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)

THREE-W/DANTE

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

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DOPPLER RADARs (CREDITS: CLIMATEX)

INDIAN OCEAN DIPOLE, AN EL-NINO OF INDIAN OCEAN




The term Indian Ocean Dipole (IOD) was introduced to denote this basin-wide ocean-atmosphere coupled mode in the Indian Ocean. The positive IOD event is characterized by the strong positive Sea Surface Temperature Anomalies (SSTA) in the tropical western Indian Ocean (50oE-70oE, 10oS-10oN) and the negative SSTA in the southeastern Indian Ocean (90oE- 110oE, 10oS- Eq.). Thus the Indian Ocean Dipole Mode Index (IODMI) is defined as the zonal difference of SST anomaly of western pole from eastern pole.

The Indian Ocean has its own seesaw behavior, the Indian Ocean Dipole. During a so-called positive phase, warmer-than-usual water temperatures in the western Indian Ocean bring heavy rains to East Africa and India and colder-than-usual waters bring drought to Southeast Asia including Philippines. In the negative phase, ocean and monsoonal conditions reverse (colder-than-usual water temperatures in the western Indian Ocean bring drought to East Africa and India and warmer-than-usual waters bring heavy rains to Southeast Asia including Philippines).


The dipole is stronger in September—November and weaker in January—April than in other months and it also appears obviously inter-annual and inter-decadal variations. Although the Indian Ocean dipole in the individual year seems to be independent of ENSO in the equatorial Pacific Ocean, in general, the Indian Ocean dipole has obviously negative correlation with the Pacific Ocean dipole (similar to the inverse phase of ENSO mode). The atmospheric zonal (Walker) circulation over the equator is fundamental to relate the two dipoles to each other.



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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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