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. JULY 03, 2026 SYNOPSIS: Easterlies affecting the eastern sections of Central Luzon, Southern Luzon, and Visayas.

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Showing posts with label #JULY2015. Show all posts
Showing posts with label #JULY2015. Show all posts

TROPICAL CYCLONE FOURTEEN 14W

TROPICAL CYCLONE FOURTEEN 14W (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

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE ONE 01P

TROPICAL CYCLONE ONE 01P (FOR LATEST POSITION, MOVEMENT AND INTENSITY)

REAL TIME CLOSEUP VISIBLE IMAGERY (UPDATED EVERY 10 MINUTES) NEW IMAGERY

REAL TIME THUNDERSTORM/PRECIPONETION IMAGERY (CLICK TO ZOOM IN, CTRL CLICK TO ZOOM OUT)

-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 (UPDATED EVERY 30 MINUTES)
REAL TIME WIND AND IR IMAGERY
REAL TIME MICROWAVE ANIMATION
REAL TIME RBTOP IMAGERY (CLICK IMAGERY TO ANIMATE) WUNDERGROUND REAL TIME IMAGERY
FORECAST TRACK>TROPICAL STORM RISK
GFS AND NAVGEM TRACKGEFS TRACKCMC TRACK
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 (250M 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 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
TROPICAL CYCLONE SIGNAL NO: CLICK HERE
CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE SOUDELOR HANNA 13W SUMMARY

SUPER TYPHOON SOUDELOR HANNA SUMMARY 2015


THERMAL IR IMAGERY (PEAK)

PEAK SURFACE WINDSPEED

TRACK

Multiplatform Tropical Cyclone MSLP and Maximum Winds

DVORAK GRAPH




SUMMARY


CATEGORY: CATEGORY 5 SUPER TYPHOON
BIRTH: 2015-08-01 06:00:00 UTC
DEATH: 2015-08-11 12:00:00 UTC
MAXIMUM WIND: 155kt AND GUST 190kt
LOWEST PRESSURE: 900mb
ACCUMULATED CYCLONE ENERGY: 2.3768E+05
DVORAK MAX WIND: 149.0kt
DVORAK SEA LEVEL PRESSURE: 909.9mb
DVORAK DATA LINK
ARTICLE

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE GUILLERMO 09E


TROPICAL CYCLONE GUILLERMO 09E (POSITION, MOVEMENT AND INTENSITY)

HAWAII DOPPLER RADAR EVERY 10 MINUTES

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

VORTICITY Percent Pixels Colder than -40°C 850-200 hPa Vertical Shear (kt) 850 hPa Horizontal Division (×10-6 s-1)MSLP (hPa)

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