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.

ACTIVE LOW OR TROPICAL CYCLONES

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

SAOLA

LANGUAGE TRANSLATION

LAS PINAS CITY REALTIME DATA (CREDITS: MANILA OBSERVATORY)

PRESSURE TEMPERATURE RAINFALL WINDSPEED SOLAR RADIATION

PHILIPPINES HIMAWARI SATELLITE IMAGERY (10 MINUTES UPDATE) AND RAINFALL MAP (CREDITS: CLIMATEX)

WESTERN PACIFIC HIMAWARI IR IMAGERY (CLICK LINK TO VIEW)
WESTERN PACIFIC HIMAWARI DAYTIME VISIBLE IMAGERY (CLICK LINK TO VIEW)
HIMAWARI 30MINUTES WATER VAPOR LOOP IMAGERY (CLICK LINK TO VIEW)
HIMAWARI HOURLY FUNKTOP LOOP IMAGERY (RAINFALL) (CLICK LINK TO VIEW)
HIMAWARI CLOUDTOP IMAGERY (THUNDERSTORMS COURTESY OF THAILAND METEOROLOGICAL DEPT.) (CLICK LINK TO VIEW)
BACK TO THERMAL IMAGERY (CLICK LINK TO VIEW)

REAL TIME HOURLY SURFACE WIND AND RAINRATE WITH VALUE

CREDIT: VENTUSKY

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DOPPLER RADARs (CREDITS: CLIMATEX)

TROPICAL CYCLONE GIL 07E


TROPICAL CYCLONE GIL 07E (POSITION, MOVEMENT AND INTENSITY)

REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY
-30°C: +2.5mm; -50°C: +5mm; -70°C: +15mm; -85°C: +25mm -15°C: +35mm; -110°C: +50mm

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






REAL TIME THERMAL IR IMAGERY UPDATED EVERY 15-30MIN
REAL TIME VISIBLE (UPDATED EVERY 30 MINUTES)

REAL TIME WIND AND IR IMAGERY
REAL TIME DVORAK TIME SERIES
WUNDERGROUND REAL TIME IMAGERY REAL TIME RBTOP IMAGERY (CLICK IMAGERY TO ANIMATE)

FORECAST TRACK

TRACK, RAINFALL AND CURRENT INTENSITY (UPDATED EVERY 6 HRS)

RELATIVE VORTICITY

WIND SHEAR


VISIBLE SATELLITE IMAGERY (WITH SUNSHINE ONLY)

VISIBLE MODIS IMAGERY (250M ZOOOM)

SATCON AMSU BRIGHTNESS TEMPERATURE SATCON WIND CHART
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
STEERING WIND ANALSIS
SHALLOW LAYER STEERINGMIDDLE LAYER STEERINGDEEP LAYER STEERING

STEERING WIND ANALYSIS (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT)
CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

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RAPID FIRE STATION

REAL TIME WEATHER NEAR MY PLACE



AYALA ALABANG

TWO FRAME RAINRATE IMAGERY


DMSP SSM/IS RAINRATE

AMSU RAINRATE

NORTH INDIAN OCEAN WESTERN PACIFIC CENTRALPACIFIC
SOUTH INDIAN OCEAN SOUTH PACIFIC OCEAN SOUTH ATLANTIC
EASTERN PACIFIC NORTH ATLANTIC
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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