HIMAWARI THERMAL IMAGERY (STATIC)  | 
GEO 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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