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 HAISHEN 05W

TROPICAL CYCLONE HAISHEN 05W (FOR LATEST POSITION, MOVEMENT AND INTENSITY)

REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY

-30°C: +2.5mm; -50°C: +5mm; -70°C: +15mm; -85°C: +25mm -95°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 30 MINUTES)
REAL TIME VISIBLE
REAL TIME WIND AND IR IMAGERY
MICROWAVE IMAGERY
REAL TIME RBTOP IMAGERY WUNDERGROUND REAL TIME IMAGERY
FORECAST TRACKTROPICAL STORM RISK
CLOSE UP RELATIVE VORTICITY (CLICK TO VIEW LARGER) CLOSE UP WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
VISIBLE SATELLITE IMAGERY (WITH SUNSHINE ONLY) VISIBLE MODIS IMAGERY (200M ZOOOM)
REAL TIME DVORAK TIME SERIES 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)

REAL TIME 3 HOURS UPDATED SURFACE WIND AND PRESSURE. CLICK EARTH TO CHANGE VIEW. CLICK MAP TO KNOW VALUE/DATA
CREDIT: EARTH.NULLSCHOOL.NET
REAL TIME WEATHER STATIONS (CLOSEST LAND APPROACH)


MISAMIS STATION


CAMIGUIN STATION


NEGROS STATION


SOUTHERN LEYTE STATION


CEBU STATION


BORACAY STATION


MINDORO STATION
TROPICAL CYCLONE SIGNAL NO: CLICK HERE
CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

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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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