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 |
 SHALLOW LAYER STEERING |  MIDDLE LAYER STEERING |  DEEP LAYER STEERING |
STEERING WIND ANALYSIS (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
CEBU CITY STATION |
CAMIGUIN STATION |
SOUTHERN LEYTE STATION |
BORACAY STATION |
AKLAN STATION |
ORIEN MINDORO STATION |
TROPICAL CYCLONE SIGNAL NO: CLICK HERE
CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS
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