/dports/science/jstrack/jstrack/tracker/storms/old/2010/ |
H A D | nineteen.dis | 26 LIFTS OUT OF THE REGION AFTER ABOUT 36 HOURS. THE MAJORITY OF THE 40 STATES TROUGH. AS THIS FEATURE LIFTS OUT OF THE AREA IN ABOUT 36
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H A D | lisa.dis | 32 INDICATED AS THE TROUGH LIFTS NORTHEASTWARD AND THE SUBTROPICAL 73 AFOREMENTIONED TROUGH LIFTS OUT TO THE NORTHEAST BY 36-48 HOURS... 455 UPPER-LEVEL TROUGH IMPARTING THIS MOTION LIFTS OUT DURING THE NEXT 612 INDICATED AS THE TROUGH LIFTS NORTHEASTWARD AND THE SUBTROPICAL 654 AFOREMENTIONED TROUGH LIFTS OUT TO THE NORTHEAST BY 36-48 HOURS... 1043 UPPER-LEVEL TROUGH IMPARTING THIS MOTION LIFTS OUT DURING THE NEXT
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H A D | richard.dis | 225 PATTERN IS ABOUT TO CHANGE AS THE CURRENT TROUGH TO THE NORTH LIFTS
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H A D | earl.dis | 813 LARGE UPPER TROUGH INTERACTING WITH DANIELLE LIFTS OUT TO THE 941 LARGE UPPER TROUGH INTERACTING WITH DANIELLE LIFTS OUT TO THE
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/dports/multimedia/handbrake/ffmpeg-4.4/libavcodec/ |
H A D | snow_dwt.c | 156 #define LIFTS(src, ref, inv) \ in liftS() macro 161 dst[0] = LIFTS(src[0], mul * 2 * ref[0] + add, inverse); in liftS() 167 dst[i * dst_step] = LIFTS(src[i * src_step], in liftS() 173 dst[w * dst_step] = LIFTS(src[w * src_step], in liftS()
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/dports/emulators/vice/vice-3.5/src/lib/libffmpeg/libavcodec/ |
H A D | snow_dwt.c | 161 #define LIFTS(src, ref, inv) \ in liftS() macro 166 dst[0] = LIFTS(src[0], mul * 2 * ref[0] + add, inverse); in liftS() 172 dst[i * dst_step] = LIFTS(src[i * src_step], in liftS() 178 dst[w * dst_step] = LIFTS(src[w * src_step], in liftS()
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/dports/multimedia/ffmpeg/ffmpeg-4.4.1/libavcodec/ |
H A D | snow_dwt.c | 156 #define LIFTS(src, ref, inv) \ in liftS() macro 161 dst[0] = LIFTS(src[0], mul * 2 * ref[0] + add, inverse); in liftS() 167 dst[i * dst_step] = LIFTS(src[i * src_step], in liftS() 173 dst[w * dst_step] = LIFTS(src[w * src_step], in liftS()
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/dports/multimedia/gstreamer1-libav/gst-libav-1.16.2/gst-libs/ext/libav/libavcodec/ |
H A D | snow_dwt.c | 156 #define LIFTS(src, ref, inv) \ in liftS() macro 161 dst[0] = LIFTS(src[0], mul * 2 * ref[0] + add, inverse); in liftS() 167 dst[i * dst_step] = LIFTS(src[i * src_step], in liftS() 173 dst[w * dst_step] = LIFTS(src[w * src_step], in liftS()
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/dports/www/qt5-webengine/qtwebengine-everywhere-src-5.15.2/src/3rdparty/chromium/third_party/ffmpeg/libavcodec/ |
H A D | snow_dwt.c | 156 #define LIFTS(src, ref, inv) \ in liftS() macro 161 dst[0] = LIFTS(src[0], mul * 2 * ref[0] + add, inverse); in liftS() 167 dst[i * dst_step] = LIFTS(src[i * src_step], in liftS() 173 dst[w * dst_step] = LIFTS(src[w * src_step], in liftS()
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/dports/emulators/libretro-vice/vice-libretro-5725415/vice/src/lib/libffmpeg/libavcodec/ |
H A D | snow_dwt.c | 161 #define LIFTS(src, ref, inv) \ in liftS() macro 166 dst[0] = LIFTS(src[0], mul * 2 * ref[0] + add, inverse); in liftS() 172 dst[i * dst_step] = LIFTS(src[i * src_step], in liftS() 178 dst[w * dst_step] = LIFTS(src[w * src_step], in liftS()
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/dports/www/chromium-legacy/chromium-88.0.4324.182/third_party/ffmpeg/libavcodec/ |
H A D | snow_dwt.c | 156 #define LIFTS(src, ref, inv) \ in liftS() macro 161 dst[0] = LIFTS(src[0], mul * 2 * ref[0] + add, inverse); in liftS() 167 dst[i * dst_step] = LIFTS(src[i * src_step], in liftS() 173 dst[w * dst_step] = LIFTS(src[w * src_step], in liftS()
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/dports/science/jstrack/jstrack/tracker/storms/old/2012/ |
H A D | thirteen.dis | 63 RELATIVELY LOW. AS THIS FEATURE LIFTS OUT DURING THE NEXT DAY OR
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H A D | gordon.dis | 511 TOWARD THE EAST IS EXPECTED AS THE LOW LIFTS OUT TO THE NORTHEAST 567 TROUGH APPROACHES GORDON AND THE LARGER DEEP-LAYER LOW LIFTS 618 DAYS THE CLOSED LOW LIFTS NORTH AND THE AFOREMENTIONED SHORTWAVE
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H A D | patty.dis | 96 NORTHEASTERN CARIBBEAN SEA WEAKENS AND LIFTS OUT NORTHWARD AND TO
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H A D | rafael.dis | 20 RELAXING A BIT AS THE UPPER-LOW SHEARS OUT AND LIFTS NORTHWARD. 743 TROUGH LIFTS OUT TO THE NORTH...RAFAEL IS FORECAST TO TURN EASTWARD
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/dports/sysutils/xvidcap/xvidcap-1.1.7/ffmpeg/libavcodec/ |
H A D | snow.c | 792 #define LIFTS(src, ref, inv) \ in liftS() macro 797 dst[0] = LIFTS(src[0], mul*2*ref[0]+add, inverse); in liftS() 804 LIFTS(src[i*src_step], in liftS() 811 LIFTS(src[w*src_step], mul*2*ref[w*ref_step]+add, inverse); in liftS() 825 #define LIFTS(src, ref, inv) \ in inv_liftS() macro 830 dst[0] = LIFTS(src[0], mul*2*ref[0]+add, inverse); in inv_liftS() 837 LIFTS(src[i*src_step], in inv_liftS() 844 LIFTS(src[w*src_step], mul*2*ref[w*ref_step]+add, inverse); in inv_liftS()
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/dports/science/jstrack/jstrack/tracker/storms/old/2013/ |
H A D | eleven.dis | 73 SHORTWAVE TROUGH TO THE NORTH GRADUALLY LIFTS OUT. THIS SHOULD
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/dports/science/jstrack/jstrack/tracker/storms/old/2011/ |
H A D | ten.dis | 211 THE TROUGH LIFTS OUT AND THE WEAKENING CYCLONE COMES UNDER THE
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H A D | nate.dis | 140 LIFTS NORTHWARD. LATER IN THE FORECAST PERIOD...GLOBAL MODELS SHOW
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H A D | philippe.dis | 273 A SHORTWAVE TROUGH ALONG 40W LIFTS NORTHEASTWARD TOWARDS THE 502 CYCLONE LIFTS NORTH AND A MID-LEVEL ANTICYCLONE BUILDS NORTH OF THE 555 24 TO 36 HOURS AS THE TROUGH TO THE NORTH OF PHILIPPE LIFTS OUT.
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H A D | emily.dis | 330 BAHAMAS IN THE NEXT 24 TO 36 HOURS. AFTER THE TROUGH LIFTS OUT A
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/dports/science/jstrack/jstrack/tracker/storms/old/2008/ |
H A D | omar.dis | 207 THE FORWARD MOTION SLOWS A LITTLE AROUND DAY 3 AS THE TROUGH LIFTS 262 ATLANTIC. A PIECE OF THE TROUGH BREAKS OFF AND LIFTS OUT TO THE
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H A D | hanna.dis | 1323 LARGE MID-LATITUDE TROUGH OVER THE WESTERN ATLANTIC LIFTS NORTHWARD 1379 WESTERN ATLANTIC LIFTS NORTHWARD AND THE SUBTROPICAL RIDGE BUILDS 1445 STATES COAST LIFTS NORTHWARD...ALLOWING THE SUBTROPICAL RIDGE OVER
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/dports/science/jstrack/jstrack/tracker/storms/old/2007/ |
H A D | karen.dis | 241 THE UKMET QUICKLY LIFTS THE SAME TROUGH NORTHWARD BEYOND 72 HOURS
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/dports/science/jstrack/jstrack/tracker/storms/old/2009/ |
H A D | fred.dis | 35 TROUGH THAT CAUSES THE BREAK IN THE RIDGE LIFTS OUT...ALLOWING WEAK
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