THERMAL IR IMAGERY (PEAK) | PEAK SURFACE WINDSPEED |
TRACK | Multiplatform Tropical Cyclone MSLP and Maximum Winds |
DVORAK GRAPH |
LINK HISTORY
RAMMBCIRA LINK
DIGITAL TYPHOON
DVORAK DATA LINK
ARTICLE
JUST VOTE OR COMMENT FOR FEEDBACK
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.
CLICK IMAGERIES TO REDIRECT ON COMPLETE IMAGERIES AND INFORMATIONS (Imageries will be seen after Philippines imagery below) | ||||
96W/#CrisingPH |
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THERMAL IR IMAGERY (PEAK) | PEAK SURFACE WINDSPEED |
TRACK | Multiplatform Tropical Cyclone MSLP and Maximum Winds |
DVORAK GRAPH |
![]() 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 |