WELCOME TO TYPHOON AND WEATHER IMAGERY. THIS BLOG CONTAINS REAL TIME WEATHER, TROPICAL CYCLONE UPDATES AND IMAGERY, AND TROPICAL CYCLONE FORECAST. CONTENTS OF DROP DOWN MENU CAN BE FOUND AFTER PHILIPPINE IMAGERY BELOW (SCROLL DOWNWARD). THANK YOU VERY MUCH FOR VISITING THIS SITE. YOU ARE FREE TO MAKE ANY COMMENT(S) OR FEEDBACK(S) ABOUT THIS BLOG. As of 10PM MARCH 17, 2024 - SYNOPSIS: EASTERLIES AFFECTING THE COUNTRY

ACTIVE LOW OR TROPICAL CYCLONES

CLICK IMAGERIES TO REDIRECT ON COMPLETE IMAGERIES AND INFORMATIONS (Imageries will be seen after Philippines imagery below)

NO ACTIVE SYSTEM

LANGUAGE TRANSLATION

PHILIPPINES RADAR COURTESY OF RAINVIEWER THRU PAGASA DOPPLER RADAR


NCR DOPPLER RADAR

PHILIPPINES DOPPLER RADAR
RealEarth


TROPICAL CYCLONE MARIA

TROPICAL CYCLONE MARIA 15L REAL TIME ANIMATED IMAGERY

GEO THERMAL IMAGERY (STATIC)

GEO VISIBLE LOOP IMAGERY

GEO REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY LOOP (15 MINUTES)

0-1.25mm/hr 1.25-7.5mm/hr 7.5-20mm/hr 20-30mm/hr 30-50mm/hr +50mm/hr
Weak TStorm Strong TStorm Intense TStorm Very Int. TStorm Ext. Int. TStorm

REAL TIME DVORAK (FOR REALTIME POSITION) movies (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT)





REAL TIME DVORAK TIME SERIES
WIND AND TRACK

MICROWAVE IMAGERY



REAL TIME HOURLY SURFACE WIND WITH VALUE.
CREDIT: VENTUSKY

RAINRATE


REAL TIME WITH VALUE.
CREDIT: VENTUSKY

TROPICAL CYCLONE FORECAST TRACK


NHC TRACK

COMPUTER MODEL FORECAST

GFS AND NAVGEM TRACK

GEFS TRACK

CMC TRACK
STEERING WIND ANALSIS

SHALLOW LAYER STEERING

MIDDLE LAYER STEERING

DEEP LAYER STEERING

STEERING WIND ANALYSIS (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT)
ENVIRONMENTAL CONDITIONS

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 environmentsUPPER 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

REAL TIME ANIMATION CLOUDTOP - APPROACH

OTHER SOURCES SELECT BELOW
CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

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VORTICITY Percent Pixels Colder than -40°C 850-200 hPa Vertical Shear (kt) Cloud-cleared Water Vapor Brightness Temperature (°C)MSLP (hPa)

HIMAWARI WESTERN PACIFIC IR TEMPERATURE IMAGERY

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