_mesh) | MESH, | ||
| type(bief_obj), intent(inout) | T1, | ||
| type(bief_obj), intent(inout) | T2, | ||
| type(bief_obj), intent(inout) | T3, | ||
| type(bief_obj), intent(inout) | T4, | ||
| type(bief_obj), intent(inout) | T5, | ||
| type(bief_obj), intent(inout) | T6, | ||
| type(bief_obj), intent(inout) | T7, | ||
| type(bief_obj), intent(inout) | HT, | ||
| double precision, intent(in) | DT, | ||
| logical, intent(in) | ENTET, | ||
| logical, intent(in) | MSK, | ||
| type(bief_obj), intent(in) | MASKEL, | ||
| integer, intent(in) | OPTSOU, | ||
| integer, dimension(nptfr), intent(inout) | LIMTRA, | ||
| integer, intent(in) | KDIR, | ||
| integer, intent(in) | KDDL, | ||
| integer, intent(in) | NPTFR, | ||
| type(bief_obj), intent(inout) | FLBOR, | ||
| logical, intent(in) | YAFLBOR, | ||
| type(bief_obj), intent(in) | UNSV2D, | ||
| integer, intent(in) | IOPT, | ||
| type(bief_obj), intent(inout) | FLBORTRA, | ||
| integer, dimension(*), intent(in) | GLOSEG1, | ||
| integer, dimension(*), intent(in) | GLOSEG2, | ||
| integer, dimension(nptfr), intent(in) | NBOR, | ||
| double precision, dimension(*), intent(in) | FLULIM, | ||
| logical, intent(in) | YAFLULIM, | ||
| logical, intent(in) | RAIN, | ||
| type(bief_obj), intent(in) | PLUIE, | ||
| double precision, intent(in) | TRAIN, | ||
| type(bief_obj), intent(in) | GIVEN_FLUX, | ||
| logical, intent(in) | FLUX_GIVEN, | ||
| integer, intent(in) | NITMAX | ||
| ) |
- Parameters
-
[in] optsou DIFT Logical, if yes there is diffusion of f [in] DM1 The piece-wise constant part of advection field IS DM1*GRAD(ZCONV), SEE SOLSYS. [in] DT Time step [in] ENTET Logical, if yes information is given on mass CONSERVATION. [out] F F at time t(n+1) [in] FBOR Dirichlet conditions on f. [in] FLBOR Fluxes at boundaries [in,out] FLBORTRA Tracer fluxes at boundaries [in] FLUX_GIVEN If given_flux=yes, the flux is given in GIVEN_FLUX [in] FN F at time t(n) [in] FSCEXP Explicit part of the source term EQUAL TO ZERO EVERYWHERE BUT ON SOURCES WHERE THERE IS FSCE - (1-TETAT) FN SEE DIFSOU [in] GIVEN_FLUX If given_flux=yes, the flux is given in GIVEN_FLUX AND WILL NOT BE COMPUTED HERE [in] GLOSEG1 First point of segments [in] GLOSEG2 Second point of segments [out] HT Work array (depth going from hn to h) [in] HPROP Propagation depth (done in cvdftr). [in] IOPT Options for computation (number between 0 and 13) THE TENS (IOPT2, I.E. 0 OR 1): 0: UCONV OBEYS THE CONTINUITY EQUATION 1: UCONV DOES NOT OBEY THE CONTINUITY EQUATION THE UNITS (IOPT1, I.E. 0 TO 3): VARIANT FOR FLUXES 0: CONSTANT PER ELEMENT = 0 1: CHI-TUAN PHAM'S CONSTANT 2: N SCHEME 3: PSI SCHEME [in] KDDL Convention for degree of freedom [in] KDIR Convention for dirichlet point [in] LIMTRA Boundary conditions on booundary points [in] MASKEL Masking of elements =1. : NORMAL =0. : MASKED ELEMENT [in] MESH Mesh structure [in] MSK If yes, there is masked elements. [in] NBOR Global numbers of boundary points [in] NITMAX Maximum number of iterations [in] NPTFR Number of boundary points [in] OPTSOU Type of sources 1: NORMAL 2: DIRAC [in] PLUIE Rain or evaporation, in m/s [in] RAIN If yes: rain or evaporation [in] SM Source terms. [in] SMH Source term in continuity equation [in] SMI Implicit source term [in] SOLSYS 1 or 2. if 2 advection field is uconv + dm1*grad(zconv) [in,out] T1 Work bief_obj structure [in,out] T2 Work bief_obj structure [in,out] T3 Work bief_obj structure [in,out] T4 Work bief_obj structure [in,out] T5 Work bief_obj structure [in,out] T6 Work bief_obj structure [in,out] T7 Work bief_obj structure [in] TRAIN Value of tracer in the rain [in] UDEL X-component of advection velocity [in] UNSV2D Inverse of v2dpar [in] VDEL X-component of advection velocity [in] YAFLBOR If yes flbor is given [in] YASMH If yes, smh must be taken into account [in] YASMI If yes, smi must be taken into account [in] ZCONV The piece-wise constant part of advection field IS DM1*GRAD(ZCONV), SEE SOLSYS. [in] kdir DIFT Logical, if yes there is diffusion of f [in] DM1 The piece-wise constant part of advection field IS DM1*GRAD(ZCONV), SEE SOLSYS. [in] DT Time step [in] ENTET Logical, if yes information is given on mass CONSERVATION. [out] F F at time t(n+1) [in] FBOR Dirichlet conditions on f. [in] FLBOR Fluxes at boundaries [in,out] FLBORTRA Tracer fluxes at boundaries [in] FLUX_GIVEN If given_flux=yes, the flux is given in GIVEN_FLUX [in] FN F at time t(n) [in] FSCEXP Explicit part of the source term EQUAL TO ZERO EVERYWHERE BUT ON SOURCES WHERE THERE IS FSCE - (1-TETAT) FN SEE DIFSOU [in] GIVEN_FLUX If given_flux=yes, the flux is given in GIVEN_FLUX AND WILL NOT BE COMPUTED HERE [in] GLOSEG1 First point of segments [in] GLOSEG2 Second point of segments [out] HT Work array (depth going from hn to h) [in] HPROP Propagation depth (done in cvdftr). [in] IOPT Options for computation (number between 0 and 13) THE TENS (IOPT2, I.E. 0 OR 1): 0: UCONV OBEYS THE CONTINUITY EQUATION 1: UCONV DOES NOT OBEY THE CONTINUITY EQUATION THE UNITS (IOPT1, I.E. 0 TO 3): VARIANT FOR FLUXES 0: CONSTANT PER ELEMENT = 0 1: CHI-TUAN PHAM'S CONSTANT 2: N SCHEME 3: PSI SCHEME [in] KDDL Convention for degree of freedom [in] KDIR Convention for dirichlet point [in] LIMTRA Boundary conditions on booundary points [in] MASKEL Masking of elements =1. : NORMAL =0. : MASKED ELEMENT [in] MESH Mesh structure [in] MSK If yes, there is masked elements. [in] NBOR Global numbers of boundary points [in] NITMAX Maximum number of iterations [in] NPTFR Number of boundary points [in] OPTSOU Type of sources 1: NORMAL 2: DIRAC [in] PLUIE Rain or evaporation, in m/s [in] RAIN If yes: rain or evaporation [in] SM Source terms. [in] SMH Source term in continuity equation [in] SMI Implicit source term [in] SOLSYS 1 or 2. if 2 advection field is uconv + dm1*grad(zconv) [in,out] T1 Work bief_obj structure [in,out] T2 Work bief_obj structure [in,out] T3 Work bief_obj structure [in,out] T4 Work bief_obj structure [in,out] T5 Work bief_obj structure [in,out] T6 Work bief_obj structure [in,out] T7 Work bief_obj structure [in] TRAIN Value of tracer in the rain [in] UDEL X-component of advection velocity [in] UNSV2D Inverse of v2dpar [in] VDEL X-component of advection velocity [in] YAFLBOR If yes flbor is given [in] YASMH If yes, smh must be taken into account [in] YASMI If yes, smi must be taken into account [in] ZCONV The piece-wise constant part of advection field IS DM1*GRAD(ZCONV), SEE SOLSYS. [in] nptfr DIFT Logical, if yes there is diffusion of f [in] DM1 The piece-wise constant part of advection field IS DM1*GRAD(ZCONV), SEE SOLSYS. [in] DT Time step [in] ENTET Logical, if yes information is given on mass CONSERVATION. [out] F F at time t(n+1) [in] FBOR Dirichlet conditions on f. [in] FLBOR Fluxes at boundaries [in,out] FLBORTRA Tracer fluxes at boundaries [in] FLUX_GIVEN If given_flux=yes, the flux is given in GIVEN_FLUX [in] FN F at time t(n) [in] FSCEXP Explicit part of the source term EQUAL TO ZERO EVERYWHERE BUT ON SOURCES WHERE THERE IS FSCE - (1-TETAT) FN SEE DIFSOU [in] GIVEN_FLUX If given_flux=yes, the flux is given in GIVEN_FLUX AND WILL NOT BE COMPUTED HERE [in] GLOSEG1 First point of segments [in] GLOSEG2 Second point of segments [out] HT Work array (depth going from hn to h) [in] HPROP Propagation depth (done in cvdftr). [in] IOPT Options for computation (number between 0 and 13) THE TENS (IOPT2, I.E. 0 OR 1): 0: UCONV OBEYS THE CONTINUITY EQUATION 1: UCONV DOES NOT OBEY THE CONTINUITY EQUATION THE UNITS (IOPT1, I.E. 0 TO 3): VARIANT FOR FLUXES 0: CONSTANT PER ELEMENT = 0 1: CHI-TUAN PHAM'S CONSTANT 2: N SCHEME 3: PSI SCHEME [in] KDDL Convention for degree of freedom [in] KDIR Convention for dirichlet point [in] LIMTRA Boundary conditions on booundary points [in] MASKEL Masking of elements =1. : NORMAL =0. : MASKED ELEMENT [in] MESH Mesh structure [in] MSK If yes, there is masked elements. [in] NBOR Global numbers of boundary points [in] NITMAX Maximum number of iterations [in] NPTFR Number of boundary points [in] OPTSOU Type of sources 1: NORMAL 2: DIRAC [in] PLUIE Rain or evaporation, in m/s [in] RAIN If yes: rain or evaporation [in] SM Source terms. [in] SMH Source term in continuity equation [in] SMI Implicit source term [in] SOLSYS 1 or 2. if 2 advection field is uconv + dm1*grad(zconv) [in,out] T1 Work bief_obj structure [in,out] T2 Work bief_obj structure [in,out] T3 Work bief_obj structure [in,out] T4 Work bief_obj structure [in,out] T5 Work bief_obj structure [in,out] T6 Work bief_obj structure [in,out] T7 Work bief_obj structure [in] TRAIN Value of tracer in the rain [in] UDEL X-component of advection velocity [in] UNSV2D Inverse of v2dpar [in] VDEL X-component of advection velocity [in] YAFLBOR If yes flbor is given [in] YASMH If yes, smh must be taken into account [in] YASMI If yes, smi must be taken into account [in] ZCONV The piece-wise constant part of advection field IS DM1*GRAD(ZCONV), SEE SOLSYS. [in] solsys DIFT Logical, if yes there is diffusion of f [in] DM1 The piece-wise constant part of advection field IS DM1*GRAD(ZCONV), SEE SOLSYS. [in] DT Time step [in] ENTET Logical, if yes information is given on mass CONSERVATION. [out] F F at time t(n+1) [in] FBOR Dirichlet conditions on f. [in] FLBOR Fluxes at boundaries [in,out] FLBORTRA Tracer fluxes at boundaries [in] FLUX_GIVEN If given_flux=yes, the flux is given in GIVEN_FLUX [in] FN F at time t(n) [in] FSCEXP Explicit part of the source term EQUAL TO ZERO EVERYWHERE BUT ON SOURCES WHERE THERE IS FSCE - (1-TETAT) FN SEE DIFSOU [in] GIVEN_FLUX If given_flux=yes, the flux is given in GIVEN_FLUX AND WILL NOT BE COMPUTED HERE [in] GLOSEG1 First point of segments [in] GLOSEG2 Second point of segments [out] HT Work array (depth going from hn to h) [in] HPROP Propagation depth (done in cvdftr). [in] IOPT Options for computation (number between 0 and 13) THE TENS (IOPT2, I.E. 0 OR 1): 0: UCONV OBEYS THE CONTINUITY EQUATION 1: UCONV DOES NOT OBEY THE CONTINUITY EQUATION THE UNITS (IOPT1, I.E. 0 TO 3): VARIANT FOR FLUXES 0: CONSTANT PER ELEMENT = 0 1: CHI-TUAN PHAM'S CONSTANT 2: N SCHEME 3: PSI SCHEME [in] KDDL Convention for degree of freedom [in] KDIR Convention for dirichlet point [in] LIMTRA Boundary conditions on booundary points [in] MASKEL Masking of elements =1. : NORMAL =0. : MASKED ELEMENT [in] MESH Mesh structure [in] MSK If yes, there is masked elements. [in] NBOR Global numbers of boundary points [in] NITMAX Maximum number of iterations [in] NPTFR Number of boundary points [in] OPTSOU Type of sources 1: NORMAL 2: DIRAC [in] PLUIE Rain or evaporation, in m/s [in] RAIN If yes: rain or evaporation [in] SM Source terms. [in] SMH Source term in continuity equation [in] SMI Implicit source term [in] SOLSYS 1 or 2. if 2 advection field is uconv + dm1*grad(zconv) [in,out] T1 Work bief_obj structure [in,out] T2 Work bief_obj structure [in,out] T3 Work bief_obj structure [in,out] T4 Work bief_obj structure [in,out] T5 Work bief_obj structure [in,out] T6 Work bief_obj structure [in,out] T7 Work bief_obj structure [in] TRAIN Value of tracer in the rain [in] UDEL X-component of advection velocity [in] UNSV2D Inverse of v2dpar [in] VDEL X-component of advection velocity [in] YAFLBOR If yes flbor is given [in] YASMH If yes, smh must be taken into account [in] YASMI If yes, smi must be taken into account [in] ZCONV The piece-wise constant part of advection field IS DM1*GRAD(ZCONV), SEE SOLSYS.
Definition at line 13 of file cvtrvf_nerd.f.
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