🚨 Kaibab Plateau; Marble and Glen Canyons; Grand Canyon Country; Coconino Plateau; Yavapai County Mountains; Northeast Plateaus and Mesas Hwy 264 Northward; Chinle Valley; Chuska Mountains and Defiance Plateau; Little Colorado River Valley in Coconino County; Little Colorado River Valley in Navajo County; Little Colorado River Valley in Apache County; Western Mogollon Rim; Eastern Mogollon Rim; White Mountains; Northern Gila County; Yavapai County Valleys and Basins; Oak Creek and Sycamore Canyons; Black Mesa Area; Northeast Plateaus and Mesas South of Hwy 264: Red Flag Warning issued June 25 at 10:32AM MST until June 28 at 8:00PM MST by NWS Flagstaff AZ 🚨 Sublette, WY: Severe Thunderstorm Warning issued June 25 at 11:32AM MDT until June 25 at 12:00PM MDT by NWS Riverton WY 🚨 Yosemite NP outside of the valley; Upper San Joaquin River; Kings Canyon NP; Sequoia NP; South End of the Upper Sierra: Wind Advisory issued June 25 at 10:30AM PDT until June 27 at 5:00AM PDT by NWS Hanford CA 🚨 Indian Wells Valley; Mojave Desert: Wind Advisory issued June 25 at 10:30AM PDT until June 28 at 5:00AM PDT by NWS Hanford CA 🚨 Upper St. Bernard; Lower St. Bernard; Western Orleans; Upper Jefferson; Upper Plaquemines; Central Plaquemines; Central Jefferson: Special Weather Statement issued June 25 at 12:30PM CDT by NWS New Orleans LA 🚨 Pratt, KS: Flood Warning issued June 25 at 12:29PM CDT until June 26 at 10:00PM CDT by NWS Dodge City KS 🚨 Western Nevada Basin and Range including Pyramid Lake: Lake Wind Advisory issued June 25 at 10:29AM PDT until June 27 at 11:00PM PDT by NWS Reno NV 🚨 Lassen-Eastern Plumas-Eastern Sierra Counties: Lake Wind Advisory issued June 25 at 10:29AM PDT until June 27 at 11:00PM PDT by NWS Reno NV 🚨 Mineral and Southern Lyon Counties: Lake Wind Advisory issued June 25 at 10:29AM PDT until June 27 at 11:00PM PDT by NWS Reno NV 🚨 Western Nevada Basin and Range including Pyramid Lake: Lake Wind Advisory issued June 25 at 10:29AM PDT until June 25 at 11:00PM PDT by NWS Reno NV
Active Tropical Systems & Formation Outlook
A whole-basin summary of all active tropical cyclones and the NHC
Tropical Weather Outlook, generated with the
tropycal
package. Select a storm below for its official forecast and model guidance.
HAFS and GEFS guidance is only available for storms in the US/NHC domain (Atlantic & East/Central Pacific). For this system, the basin summary and best-track position are shown.
WDPN31 PGTW 251500
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 07W (MEKKHALA) WARNING NR
028//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 25.5N 126.2E
INITIAL INTENSITY: 50 KTS
GEOGRAPHIC REFERENCE: 105 NM SOUTHWEST OF KADENA AB
MOVEMENT PAST 6 HOURS: NORTH-NORTHEASTWARD AT 07 KTS
SIGNIFICANT WAVE HEIGHT: 25 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS TROPICAL
STORM (TS) 07W INCREASINGLY SHEARED WITH THE DEEP CONVECTION
DISPLACED FAR TO THE SOUTHEAST. THE PARTIAL 251202Z METOP-B ASCAT
DATA REVEALED THE STRONGEST WIND SPEEDS IN THE SWATH ARE CONFINED TO
THE SOUTHWESTERN QUADRANT. ADDITIONALLY, SURFACE OBSERVATION STATIONS
FROM NAHA AND KUMEJIMA ARE REPORTING MAXIMUM 23KT SOUTHEASTERLY WINDS,
HOWEVER, THE STORM IS STILL APPROXIMATELY 100 NM AWAY FROM BOTH
STATIONS. ENVIRONMENTAL ANALYSIS REVEALS AN UNFAVORABLE ENVIRONMENT
CHARACTERIZED BY THE VWS, MODERATE OUTFLOW, AND DRY AIR ENTRAINMENT IN
THE NORTHERN HEMISPHERE, MARGINALLY OFFSET, BUT THE WARM (27-28 C) SEA
SURFACE TEMPERATURES. THE INITIAL POSITION AND INTENSITY ARE PLACED
WITH HIGH CONFIDENCE BASED ON THE AFOREMENTIONED 251202Z ASCAT DATA.
INITIAL WIND RADII BASIS: ADJUSTED THE WESTERN SEMICIRCLE BASED ON
THE 251202Z METOP-B ASCAT DATA
CURRENT STEERING MECHANISM: THE WESTERN PERIPHERY OF THE
SUBTROPICAL RIDGE (STR) CENTERED TO THE EAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T3.0 - 45 KTS
RJTD: T3.5 - 55 KTS
RCTP: T2.5 - 35 KTS
KNES: T3.0 - 45 KTS
CIMSS ADT: 47 KTS AT 251300Z
CIMSS AIDT: 43 KTS AT 251300Z
CIMSS D-PRINT: 36 KTS AT 251300Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: UNFAVORABLE
VWS: 15-20 KTS
SST: 27-28 CELSIUS
OUTFLOW: MODERATE EQUATORWARD
ANALYSIS CONFIDENCE:
INITIAL POSITION: HIGH
INITIAL INTENSITY: HIGH
INITIAL WIND RADII: MEDIUM
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO
THE FORECAST FROM THE PREVIOUS WARNING.
FORECAST DISCUSSION: TS 07W IS FORECAST TO CONTINUE ROUNDING THE
STEERING STR CENTERED TO THE EAST AND ACCELERATE NORTHEASTWARD.
MEKKHALA IS EXPECTED TO REACH ITS CLOSEST POINT TO OKINAWA JUST
BEFORE TAU 12, BEFORE TRACKING ALONG THE SOUTHERN COAST OF MAINLAND
JAPAN. AT AROUND TAU 24, 07W WILL ENCOUNTER HIGH (30-35 KTS) VWS
ASSOCIATED WITH THE UPPER-LEVEL WESTERLIES AND SIGNIFICANT DRY AIR
ENTRAINMENT, SHALLOWING THE VORTEX, AND INDUCING EXTRATROPICAL
TRANSITION (ETT). MEKKHALA IS FORECAST TO COMPLETE ETT BY
TAU 48 AS THE STORM PASSES SOUTH OF TOKYO. REGARDING INTENSITY, 07W
IS FORECAST TO GRADUALLY WEAKEN FROM TAU 0 THROUGH THE END OF THE
FORECAST PERIOD AT TAU 48. DESPITE THE HOSTILE ENVIRONMENT, 07W
WILL LIKELY MAINTAIN ITS INTENSITY FAIRLY WELL AS IT UNDERGOES AND
COMPLETES ETT, MAINTAINING GALE FORCE WINDS THROUGH TAU 48.
MODEL DISCUSSION: DETERMINISTIC MODEL TRACK GUIDANCE REMAINS IN
SOLID AGREEMENT THROUGHOUT THE DURATION OF THE FORECAST PERIOD.
THERE IS SLIGHT DISAGREEMENT AMONG MODELS AS 07W IS FORECAST TO
ACCELERATE NORTHEASTWARD, CAUSING MINOR ALONG-TRACK DISCREPANCIES.
THE AI-BASED AND PHYSICS-BASED ECMWF DETERMINISTIC AND ENSEMBLE
TRACKERS REMAIN FASTER THAN OTHER MODELS, BUT THE PREVIOUSLY NOTED
DIFFERENCE HAS SIGNIFICANTLY DECREASED. AS A RESULT, THE JTWC TRACK
FORECAST IS PLACED WITH OVERALL HIGH CONFIDENCE. RELIABLE INTENSITY
AIDS ARE IN GENERAL AGREEMENT THAT 07W WILL GRADUALLY WEAKEN
THROUGH TAU 48, THOUGH THE MESOSCALE MODELS ARE DEPICTING A
SLIGHTLY FASTER RATE OF DECAY. THE JTWC INTENSITY FORECAST LIES
VERY CLOSE TO THE MULTI-MODEL CONSENSUS WITH HIGH CONFIDENCE.
FORECAST CONFIDENCE:
TRACK 00-72 HR: HIGH
INTENSITY 00-72 HR: HIGH//
NNNN
HAFS and GEFS guidance is only available for storms in the US/NHC domain (Atlantic & East/Central Pacific). For this system, the basin summary and best-track position are shown.
WDPN32 PGTW 251500
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 08W (HIGOS) WARNING NR
013//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 21.2N 135.0E
INITIAL INTENSITY: 45 KTS
GEOGRAPHIC REFERENCE: 507 NM SOUTHEAST OF KADENA AB
MOVEMENT PAST 6 HOURS: NORTH-NORTHWESTWARD AT 16 KTS
SIGNIFICANT WAVE HEIGHT: 20 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS THE
LOW-LEVEL CIRCULATION CENTER OF TROPICAL STORM (TS) 08W (HIGOS)
FULLY OBSCURED BENEATH A SHALLOW, BUT PERSISTENT, ELONGATED CENTRAL
DENSE OVERCAST. ADDITIONALLY, ANIMATED EIR DEPICTS DRIER AIR
SURROUNDING THE SYSTEM, IDENTIFIABLE BY THE COMPLETE LACK OF
CONVECTION OUTSIDE THE IMMEDIATE VICINITY OF THE STORM. A 25120Z
PARTIAL METOP-B ASCAT PASS REVEALS THE HIGHEST WIND SPEEDS MEASURED
BY THE SWATH ARE CONFINED TO THE SOUTHEASTERN QUADRANT.
ENVIRONMENTAL ANALYSIS REVEALS A MARGINALLY FAVORABLE ENVIRONMENT,
CHARACTERIZED BY LOW (10-15 KTS) VERTICAL WIND SHEAR (VWS), WARM
(29-30 C) SEA SURFACE TEMPERATURES, OFFSET BY WEAK EQUATORWARD
OUTFLOW AND THE RELATIVELY DRIER SURROUNDING ENVIRONMENT.
INITIAL WIND RADII BASIS: ADJUSTED THE EASTERN WIND RADII USING THE
251201Z PARTIAL ASCAT PASS.
CURRENT STEERING MECHANISM: THE SOUTHWESTERN PERIPHERY OF THE
SUBTROPICAL RIDGE (STR) CENTERED TO THE NORTHEAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T3.5 - 55 KTS
RJTD: T2.5 - 35 KTS
RCTP: T2.5 - 35 KTS
KNES: T3.0 - 45 KTS
CIMSS ADT: 55 KTS AT 251340Z
CIMSS AIDT: 46 KTS AT 251340Z
CIMSS D-PRINT: 37 KTS AT 251340Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINALLY FAVORABLE
VWS: 10-15 KTS
SST: 29-30 CELSIUS
OUTFLOW: WEAK EQUATORWARD
ANALYSIS CONFIDENCE:
INITIAL POSITION: HIGH
INITIAL INTENSITY: HIGH
INITIAL WIND RADII: MEDIUM
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO
THE FORECAST FROM THE PREVIOUS WARNING.
FORECAST DISCUSSION: TS 08W IS FORECASTED TO CONTINUE TRACKING TO
THE NORTH-NORTHWEST ALONG THE SOUTHWESTERN PERIPHERY OF THE STR
POSITIONED TO THE NORTHEAST AND CROSS THE RIDGE AXIS PRIOR TO TAU
12, BEFORE TRACKING NORTH-NORTHEASTWARD UNTIL TAU 36. AT AROUND TAU
12, 08W WILL ENCOUNTER AN INCREASINGLY HOSTILE ENVIRONMENT THAT
WILL INITIATE A QUICK EXTRATROPICAL TRANSITION (ETT) AS THE SYSTEM
BECOMES FULLY EMBEDDED IN THE MID-LATITUDE WESTERLIES. INCREASED
UPPER-LEVEL SUPPORT WILL ASSIST IN SUSTAINING SURFACE INTENSITIES
NEAR 45 KTS BY TAU 36 AS TS 08W BECOMES A VERY SHALLOW, SYMMETRIC
COLD-CORE LOW. THE POSSIBILITY FOR THE SURFACE CIRCULATION TO FILL
INTO AN OPEN TROUGH PERSISTS; HOWEVER, ELEVATED SURFACE
INTENSITIES ARE FORECASTED TO REMAIN UNTIL THE END OF THE FORECAST
PERIOD REGARDLESS OF THE ULTIMATE FATE OF HIGOS. ADDITIONALLY, TS
08W MAY INTERACT WITH TS 07W (MEKKHALA) AS THE TWO STORMS APPROACH
EACH OTHER OFF THE COAST OF MAINLAND JAPAN; HOWEVER, IT IS NOT
EXPECTED THAT THE TWO STORMS WILL MERGE.
MODEL DISCUSSION: DETERMINISTIC MODEL TRACK GUIDANCE IS IN GOOD
AGREEMENT FROM TAU 0-12, BUT IS IN MODERATE AGREEMENT THEREAFTER.
SEVERAL MODELS ARE UNABLE TO TRACK A VORTEX PAST TAU 12 (GSM,
ECMWF DETERMINISTIC, AND EXPERIMENTAL AI), WHILE NAVGEM LOSES THE
CIRCULATION AT TAU 24. AS A RESULT, THE JTWC TRACK FORECAST HAS
BEEN PLACED WITH LOW CONFIDENCE DUE TO UNCERTAINTIES WITH THE
EXPECTED QUICK EXTRATROPICAL TRANSITION OR COMPLETE DISSIPATION
INTO AN OPEN TROUGH. RELIABLE INTENSITY GUIDANCE REMAINS IN
MODERATE AGREEMENT, BUT GENERALLY, RELIABLE MODELS AGREE IN A
SLIGHT INTENSIFICATION PHASE FOLLOWED BY TERMINAL WEAKENING. AS A
RESULT, THE JTWC INTENSITY FORECAST IS ASSESSED WITH MEDIUM
CONFIDENCE.
FORECAST CONFIDENCE:
TRACK 00-72 HR: LOW
INTENSITY 00-72 HR: MEDIUM//
NNNN
ECMWF 10-m Streamlines
This map visualizes near-surface winds from the ECMWF operational model using streamlines — continuous curves that show the direction of the wind at every point. Streamlines help us visually detect patterns of atmospheric flow, such as jets, troughs, and areas of rotation.
Forecasters at the NHC monitor 10-meter wind fields for signs of a closed low-level circulation — a common feature of early tropical cyclone formation. When streamlines wrap into a tight, circular pattern and form a closed loop, it may signal that a system is transitioning from a disorganized disturbance into a structured cyclone.
This early organization of wind flow is a key threshold in classifying an area as a potential tropical cyclone. While other ingredients like convection and mid-level humidity are also necessary, closed low-level circulation is often the first structural milestone forecasters look for.
Look for small, circular loops in the streamlines over oceanic regions — especially where other environmental factors also align for storm formation.
ECMWF Predictions
No active storm found in ECMWF data at this time.
Environmental Indicators
Hypothetical TC Drift Paths
This map displays hypothetical tropical cyclone (TC) paths projected from genesis-favorable zones identified by an environmental mask. These paths are computed using the Emanuel Beta and Advection Model, a physically based framework that estimates the motion of nascent cyclones by combining steering-level winds and planetary rotation effects.
The model blends winds from two critical pressure levels — 850 hPa (lower troposphere) and 250 hPa (upper troposphere) — weighted toward the lower level where most of a tropical cyclone's mass resides. It also incorporates a background component associated with beta drift, which arises from the variation of the Coriolis force with latitude.
Each pink trajectory represents a storm initialized from a grid cell where all five environmental thresholds were favorable: high CAPE, low vertical wind shear, high mid-level humidity, warm SSTs, and positive low-level vorticity. Arrows darken with time, tracing the cyclone’s evolution in 6-hour steps. These tracks can move over land given the steering winds, but in reality these storms weaken quickly when no longer over warm water. This means the tracks that move over significant would likely die out quickly and are not well represented in this model.
Hypothetical storms often drift westward and poleward, steered by large-scale tropical flow and Earth's rotation — this helps forecasters anticipate where early-stage disturbances might evolve into organized storms.
Pressure & Rainfall (hPa)
This chart shows 24-hour forecasts of surface pressure (in hPa) and precipitation (in mm) for select U.S. cities.
The data comes from the Open-Meteo API,
which sources its predictions from high-resolution numerical weather models like ICON (from the German Weather Service)
and ECMWF's IFS. These are advanced general circulation models (GCMs) that solve physical equations governing the
atmosphere — including thermodynamics, fluid motion, and radiation — to simulate and forecast future states of weather.
A sudden drop in pressure may signal the approach of a developing storm system. Increasing rainfall intensity often
tracks with tropical activity or frontal systems. These paired indicators help visualize evolving atmospheric instability and potential hazards.
NBDC Gulf Buoy Data
This data comes from the National Data Buoy Center (NDBC), a division of NOAA responsible for monitoring ocean
and atmospheric conditions using moored buoys, coastal stations, and drifting floats. These sensors play a vital role in
tracking tropical cyclone development by recording variables like wind speed,
barometric pressure, air & sea surface temperatures, and wave height — all of which
help determine storm structure and intensification.
A sudden drop in sea-level pressure or a spike in wind gusts can signal rapid cyclone strengthening.
Water temperature above ~26°C is a key fuel source for tropical cyclones. Wave and swell height give insight
into the storm’s reach and energy transfer across the ocean. Monitoring these in real time helps improve forecasts and early warnings.
Wind: ENE (60°), 5.8 kt | Gust: 7.8 kt
Pressure: 30.10 | Air Temp: 84.4 °F
Water Temp: 85.5 °F | Dew Point: 77.5 °F
Swell: 0.7 ft | Wind Wave: 0.7 ft
NWS U.S. Radar
The National Weather Service (NWS) collects radar data using the NEXRAD (Next Generation Radar) network —
a nationwide system of over 150 high-resolution Doppler radar stations. Radar works by emitting pulses of energy
that bounce off precipitation (like raindrops, hail, or snow) and return to the radar dish. Doppler radar not only detects the
location and intensity of storms, but also their motion — by measuring shifts in frequency caused by movement of particles toward
or away from the radar site. This allows meteorologists to spot rotating storms and potential tornadoes in real time.
GOES 15-min Satellite
The GOES (Geostationary Operational Environmental Satellite) system is operated by NOAA
and provides continuous weather observation over the Americas. Orbiting 22,300 miles above Earth,
GOES satellites deliver high-resolution imagery every 15 minutes, helping track tropical systems, cloud formation,
and atmospheric motion in real time. The Geocolor imagery shown here combines visible and infrared data
to highlight clouds, land, and sea in a natural-looking format.
GOES Band 13 – Infrared (IR) Imagery
Band 13 (10.3 µm) is one of the most important infrared channels for tropical meteorology, measuring emitted radiation from cloud tops.
Colder colors (red, yellow) signal deep convection, where strong thunderstorms punch through the upper atmosphere.
These features often indicate the early stages of tropical cyclone formation.
Most recent GOES Band 13 image. Provided by NOAA/NESDIS/STAR.