Changeset 19 for palm/trunk/SOURCE/header.f90
- Timestamp:
- Feb 23, 2007 4:53:48 AM (17 years ago)
- File:
-
- 1 edited
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palm/trunk/SOURCE/header.f90
r4 r19 345 345 ENDIF 346 346 IF ( ibc_pt_t == 0 ) THEN 347 roben = TRIM( roben ) // ' pt(nzt) = pt_top' 348 ELSE 349 roben = TRIM( roben ) // ' pt(nzt) = pt(nzt-1) + dpt/dz' 347 roben = TRIM( roben ) // ' pt(nzt+1) = pt_top' 348 ELSEIF( ibc_pt_t == 1 ) THEN 349 roben = TRIM( roben ) // ' pt(nzt+1) = pt(nzt)' 350 ELSEIF( ibc_pt_t == 2 ) THEN 351 roben = TRIM( roben ) // ' pt(nzt+1) = pt(nzt) + dpt/dz_ini' 350 352 ENDIF 351 353 … … 404 406 IF ( passive_scalar .AND. constant_waterflux ) THEN 405 407 WRITE ( io, 313 ) surface_waterflux 408 ENDIF 409 ENDIF 410 411 IF ( use_top_fluxes ) THEN 412 WRITE ( io, 304 ) 413 IF ( constant_top_heatflux ) THEN 414 WRITE ( io, 306 ) top_heatflux 415 ENDIF 416 IF ( moisture .OR. passive_scalar ) THEN 417 WRITE ( io, 315 ) 406 418 ENDIF 407 419 ENDIF … … 1220 1232 ' B. bound.: ',A/ & 1221 1233 ' T. bound.: ',A) 1222 303 FORMAT (/' Surface fluxes are used in diffusion terms at k=1') 1223 305 FORMAT (//' Prandtl-Layer between surface and first computational ', & 1224 'u,v-level:'// & 1234 303 FORMAT (/' Bottom surface fluxes are used in diffusion terms at k=1') 1235 304 FORMAT (/' Top surface fluxes are used in diffusion terms at k=nzt') 1236 305 FORMAT (//' Prandtl-Layer between bottom surface and first ', & 1237 'computational u,v-level:'// & 1225 1238 ' zp = ',F6.2,' m z0 = ',F6.4,' m kappa = ',F4.2/ & 1226 1239 ' Rif value range: ',F6.2,' <= rif <=',F6.2) … … 1234 1247 313 FORMAT (' Predefined constant scalar flux: ',E10.3,' kg/(m**2 s)') 1235 1248 314 FORMAT (' Predefined scalar value at the surface') 1249 315 FORMAT (' Humidity / scalar flux at top surface is 0.0') 1236 1250 317 FORMAT (//' Lateral boundaries:'/ & 1237 1251 ' left/right: ',A/ &
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