TYPHOON AND WEATHER IMAGERY

PHILIPPINES WEATHER FORECAST

2026-10-29T23:31:21.590+08:00

⚠ PHILIPPINES 48HRS WEATHER FORECAST

Courtesy of weathermanila
LUZON WEATHER
12HRS	24HRS	36HRS	48HRS
VISAYAS WEATHER
12HRS	24HRS	36HRS	48HRS
MINDANAO WEATHER
12HRS	24HRS	36HRS	48HRS

Para naman sa realtime imagery bisitahin ang link sa ibaba
(For realtime imagery visit the following link below:)
Philippines Doppler radar: https://weathergaines.blogspot.com/2012/08/philippines-doppler-radar-noah.html
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PHILIPPINE SYNOPTIC MAP AND SURFACE WIND

TROPICAL CYCLONE IN-FA

IN-FA

RealEarth

METRO MANILA VISIBLE IR RAINFALL IMAGERY (courtesy of REALEARTH)

NEW PAGASA RADAR SITE (CLICK HERE) https://www.panahon.gov.ph/

10 DAYS RAINFALL FORECAST
12HRS	24HRS	36HRS	48HRS	60HRS
72HRS	84HRS	96HRS	108HRS	120HRS
132HRS	144HRS	156HRS	168HRS	180HRS
192HRS	204HRS	216HRS	228HRS	240HRS

7 DAYS GFS WIND FORECAST
12HRS	24HRS	36HRS	48HRS	60HRS
72HRS	84HRS	96HRS	108HRS	120HRS
132HRS	144HRS	156HRS	168HRS	180HRS

24 HOURS PAGASA WAVE HEIGHT FORECAST
0HRS	6HRS	12HRS	18HRS	24HRS

RELATIVE VORTICITY (UPDATED EVERY 3 HOURS) Vorticity is a measure of curvature in atmospheric flow. A positive value indicates counter clockwise motion in the northern hemisphere and lockwise motion in the southern hemisphere. A positive vorticity environment is conducive to storm development.

WESTERN PACIFIC ANIMATED PRECIPITABLE WATER

DISCLAIMER: These are based on forecast models and realtime charts and imageries and not as an official update. Please don't use this as an official forecast unless official agencies issued warnings or updates. All informations and updates are supported by different data gathered from different agencies which well-analyzed by the author. All imageries are real time and only forecast is subject to changes by author.
CREDITS: weather-forecast.com, Naval Research Laboratory, NOAA, WEATHER ONLINE, PAGASA-DOST, CNN WEATHER, CIMSS
Layout and Discussions Prepared by: Jermaine Christopher Gaines (© 2016 All rights reserved)

TROPICAL DISTURBANCE 96W INVEST

2025-07-16T14:51:00.004+08:00

96W INVEST REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
96W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	96W AUTOMATED DVORAK TECHNIQUE POSITION
96W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
SUBSURFACE TEMP AND OCEAN HEAT CONTENT
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE 03W

2025-06-25T21:20:00.002+08:00

03W THREE REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
03W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	03W AUTOMATED DVORAK TECHNIQUE POSITION
03W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE SEPAT

2025-06-25T20:52:00.002+08:00

02W SEPAT REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
02W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	02W AUTOMATED DVORAK TECHNIQUE POSITION
02W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE WUTIP

2025-06-11T12:51:00.002+08:00

01W WUTIP REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
01W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	01W AUTOMATED DVORAK TECHNIQUE POSITION
01W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE MAN-YI

2024-11-16T16:25:00.000+08:00

25W MAN-YI REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
25W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	25W AUTOMATED DVORAK TECHNIQUE POSITION
25W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE USAGI

2024-11-11T15:23:00.015+08:00

27W USAGI REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
27W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	27W AUTOMATED DVORAK TECHNIQUE POSITION
27W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE TORAJI

2024-11-09T15:23:00.005+08:00

26W TORAJI REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
26W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	26W AUTOMATED DVORAK TECHNIQUE POSITION
26W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE YINXING

2024-11-03T15:56:00.012+08:00

24W YINXING REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
24W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	24W AUTOMATED DVORAK TECHNIQUE POSITION
24W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE KONG-REY

2024-10-25T23:41:00.007+08:00

23W KONG-REY REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
23W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	23W AUTOMATED DVORAK TECHNIQUE POSITION
23W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE TRAMI

2024-10-20T22:26:00.011+08:00

22W TRAMI REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
22W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	22W AUTOMATED DVORAK TECHNIQUE POSITION
22W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)


	TWE

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE KRATHON

2024-09-27T18:05:00.008+08:00

20W KRATHON REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
20W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	20W AUTOMATED DVORAK TECHNIQUE POSITION
20W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE JEBI

2024-09-26T22:54:00.009+08:00

19W JEBI REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
19W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	19W AUTOMATED DVORAK TECHNIQUE POSITION
19W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE CIMARON

2024-09-25T19:32:00.005+08:00

18W CIMARON REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
18W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	18W AUTOMATED DVORAK TECHNIQUE POSITION
18W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE 17W

2024-09-21T21:15:00.004+08:00

17W SEVENTEEN REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
17W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	17W AUTOMATED DVORAK TECHNIQUE POSITION
17W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE SOULIK

2024-09-20T14:40:00.000+08:00

16W SOULIK REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
16W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	16W AUTOMATED DVORAK TECHNIQUE POSITION
16W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE PULASAN

2024-09-16T00:05:00.003+08:00

15W PULASAN REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
15W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	15W AUTOMATED DVORAK TECHNIQUE POSITION
15W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE BEBINCA

2024-09-10T14:12:00.013+08:00

14W BEBINCA REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
14W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	14W AUTOMATED DVORAK TECHNIQUE POSITION
14W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE YAGI

2024-09-02T00:34:00.007+08:00

12W YAGI REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
12W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	12W AUTOMATED DVORAK TECHNIQUE POSITION
12W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE SHANSHAN

2024-08-22T14:44:00.002+08:00

11W SHANSHAN REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
11W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	11W AUTOMATED DVORAK TECHNIQUE POSITION
11W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE JONGDARI

2024-08-19T15:08:00.004+08:00

10W JONGDARI REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
10W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	10W AUTOMATED DVORAK TECHNIQUE POSITION
10W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE WUKONG

2024-08-13T23:08:00.010+08:00

09W WUKONG REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
09W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	09W AUTOMATED DVORAK TECHNIQUE POSITION
09W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE AMPIL

2024-08-12T23:08:00.011+08:00

08W AMPIL REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
08W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	08W AUTOMATED DVORAK TECHNIQUE POSITION
08W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE SON-TINH

2024-08-12T13:28:00.005+08:00

07W SON-TINH REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
07W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	07W AUTOMATED DVORAK TECHNIQUE POSITION
07W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

OTHER SOURCES SELECT BELOW

CLICK LINKS BELOW FOR OTHER REAL TIME (MOST UPDATED) INFORMATIONS

JUST VOTE OR COMMENT FOR FEEDBACK

TROPICAL CYCLONE MARIA

2024-08-07T17:11:00.009+08:00

06W MARIA REAL TIME IMAGERIES

RAINRATE
TROPICAL CYCLONE WARNING SIGNAL
06W 6HRS LOCATION AND HOURLY MARINE SURFACE PLOT	06W AUTOMATED DVORAK TECHNIQUE POSITION
06W WIND RADII [(in nautical miles) 1n.mi. = 1.852km.]	HIMAWARI THERMAL IMAGERY
HIMAWARI VISIBLE IMAGERY	DIAGNOSTIC IMAGERY

HIMAWARI REAL TIME THUNDERSTORM/PRECIPITATION IMAGERY ANIMATION (15/30 MINUTES)

0-1.25mm/hr	1.25-7.5mm/hr	7.5-20mm/hr	20-30mm/hr	30-50mm/hr	+50mm/hr
	Weak TStorm	Strong TStorm	Intense TStorm	Very Int. TStorm	Ext. Int. TStorm

REAL TIME DVORAK TIME SERIES

WIND AND TRACK

MICROWAVE IMAGERY (AVAILABLE IF TC IS PRESENT)

TC-Scale Atmospheric Motion Vectors (AMVs) - CLICK to animate

TROPICAL CYCLONE FORECAST TRACK
JTWC TRACK		PAGASA TRACK

STEERING WIND ANALSIS

700-850mb LAYER STEERING WIND

500-850mb LAYER STEERING WIND

250-850mb LAYER STEERING WIND

ENVIRONMENTAL CONDITIONS

SEA SURFACE TEMPERATURE (CLICK TO VIEW LARGER)	TROPICAL CYCLONE HEAT POTENTIAL (CLICK TO VIEW LARGER)
RELATIVE VORTICITY (CLICK TO VIEW LARGER)	WIND SHEAR AND DIRECTION (CLICK TO VIEW LARGER)
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 environments	UPPER 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
LOW LEVEL WINDS (CLICK TO VIEW LARGER): Mid-level infrared AMVs are utilized to monitor the atmospheric motion in the lower and middle troposphere (above the boundary layer), typically between 500mb and 950mb (explanation of heights) by tracking cloud edges over a sequence of infrared imagery. Low-level rotation of developing tropical waves and mid-level steering currents can be identified by tropical cyclone (TC) forecasters to help determine current atmospheric conditions that could affect TC development, intensity change, and movement	UPPER LEVEL WIND (CLICK TO VIEW LARGER): Upper-level water vapor and infrared AMVs are utilized to monitor the atmospheric motion in the middle and upper troposphere, typically between 100mb and 500mb (explanation of heights). by tracking gradients in a sequence of water vapor imagery and cloud edges in infrared imagery. Jet regions, steering currents, and tropical cyclone (TC) upper-level outflow regions can be identified by TC forecasters to help determine current atmospheric conditions that could affect TC intensity and movement

Tropical Cyclones - Diurnal Pulsing (CLICK TO ANIMATE)

REAL TIME ANIMATION THERMAL/IR - APPROACH

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