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)

JOSE

Maria

LOW 90W

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)

LAS-PINAS, PHILIPPINES EXPERIENCE HAILSTORM

Las-Pinas City particularly parts of Zapote (including our place) in Manila, Philippines experience hailstorms at the height of severe thunderstorms at around 2:30P (0630UTC). My wife and residences here in our area said they saw this very dark cumulonimbo clouds accompanied by strong strikes of lightning and hard louding thunder with strong gust of winds (which i believe an updraft) of up to 60kph or more before the said hail fall. Thanks God no tornado spotted because usually hailstorms followed by a tornado due to strong updraft along the area.


Hail usually forms in cumulonimbus clouds when supercooled water droplets freeze on contact with condensation nuclei. The storm's updraft, with upwardly directed wind speeds as high as 110 miles per hour (180 km/h), blow the hailstones back up the cloud. The updraft dissipates and the hailstones fall down, back into the updraft, and are lifted up again. These type of strong updrafts can also indicate the presence of a tornado. Any thunderstorm which produces hail that reaches the ground is known as a hailstorm. Hail has a diameter of 5 millimetres (0.20 in) or more.


Hail forms in strong thunderstorm clouds, particularly those with intense updrafts, high liquid water content, great vertical extent, large water droplets, and where a good portion of the cloud layer is below freezing 0 °C (32 °F).[1] The growth rate is maximized where air is near a temperature of −13 °C (9 °F). Hail growth becomes vanishingly small when air temperatures fall below −30 °C (−22 °F) as supercooled water droplets become rare at these temperatures.[9] Around thunderstorms, hail is most likely within the cloud at elevations above 20,000 feet (6,100 m). Between 10,000 feet (3,000 m) and 20,000 feet (6,100 m), 60 percent of hail is still within the thunderstorm, though 40 percent now lies within the clear air under the anvil. Below 10,000 feet (3,000 m), hail is equally distributed in and around a thunderstorm to a distance of 2 nautical miles (3.7 km)





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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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