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 9PM MARCH 27, 2024 - SYNOPSIS: WARM EASTERLIES AFFECTING THE EASTERN SECTION OF 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 HILDA 10E


TROPICAL CYCLONE HILDA 10E (POSITION, MOVEMENT AND INTENSITY)

REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY


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 (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)
GFS AND NAVGEM TRACKGEFS TRACKCMC TRACK

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)

REAL TIME 3 HOURS UPDATED SURFACE WIND AND PRESSURE. CLICK EARTH TO CHANGE VIEW. CLICK MAP TO KNOW VALUE/DATA
CREDIT: EARTH.NULLSCHOOL.NET
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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