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/dports/math/dune-pdelab/dune-pdelab-20c7085389d3eb4f8ca99e1bc60f7fa6036536c8/dune/pdelab/constraints/
H A Dconforming.hh193 template<class GFS>
194 void compute_ghosts (const GFS& gfs) in compute_ghosts()
/dports/science/jstrack/jstrack/tracker/storms/old/2017/
H A Dsix.dis22 This scenario is in agreement with the GFS and ECMWF models, which
34 HWRF and GFS solutions, and the slower ECMWF.
H A Dsixteen.dis27 high side of the intensity guidance since much of the GFS-based
41 the representation of the Florida Straits trough. The GFS-based
120 the short term, with the GFS and ECMWF being 90 miles apart on the
122 differences down the road, with the GFS-based guidance moving
218 the guidance envelope. The GFS, on the other hand, shows no such
221 hours because it keeps the ECMWF on an eastern route and the GFS on
323 and UKMET models shifting westward, closer to the previous GFS and
/dports/science/jstrack/jstrack/tracker/storms/old/2012/
H A Deleven.dis30 POINT...AS SHOWN BY THE GFS MODEL.
39 IS CLOSE TO A BLEND OF THE GFS AND ECMWF MODELS THROUGH 72 HOURS
H A Dnine.dis28 TVCA...WHICH IS A COMPROMISE OF THE FASTER GFS MODEL AND SLOWER
87 COAST OF HISPANIOLA...AND THE ECMWF AND GFS ON THE LEFT EDGE
91 IN BEST AGREEMENT WITH A BLEND OF THE GFS AND ECMWF MODELS.
H A Dfive.dis23 MOVES OVER THE CARIBBEAN. THE GFS FORECASTS THE UPPER-LEVEL
27 TOWARD TO THE GFS...BUT TIME WILL TELL.
134 NORTH. THE ECMWF/GFS SOLUTIONS SHOW A STRONGER RIDGE AND MAINTAIN A
137 TO THE MORE RELIABLE ECMWF/GFS OUTPUT ON DAYS 4-5.
H A Dberyl.dis38 MORE RELIABLE ECMWF AND GFS SOLUTIONS AND IS A BIT SOUTH OF THE
107 QUICKLY AHEAD OF THE TROUGH. THE GFS AND GFS ENSEMBLE MEAN SHOW
159 SEVERAL OF THE MODELS INCLUDING THE GFS...GFS ENSEMBLE MEAN...AND
165 FORECAST...WHICH BLENDS THE GFS AND ECMWF GUIDANCE...IS A LITTLE
220 GFS...GFDL...AND HWRF MODELS TAKE BERYL A COUPLE HUNDRED MILES
222 THE GFS AND ECMWF MODELS AND IS VERY SIMILAR TO THE PREVIOUS ONE
344 WILL MOVE OVER NORTHERN FLORIDA OR SOUTHERN GEORGIA. THE GFS
397 FORECAST AS SUGGESTED BY THE GFS.
414 FORWARD SPEED. THE OFFICIAL FORECAST LIES BETWEEN THE GFS AND
776 ESSENTIALLY BLENDS THE ECMWF AND GFS GUIDANCE...WITH MORE
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/dports/science/jstrack/jstrack/tracker/storms/old/2015/
H A Derika.dis29 strength. Meanwhile, the ECMWF and GFS weaken the system in about
46 is close to the ECMWF and GFS ensemble mean, which is south of the
47 consensus but not as far south as the GFS.
92 The GFS weakens Erika to a trough by 5 days while the ECMWF has
109 ensemble mean. This track is to the right of the GFS but well left
341 vortex in the GFS forecast. The HWRF is also very slow to
344 more robust cyclone in its latest forecast, while the GFS, as
502 four and five, but the normally reliable GFS and ECMWF define
575 very close to the consensus of the ECMWF and the GFS models.
769 data will be reflected primarily in the 00Z run of the GFS.
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H A Dida.dis25 variables in the storm's environment than in the GFS. The new
97 trough solution while the GFS has Ida missing the trough and
312 two extremes but leans more toward the GFS, given the current
586 multi-model consensus without the GFS.
729 ECMWF, GFS, and GFS ensemble mean.
792 the GFS ensemble mean and FSU Superensemble.
867 GFS.
1396 and GFS global models show Ida weakening as a result of the
1465 trough as indicated by the GFS.
1760 guidance except for the GFS.
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H A Dfred.dis177 with the GFEX (GFS and ECMWF) consensus model.
304 GFS and ECMWF model tracks.
383 reliable GFS and ECMWF models.
1099 consensus of the GFS and the ECMWF global models.
1367 between the GFS and the multi-model consensus. The GFS insists on
1424 as shown by the GFS and ECMWF models.
1552 GFS and the ECMWF solutions.
1594 after recurvature. This is indicated by the SHIPS/GFS and
1595 SHIPS/ECMWF intensity guidance, and the GFS global model.
1604 GFS and the ECMWF global models.
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H A Dnine.dis22 After that time, the GFS and ECMWF models show the system weakening
32 the middle of the guidance envelope and near a blend of the GFS and
75 agreement with the latest GFS forecast.
181 disturbance weakens. The GFS weakens both the depression and the
248 in best agreement with the GFS and shallow BAM and lies south of the
297 in 4 to 5 days, in best agreement with the latest GFS forecast.
309 motion and is near the shallow BAMS and the GFS.
446 such as the GFS and the GEFS ensemble mean, on the left side of the
483 open up into a trough as shown by the latest GFS and ECMWF
490 agreement with the GFS model. The new NHC track is similar to the
/dports/science/jstrack/jstrack/tracker/storms/old/2007/
H A Dchantal.dis56 MODELS...ESPECIALLY THE GFS...FORECAST THE SYSTEM TO BECOME A
104 SHOWING A SLOWER MOTION THAN EITHER THE GFS OR NOGAPS. THE
106 GFS GLOBAL MEAN ENSEMBLE.
H A Dkaren.dis20 50W-53W...WHILE THE UKMET AND GFS ENSEMBLE MEAN SHOW A
93 HWRF AND GFS TRACKS ARE NEAR THE RIGHT SIDE OF THE GUIDANCE
129 UPPER-TROPOSPHERIC TROUGH THAT THE GFS DEPICTS DEVELOPING IN THE
181 ALLOWING A TURN TOWARD THE NORTHWEST. THE GFS AND UKMET
243 DEVELOPING WEST ATLANTIC RIDGE. THE GFS IS BETWEEN THESE TWO
247 OFFICIAL FORECAST LEANS TOWARD THE GFS SOLUTION BASED ITS PAST
431 THE GFDL/GFS/UKMET MODELS GENERALLY HAVE A WEAKER STORM AT THAT
481 SOLUTION...WHICH IS CLOSE WITH THE GFS AS WELL AS THE PREVIOUS
542 BASED ON THE GFS AND ECMWF SOLUTION AND IS VERY CLOSE TO THE
696 FOLLOWS MOST CLOSELY WITH THE GFDL AND GFS GUIDANCE.
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/dports/science/jstrack/jstrack/tracker/storms/old/2008/
H A Dtwo.dis16 GFS...SUGGESTED THE POSSIBILITY OF GENESIS IN THIS AREA OVER A WEEK
26 GFS/HWRF/GFDL...TURN THE DEPRESSION MORE TOWARD THE NORTHWEST...
/dports/science/jstrack/jstrack/tracker/storms/old/2014/
H A Dnine.dis31 cyclone merging with the frontal system, while the GFS keeps the
136 global models, primarily the GFS and the HWRF, forecast a favorable
150 uncertain, and is based on the blend of the GFS, ECMWF and HWRF
196 hours or so. The GFS changed its tune significantly between the
201 uncertain, primarily since the GFS model could redevelop a cyclone
/dports/cad/jspice3/jspice3-2.5/lib/
H A Dmfbcap119 GFS=\E\E\E\E\E\E\E\E\E\E0$<#3000>\E`\200^L^A,
163 GFS=\E\E\E\E\E\E\E\E\E\E0$<#2500>\E`\100^L^A,
210 GFS=\E\E\E\E\E\E\E\E\E\E0$<#3000>\E`\100^L^A,
584 GFS=\EH\EJ\E*mR\E*dlaeD$<#1000>,
623 MLS#6, SLS=LT%X%+#1%d;, GFS=SP0;, SSLS=LT;,
653 GFS=s(t240)s(t240)s(t120)s(e)\E\\^@,
756 GFS=\E\E\E\E\E\E\E\E\E0$<#2000>\E`\100^L^A,
839 GFS=\017\033%%!3,
898 # GFS
906 GFS=\E[?38l$<#100>\E[!p,
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/dports/sysutils/cluster-glue/Reusable-Cluster-Components-glue--0a7add1d9996/doc/stonith/
H A DREADME.meatware6 This is a port of the "meatware" stomith method found in the GFS
/dports/science/jstrack/jstrack/tracker/storms/old/2011/
H A Dtwelve.dis24 IMPARTED BY THE TROPICAL CYCLONE VORTEX IN THE GFS MODEL FIELDS...
43 MUCH FASTER THAN THE LATEST RUN OF THE GFS.
133 THE LATEST ECMWF AND GFS SOLUTION...BUT LEANS MORE TOWARD THE ECMWF
134 TRACK AS THE GFS SEEMS TO BE TOO SLOW IN THE LATTER PART OF THE
174 FASTEST...WHEREAS THE GFS...HWRF...AND NOGAPS ARE SLOWER.
/dports/math/dune-pdelab/dune-pdelab-20c7085389d3eb4f8ca99e1bc60f7fa6036536c8/dune/pdelab/test/fem/
H A Dtestfemwithgfs.cc39 > GFS; in test_fem() typedef
41 GFS gfs(gv,fem,constraints,vbe); in test_fem()
/dports/math/dune-pdelab/dune-pdelab-20c7085389d3eb4f8ca99e1bc60f7fa6036536c8/dune/pdelab/ordering/
H A Dutility.hh50 template<typename GFS, typename Child, typename TreePath, typename ChildIndex>
51 void afterChild(const GFS& gfs, Child& child, TreePath tp, ChildIndex childIndex) const in afterChild()
/dports/science/jstrack/jstrack/tracker/storms/old/2016/
H A Dmatthew.dis30 takes place and how sharp it will be. The GFS takes the cyclone
33 lies near a consensus of the faster GFS and slower ECMWF.
217 is in best agreement with the GFS and GFS ensemble mean in bringing
630 bit to the west of the GFS/ECMWF blend.
920 the latest GFS track.
1339 Mexico. The 12Z UKMET and 18Z GFS and GFS-ensemble mean models now
1656 near a blend of the 18Z GFS and 12Z ECMWF model solutions.
1997 GFS and ECMWF models.
2098 the GFS, ECMWF, and UKMET models.
2772 this guidance and lies between the GFS and ECMWF.
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/dports/science/jstrack/jstrack/tracker/storms/old/2013/
H A Deleven.dis83 CLOSE TO A BLEND OF THE GFS AND ECMWF MODELS.
85 ALTHOUGH THE GFS-BASED SHIPS INTENSITY MODEL IS ONLY INDICATING 9 KT
92 BY MOST OF THE MODELS...ESPECIALLY THE GFS AND ECMWF...TO MOVE IN
136 STRENGTHENING IS FORECAST IN A DAY OR SO. THE LATEST GFS RUN DOES
146 TURN TOWARD THE RIGHT. THE GFS AND ECMWF GLOBAL MODELS AS WELL AS
202 OFFICIAL TRACK FORECAST IS FAIRLY SIMILAR TO THE LATEST GFS
H A Ddorian.dis74 OF DORIAN. THE GFS...UKMET...AND CANADIAN MODELS MAINTAIN A ROBUST
84 TOWARD THE SLOWER GFS...UKMET...AND CANADIAN MODEL SOLUTIONS.
91 RE-STRENGTHENING TO OCCUR. THE LATEST RUNS OF THE GFS AND ECMWF
241 MODELS...SUCH AS THE GFS RUN OFF THE NEW WCOSS SUPERCOMPUTER...MADE
253 FLOW. GIVEN THAT THE GFS-ENSEMBLE MEAN...HWRF...AND UKMET MODELS
267 TO STRONG SOUTHWESTERLY SHEAR CONDITIONS ACCORDING TO THE GFS AND
307 SHIFTED A LITTLE SOUTHWARD ON THIS CYCLE. THE 18Z RUN OF THE GFS
364 DURING THE FORECAST PERIOD. THE GFS...NAVGEM...AND HWRF ARE THE
377 THE GFS SHOWS CONTINUING SHEAR DURING THIS INTERACTION...THE ECMWF
429 PREVIOUS NHC TRACK AND LEANS TOWARD THE GFS AND HWRF SOLUTIONS.
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/dports/devel/libdap/libdap-3.20.8/tests/dmr-testsuite/
H A Dignore_foreign_xml_3.xml.baseline263 <Value>Analysis from GFS (Global Forecast System)</Value>
275 …ridWriter2)\012Original Dataset = /data/ldm/pub/native/grid/NCEP/GFS/Global_0p25deg/GFS-Global_0p2…
/dports/graphics/tesseract/tesseract-5.0.0/src/lstm/
H A Dlstm.h37 GFS, // Forget gate at the memory, looking back in the other dimension. enumerator

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