|   HIMAWARI THERMAL IMAGERY (STATIC) | 
| HIMAWARI VISIBLE LOOP IMAGERY | 
| REAL TIME DVORAK (FOR REALTIME POSITION) movies (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT) | 
|  | REAL TIME 3 HOURS UPDATED SURFACE WIND AND PRESSURE. CLICK EARTH TO CHANGE VIEW. CLICK MAP TO KNOW VALUE/DATA CREDIT: EARTH.NULLSCHOOL.NET | 
|  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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