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Searched refs:OUTFLOW (Results 1 – 25 of 116) sorted by relevance

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/dports/math/mdal/MDAL-release-0.9.0/tests/data/flo2d/BarnHDF5/
H A DOUTNQ.OUT1 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
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H A DSUMMARY.OUT2 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
H A DBASE.OUT637 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
/dports/science/sparta/sparta-20Oct2021/src/KOKKOS/
H A Ddomain_kokkos.h24 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // several files enumerator
53 case OUTFLOW: in collide_kokkos()
54 return OUTFLOW; in collide_kokkos()
H A Ddomain_kokkos.cpp34 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // several files enumerator
H A Dcompute_boundary_kokkos.h43 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // same as Domain
100 } else if (istyle == OUTFLOW) {
/dports/science/sparta/sparta-20Oct2021/src/
H A Ddomain.cpp34 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()
H A Dcompute_boundary.cpp31 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // same as Domain enumerator
208 } else if (istyle == OUTFLOW) { in boundary_tally()
H A Ddump.cpp40 enum{PERIODIC,OUTFLOW,REFLECT,SURFACE,AXISYM}; // same as Domain enumerator
210 else if (domain->bflag[idim*2+iside] == OUTFLOW) boundstr[m++] = 'o'; in init()
/dports/science/elmerfem/elmerfem-release-9.0/elmerice/examples/Inverse_Methods/src/
H A DMacAyeal_USFs.F9091 FUNCTION OUTFLOW(Model,nodenumber,tx) RESULT(VarOut) function
101 END FUNCTION OUTFLOW
/dports/cad/calculix/CalculiX/cgx_2.18/examples/airfoil/ISAAC/
H A Disaac.fbl10 send all isaac WALL profil TANGENCY wall "SUBSONIC OUTFLOW" out JET in
/dports/science/jstrack/jstrack/tracker/storms/old/2008/
H A Dthirteen.dis14 UPPER-LEVEL ANTICYCLONIC FLOW WITH DEVELOPING OUTFLOW.
51 UPPER-LEVEL ANTICYCLONIC FLOW WITH DEVELOPING OUTFLOW.
H A Deight.dis16 HAS BEEN GRADUALLY ABATING AND THE OUTFLOW IS BECOMING ESTABLISHED
73 HAS BEEN GRADUALLY ABATING AND THE OUTFLOW IS BECOMING ESTABLISHED
H A Dnine.dis11 CYCLONICALLY CURVED BANDS AND A WELL ESTABLISHED OUTFLOW. DVORAK
H A Ddolly.dis82 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
H A Dseven.dis23 STRENGTH OF THE SYSTEM. UPPER-LEVEL OUTFLOW IS WELL-DEFINED OVER
/dports/science/jstrack/jstrack/tracker/storms/old/2012/
H A Dten.dis18 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.
H A Dmichael.dis11 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
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/dports/science/jstrack/jstrack/tracker/storms/old/2010/
H A Djulia.dis126 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...
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H A Dseven.dis12 ESTABLISHED UPPER-LEVEL OUTFLOW IN THE WESTERN SEMICIRCLE.
67 ESTABLISHED UPPER-LEVEL OUTFLOW IN THE WESTERN SEMICIRCLE.
H A Dearl.dis201 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
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/dports/science/jstrack/jstrack/tracker/storms/old/2007/
H A Dsix.dis13 WITH PLENTY OF CURVED BANDS AND AN EXPANDING OUTFLOW PATTERN.
87 STRENGTHENING. GIVEN THE GOOD OUTFLOW ALOFT AND THE FORECAST
H A Dfourteen.dis11 ESTABLISHED OUTFLOW. A SHIP LOCATED JUST TO THE NORTH OF THE CENTER
52 TODAY. THERE ARE PATCHES OF DEEP CONVECTION BUT THE OUTFLOW IS
/dports/science/jstrack/jstrack/tracker/storms/old/2013/
H A Dsix.dis17 THERE IS A WELL-DEFINED UPPER TROPOSPHERIC OUTFLOW PATTERN OVER THE
/dports/science/jstrack/jstrack/tracker/storms/old/2011/
H A Djose.dis16 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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