HIMAWARI VISIBLE LOOP IMAGERY |
 HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY LOOP (15 MINUTES) 
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HIMAWARI 10 MINUTE DAYTIME VISIBLE LOOP IMAGERY |
REAL TIME DVORAK (FOR REALTIME POSITION) movies (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |  REAL TIME DVORAK TIME SERIES |
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 JTWC TRACK | ||
 GFS AND NAVGEM TRACK |  GEFS TRACK |  CMC TRACK |
 SHALLOW LAYER STEERING |  MIDDLE LAYER STEERING |  DEEP LAYER STEERING |
STEERING WIND ANALYSIS (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) |
 RELATIVE VORTICITY (CLICK TO VIEW LARGER) |  WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER) |
 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 |
MISAMIS STATION |
CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS
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