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)

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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)

MOISTURE, VORTICITY, TPW


RELATIVE VORTICITY: Vorticity is a measure of curvature in atmospheric flow. A positive value indicates clockwise motion in the northern hemisphere and counter clockwise motion in the southern hemisphere. A positive vorticity environment is conducive to storm development (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT)


REAL TIME TROPICAL PRECIPITABLE WATER

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NESDIS PRECIPITABLE WATER AND ANOMALIES



VELOCITY POTENTIAL. Velocity potential anomalies are proportional to divergence with GREEN corresponding to regions in which CONVECTION tend to be ENHANCED while BROWN tend to be SUPPRESSED

850 hPa Circulation (kt): The 850 hPa circulation determined from a line integral of the wind component tangent to the boundary of each 5 by 5 degree area

MSLP (hPa)

WIND SHEAR: The 850-200 hPa shear determined by averaging the 850 hPa and 200 hPa wind vectors over each 5 by 5 degree area, and then calculating the magnitude of the shear vector

COLD PIXEL COUNT: The percent of channel 3 pixels colder than -40 °C in each 5° by 5° sub-region. All full disk images within 3 hours after and 6 hours before each synoptic time are include, so that this parameter represents the amount of sustained deep convection

CLOUD-CLEARED WATER VAPOR BRIGHTNESS TEMPERATURE: The average channel 3 brightness temperature over each 5° by 5° sub-region, after the cold pixels in parameter 9 above have been eliminated. This parameter is a measure of mid- to upper-level moisture
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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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