ALL INFORMATIONS AND/OR DATA PUBLISHED ON THIS BLOG ARE SUPPORTED BY ALL WEATHER AGENCIES (SEE BELOW OF THIS BLOG). THIS WAS DONE FOR RECORDS AND USAGE FOR REAL TIME OBSERVATIONS RELEVANT TO TROPICAL CYCLONE INFORMATIONS AND WEATHER UPDATES. KINDLY REFER TO YOUR RESPECTIVE WEATHER AGENCIES FOR UP TO DATE INFORMATIONS. PLEASE REFRESH THIS BLOG TO HAVE AN UP TO DATE SATELLITE IMAGERY.
THERMAL IR IMAGERY (PEAK) | PEAK SURFACE WINDSPEED |
TRACK | Multiplatform Tropical Cyclone MSLP and Maximum Winds |
 REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT)  -30°C: +2.5mm; -50°C: +5mm; -70°C: +15mm; -85°C: +25mm -95°C: +35mm; -110°C: +50mm | REAL TIME DVORAK (FOR REALTIME POSITION) movies (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
 REAL TIME THERMAL IR IMAGERY (UPDATED EVERY 30 MINUTES) | 
REAL TIME VISIBLE (UPDATED EVERY 30 MINUTES) |
 REAL TIME WIND AND IR IMAGERY  |  MICROWAVE REAL TIME IMAGERY |
 REAL TIME RBTOP IMAGERY (CLICK IMAGERY TO ANIMATE) |  WUNDERGROUND REAL TIME IMAGERY |
 FORECAST TRACK | > TROPICAL STORM RISK |
CLOSE UP RELATIVE VORTICITY (CLICK TO VIEW LARGER) |  CLOSE UP WIND SHEAR AND DIRECTION (CLICK TO
VIEW LARGER) |
 VISIBLE SATELLITE IMAGERY
(WITH SUNSHINE ONLY) |  VISIBLE MODIS IMAGERY (250M
ZOOOM) |
 REAL TIME DVORAK TIME SERIES |  SATCON WIND CHART |
 LOW LEVEL CONVERGENCE (CLICK TO VIEW LARGER): To identify potential areas where TC development may occur. Since
the development of the TC secondary circulation (low-level inflow, updrafts in the TC eyewall, and upper-level outflow) is essential in the maturation and sustainment
of a TC, identification of regions where strong TC convergent inflow near the surface can pinpoint those regions which are in favorable environments |  UPPER LEVEL DIVERGENCE (CLICK TO VIEW LARGER): To estimate the strength of the TC secondary circulation, including
the low-level inflow into the TC core, the convective updraft strength within the TC eyewall, and the resulting outflow/venting at the top of the TC. This dynamic can
be important for storm growth and development |
STEERING WIND ANALYSIS (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
 REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) -30°C: +2.5mm; -50°C: +5mm; -70°C: +15mm; -85°C: +25mm -95°C: +35mm; -110°C: +50mm | REAL TIME DVORAK (FOR REALTIME POSITION) movies (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
 REAL TIME THERMAL IR IMAGERY (UPDATED EVERY 30 MINUTES) | 
REAL TIME VISIBLE (UPDATED EVERY 30 MINUTES) |
 REAL TIME WIND AND IR IMAGERY |  REAL TIME DVORAK TIME SERIES |
 REAL TIME RBTOP IMAGERY (CLICK IMAGERY TO ANIMATE) |  WUNDERGROUND REAL TIME IMAGERY |
 FORECAST TRACK | > TROPICAL STORM RISK |
| CLOSE UP RELATIVE VORTICITY (CLICK TO VIEW LARGER) | CLOSE UP WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER) |
 VISIBLE SATELLITE IMAGERY (WITH SUNSHINE ONLY) |  VISIBLE MODIS IMAGERY (250M ZOOOM) |
 SATCON AMSU BRIGHTNESS TEMPERATURE |  SATCON WIND CHART |
| LOW LEVEL CONVERGENCE (CLICK TO VIEW LARGER): To identify potential areas where TC development may occur. Since the development of the TC secondary circulation (low-level inflow, updrafts in the TC eyewall, and upper-level outflow) is essential in the maturation and sustainment of a TC, identification of regions where strong TC convergent inflow near the surface can pinpoint those regions which are in favorable environments | UPPER LEVEL DIVERGENCE (CLICK TO VIEW LARGER): To estimate the strength of the TC secondary circulation, including the low-level inflow into the TC core, the convective updraft strength within the TC eyewall, and the resulting outflow/venting at the top of the TC. This dynamic can be important for storm growth and development |
STEERING WIND ANALYSIS (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
 REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) -30°C: +2.5mm; -50°C: +5mm; -70°C: +15mm; -85°C: +25mm -95°C: +35mm; -110°C: +50mm | REAL TIME DVORAK (FOR REALTIME POSITION) movies (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
 REAL TIME THERMAL IR IMAGERY (UPDATED EVERY 30 MINUTES) | 
REAL TIME VISIBLE (UPDATED EVERY 30 MINUTES) |
 REAL TIME WIND AND IR IMAGERY |  MIOCROWAVE IMAGERY |
 REAL TIME RBTOP IMAGERY (CLICK IMAGERY TO ANIMATE) |  WUNDERGROUND REAL TIME IMAGERY |
 FORECAST TRACK |  TROPICAL STORM RISK |
CLOSE UP RELATIVE VORTICITY (CLICK TO VIEW LARGER) |  CLOSE UP WIND SHEAR AND DIRECTION (CLICK
TO
VIEW LARGER) |
 VISIBLE SATELLITE IMAGERY
(WITH SUNSHINE ONLY) |  VISIBLE MODIS IMAGERY (250M
ZOOOM) |
 REAL TIME DVORAK TIME SERIES |  SATCON WIND CHART |
 LOW LEVEL CONVERGENCE (CLICK TO VIEW LARGER): To identify potential areas where TC development may occur. Since
the development of the TC secondary circulation (low-level inflow, updrafts in the TC eyewall, and upper-level outflow) is essential in the maturation and sustainment
of a TC, identification of regions where strong TC convergent inflow near the surface can pinpoint those regions which are in favorable environments |  UPPER LEVEL DIVERGENCE (CLICK TO VIEW LARGER): To estimate the strength of the TC secondary circulation, including
the low-level inflow into the TC core, the convective updraft strength within the TC eyewall, and the resulting outflow/venting at the top of the TC. This dynamic can
be important for storm growth and development |
STEERING WIND ANALYSIS (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
 VORTICITY |
 Percent Pixels Colder than -40°C |
 850-200 hPa Vertical Shear (kt) |
 850 hPa Horizontal Division (×10-6 s-1) |  MSLP (hPa) |
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