/dports/math/mdal/MDAL-release-0.9.0/tests/data/flo2d/BarnHDF5/ |
H A D | OUTNQ.OUT | 1 THE MAX Q AT OUTFLOW ELEMENT: 1 IS: 66.61 CFS AT TIME: 1.64 2 THE MAX Q AT OUTFLOW ELEMENT: 2 IS: 30.76 CFS AT TIME: 1.64 3 THE MAX Q AT OUTFLOW ELEMENT: 3 IS: 20.17 CFS AT TIME: 1.67 4 THE MAX Q AT OUTFLOW ELEMENT: 4 IS: 52.57 CFS AT TIME: 1.84 5 THE MAX Q AT OUTFLOW ELEMENT: 5 IS: 75.46 CFS AT TIME: 1.85 6 THE MAX Q AT OUTFLOW ELEMENT: 6 IS: 106.12 CFS AT TIME: 1.84 7 THE MAX Q AT OUTFLOW ELEMENT: 7 IS: 53.45 CFS AT TIME: 1.86 8 THE MAX Q AT OUTFLOW ELEMENT: 8 IS: 16.96 CFS AT TIME: 1.85 9 THE MAX Q AT OUTFLOW ELEMENT: 9 IS: 30.27 CFS AT TIME: 1.87 10 THE MAX Q AT OUTFLOW ELEMENT: 10 IS: 31.00 CFS AT TIME: 1.88 [all …]
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H A D | SUMMARY.OUT | 2 INDICATES EXCESS VOLUME (OUTFLOW + STORAGE > INFLOW) 32 MASS BALANCE INFLOW - OUTFLOW VOLUME 43 *** SURFACE OUTFLOW (ACRE-FT) *** 53 FLOODPLAIN OUTFLOW HYDROGRAPH (W/STREETS) 10.50 17.89 56 FLOODPLAIN OUTFLOW AND STORAGE 21.112 34.680 61 TOTAL SURFACE OUTFLOW AND STORAGE 21.112 69 TOTAL OUTFLOW FROM GRID SYSTEM 10.496 17.886 72 TOTAL VOLUME OF OUTFLOW AND STORAGE 21.112 34.680
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H A D | BASE.OUT | 637 MASS BALANCE INFLOW - OUTFLOW VOLUME 648 *** SURFACE OUTFLOW (ACRE-FT) *** 658 FLOODPLAIN OUTFLOW HYDROGRAPH (W/STREETS) 0.77 1.28 661 FLOODPLAIN OUTFLOW AND STORAGE 21.10 34.65 666 TOTAL SURFACE OUTFLOW AND STORAGE 21.10 674 TOTAL OUTFLOW FROM GRID SYSTEM 0.77 1.28 677 TOTAL VOLUME OF OUTFLOW AND STORAGE 21.10 34.65
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/dports/science/sparta/sparta-20Oct2021/src/KOKKOS/ |
H A D | domain_kokkos.h | 24 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // several files enumerator 53 case OUTFLOW: in collide_kokkos() 54 return OUTFLOW; in collide_kokkos()
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H A D | domain_kokkos.cpp | 34 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // several files enumerator
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H A D | compute_boundary_kokkos.h | 43 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // same as Domain 100 } else if (istyle == OUTFLOW) {
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/dports/science/sparta/sparta-20Oct2021/src/ |
H A D | domain.cpp | 34 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // several files enumerator 159 if (c == 'o') bflag[m] = OUTFLOW; in set_boundary() 294 case OUTFLOW: in collide() 295 return OUTFLOW; in collide()
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H A D | compute_boundary.cpp | 31 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // same as Domain enumerator 208 } else if (istyle == OUTFLOW) { in boundary_tally()
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H A D | dump.cpp | 40 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // same as Domain enumerator 210 else if (domain->bflag[idim*2+iside] == OUTFLOW) boundstr[m++] = 'o'; in init()
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/dports/science/elmerfem/elmerfem-release-9.0/elmerice/examples/Inverse_Methods/src/ |
H A D | MacAyeal_USFs.F90 | 91 FUNCTION OUTFLOW(Model,nodenumber,tx) RESULT(VarOut) function 101 END FUNCTION OUTFLOW
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/dports/cad/calculix/CalculiX/cgx_2.18/examples/airfoil/ISAAC/ |
H A D | isaac.fbl | 10 send all isaac WALL profil TANGENCY wall "SUBSONIC OUTFLOW" out JET in
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/dports/science/jstrack/jstrack/tracker/storms/old/2008/ |
H A D | thirteen.dis | 14 UPPER-LEVEL ANTICYCLONIC FLOW WITH DEVELOPING OUTFLOW. 51 UPPER-LEVEL ANTICYCLONIC FLOW WITH DEVELOPING OUTFLOW.
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H A D | eight.dis | 16 HAS BEEN GRADUALLY ABATING AND THE OUTFLOW IS BECOMING ESTABLISHED 73 HAS BEEN GRADUALLY ABATING AND THE OUTFLOW IS BECOMING ESTABLISHED
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H A D | nine.dis | 11 CYCLONICALLY CURVED BANDS AND A WELL ESTABLISHED OUTFLOW. DVORAK
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H A D | dolly.dis | 82 OUTFLOW IS GRADUALLY EXPANDING...EVEN TO THE WEST...AS WATER VAPOR 200 INFLUENCE. UPPER-LEVEL OUTFLOW IS EXPANDING OVER THE NORTHERN 251 CIRCULATION...AND OUTFLOW CONTINUES TO EXPAND IN ALL QUADRANTS. A 435 OUTFLOW CHANNEL EMANATING FROM THE NORTHWESTERN PART OF THE 438 OUTFLOW IS BEING INHIBITED OVER THE SOUTHERN PART OF THE STORM BY 440 INDICATES A MORE SYMMETRIC OUTFLOW PATTERN EVOLVING OVER THE NEXT 491 BETTER DEFINED OUTFLOW. BEST ESTIMATE OF INITIAL INTENSITY IS 60 583 CYCLONE'S OUTFLOW IS BEGINNING TO BECOME RESTRICTED TO THE WEST BY 636 IN FEEDER BANDS OVER THE PAST SEVERAL HOURS. CIRRUS-LEVEL OUTFLOW
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H A D | seven.dis | 23 STRENGTH OF THE SYSTEM. UPPER-LEVEL OUTFLOW IS WELL-DEFINED OVER
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/dports/science/jstrack/jstrack/tracker/storms/old/2012/ |
H A D | ten.dis | 18 UPPER-LEVEL OUTFLOW FROM TROPICAL STORM ISAAC LATE IN THE FORECAST 77 THE UPPER-LEVEL OUTFLOW FROM TROPICAL STORM ISAAC...AND THE FLOW 79 ATLANTIC...ARE DISTORTING THE OUTFLOW OF TROPICAL DEPRESSION NINE 123 CYCLONE COULD THEN BE AFFECTED BY THE UPPER-LEVEL OUTFLOW OF 194 VERTICAL SHEAR MAY INCREASE DUE TO THE OUTFLOW OF ISAAC.
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H A D | michael.dis | 11 UPPER-LEVEL OUTFLOW...HOWEVER...EXISTS ONLY ON THE EASTERN 215 OUTFLOW ASSOCIATED WITH HURRICANE LESLIE. THE NHC INTENSITY 282 COMPLEX...AND IT IS POSSIBLE THAT THE OUTFLOW FROM LESLIE COULD 339 DUE TO THE OUTFLOW OF HURRICANE LESLIE. THE OFFICIAL FORECAST IS 475 OUTFLOW FROM LESLIE SHOULD PRODUCE STRONG NORTHERLY SHEAR ON THE 579 INCREASE IN NORTHERLY SHEAR...PARTIALLY RELATED TO OUTFLOW FROM 625 OUTFLOW PATTERN. SATELLITE INTENSITY ESTIMATES ARE ABOUT THE 810 SOUTH OF A RIDGE AXIS TO A POSITION UNDERNEATH THE OUTFLOW 871 STRONG NORTH-NORTHEASTERLY SHEAR ASSOCIATED WITH THE OUTFLOW OF 912 ASSOCIATED WITH THE OUTFLOW OF TROPICAL STORM LESLIE...SHOULD [all …]
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/dports/science/jstrack/jstrack/tracker/storms/old/2010/ |
H A D | julia.dis | 126 PORTION OF THE CYCLONE...WHERE THE UPPER-LEVEL OUTFLOW IS THE MOST 139 OUTFLOW ASSOCIATED WITH HURRICANE IGOR WILL CREATE MODERATE TO 305 ASSOCIATED WITH THE OUTFLOW OF HURRICANE IGOR...SHOULD INDUCE 354 TROUGH...PARTIALLY RELATED TO THE OUTFLOW OF HURRICANE IGOR... 409 OUTFLOW HAS BECOME A BIT RESTRICTED TO THE WEST...INDICATIVE OF 434 MID- TO UPPER-LEVEL TROUGH...PARTIALLY RELATED TO THE OUTFLOW OF 441 OUTFLOW FROM HURRICANE IGOR ADVERSELY AFFECTING JULIA. ALTHOUGH 1070 SHEAR...WHICH IS PRIMARILY ASSOCIATED WITH THE MASSIVE OUTFLOW 1223 ASSOCIATED WITH THE OUTFLOW OF HURRICANE IGOR...SHOULD INDUCE 1274 TROUGH...PARTIALLY RELATED TO THE OUTFLOW OF HURRICANE IGOR... [all …]
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H A D | seven.dis | 12 ESTABLISHED UPPER-LEVEL OUTFLOW IN THE WESTERN SEMICIRCLE. 67 ESTABLISHED UPPER-LEVEL OUTFLOW IN THE WESTERN SEMICIRCLE.
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H A D | earl.dis | 201 DEVELOPMENT DUE TO ENHANCED OUTFLOW TO THE NORTH AND SOUTH OF THE 269 SHOULD ACT TO ENHANCE THE OUTFLOW TO THE NORTH AND SOUTH OF THE 305 UPPER-LEVEL OUTFLOW. THIS NORMALLY IS AN INDICATION OF 392 OF DEEP CONVECTION AND FAIR OUTFLOW. DVORAK SATELLITE ESTIMATES 617 FROM SOME MODEST NORTHERLY SHEAR CAUSED BY THE OUTFLOW OF LARGER 1097 IMAGERY SHOWS THAT THE UPPER-LEVEL OUTFLOW IS BEING IMPEDED OVER 1150 SET TO 90 KT FOR THIS ADVISORY. THE OUTFLOW IS IMPROVING IN THE 1379 IMAGERY SHOWS THAT THE UPPER-LEVEL OUTFLOW IS BEING IMPEDED OVER 1435 SET TO 90 KT FOR THIS ADVISORY. THE OUTFLOW IS IMPROVING IN THE 1834 AND THE UPPER-LEVEL OUTFLOW IS WELL-DEFINED OVER ALL BUT THE [all …]
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/dports/science/jstrack/jstrack/tracker/storms/old/2007/ |
H A D | six.dis | 13 WITH PLENTY OF CURVED BANDS AND AN EXPANDING OUTFLOW PATTERN. 87 STRENGTHENING. GIVEN THE GOOD OUTFLOW ALOFT AND THE FORECAST
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H A D | fourteen.dis | 11 ESTABLISHED OUTFLOW. A SHIP LOCATED JUST TO THE NORTH OF THE CENTER 52 TODAY. THERE ARE PATCHES OF DEEP CONVECTION BUT THE OUTFLOW IS
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/dports/science/jstrack/jstrack/tracker/storms/old/2013/ |
H A D | six.dis | 17 THERE IS A WELL-DEFINED UPPER TROPOSPHERIC OUTFLOW PATTERN OVER THE
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/dports/science/jstrack/jstrack/tracker/storms/old/2011/ |
H A D | jose.dis | 16 OF 40-50 KT OVER THE CYCLONE...ASSOCIATED WITH THE OUTFLOW OF 50 OUTFLOW OF HURRICANE IRENE HAS PREVENTED ANY BURST FROM LASTING
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