🚨 Jackson; Franklin: Special Weather Statement issued September 6 at 12:31AM CDT by NWS Huntsville AL 🚨 Coastal waters east of Ipswich Bay and the Stellwagen Bank National Marine Sanctuary; Coastal waters from Provincetown MA to Chatham MA to Nantucket MA out 20 NM; Coastal Waters extending out to 25 NM South of Marthas Vineyard and Nantucket: Small Craft Advisory issued September 6 at 1:29AM EDT until September 6 at 8:00PM EDT by NWS Boston/Norton MA 🚨 Montgomery: None 🚨 Williamson; Marshall; Rutherford; Bedford: Special Weather Statement issued September 6 at 12:09AM CDT by NWS Nashville TN 🚨 Hunt; Delta; Hopkins: Heat Advisory issued September 6 at 12:09AM CDT until September 6 at 8:00PM CDT by NWS Fort Worth TX 🚨 Fannin; Lamar: Heat Advisory issued September 6 at 12:09AM CDT until September 6 at 8:00PM CDT by NWS Fort Worth TX 🚨 Montague; Cooke; Grayson; Wise; Denton; Collin; Tarrant; Dallas; Rockwall; Kaufman; Van Zandt; Rains; Johnson; Ellis; Henderson; Navarro: Heat Advisory issued September 6 at 12:09AM CDT until September 6 at 8:00PM CDT by NWS Fort Worth TX 🚨 Logan County; Sedgwick County; Phillips County: Special Weather Statement issued September 5 at 11:07PM MDT by NWS Denver CO 🚨 Marion; Baxter; Fulton; Sharp; Randolph; Stone; Izard; Independence; Lawrence; Cleburne; Jackson; Conway; Faulkner; White; Woodruff; Perry; Garland; Saline; Pulaski; Lonoke; Prairie; Monroe; Pike; Clark; Hot Spring; Grant; Jefferson; Arkansas; Dallas; Cleveland; Lincoln; Desha; Ouachita; Calhoun; Bradley; Drew; Boone County Except Southwest; Newton County Higher Elevations; Searcy County Lower Elevations; Southern Johnson County; Southern Pope County; Southeast Van Buren County; Western and Northern Logan County; Northern Scott County; Northwest Yell County; Polk County Lower Elevations; Central and Eastern Montgomery County; Boone County Higher Elevations; Newton County Lower Elevations; Northwest Searcy County Higher Elevations; Johnson County Higher Elevations; Pope County Higher Elevations; Van Buren County Higher Elevations; Southern and Eastern Logan County; Central and Southern Scott County; Yell Excluding Northwest; Northern Polk County Higher Elevations; Northern Montgomery County Higher Elevations; Eastern, Central, and Southern Searcy County Higher Elevations; Southeast Polk County Higher Elevations; Southwest Montgomery County Higher Elevations: Heat Advisory issued September 6 at 12:06AM CDT until September 6 at 8:00PM CDT by NWS Little Rock AR 🚨 Walker; Jefferson: Special Weather Statement issued September 6 at 12:05AM CDT by NWS Birmingham AL
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.
ZCZC MIATCDEP3 ALL
TTAA00 KNHC DDHHMM
Hurricane Marie Discussion Number 20
NWS National Hurricane Center Miami FL EP132026
800 PM PDT Sat Sep 05 2026
The eye of Marie has become increasingly ragged and misshapen over
the past few hours, while cloud tops in its center have begun to
cool. A recent GPM GMI microwave pass from earlier this evening
depicted a vertically aligned cyclone, but the eyewall remained
poorly defined along the western and southwestern sides. Objective
and subjective Dvorak intensity estimates range from 77-94 kt.
However, given the degradation in structure, the initial intensity
is set at 80 kt for this advisory.
Marie is moving northwestward around 6 kt, steered by a strong
mid-level ridge anchored over the central United States. This
general motion is forecast to continue through Sunday. As Marie
weakens and becomes more shallow, a turn back toward the
west-northwest is forecast as the cyclone becomes increasingly
steered by the low-level flow. By midweek, a closed low moving
southward along the U.S. West Coast is expected to induce an
acceleration toward the northwestward, followed by a turn toward the
north.
Environmental conditions are expected to gradually become less
favorable over the next couple days as Marie moves over cooler sea
surface temperatures, resulting in slow weakening into early next
week. More rapid weakening is anticipated thereafter as increasing
wind shear decouples the cyclone and displaces any remaining
convection well to the north of its center. The latest NHC forecast
calls for Marie to become a post-tropical remnant low by 96 h,
followed by dissipation by 120 h. The NHC track and intensity
forecasts are very close to the HCCA and Google DeepMind consensus
aids.
FORECAST POSITIONS AND MAX WINDS
INIT 06/0300Z 22.6N 121.3W 80 KT 90 MPH
12H 06/1200Z 23.2N 122.0W 70 KT 80 MPH
24H 07/0000Z 24.0N 122.9W 60 KT 70 MPH
36H 07/1200Z 24.6N 124.1W 55 KT 65 MPH
48H 08/0000Z 25.2N 125.4W 50 KT 60 MPH
60H 08/1200Z 26.1N 126.6W 45 KT 50 MPH
72H 09/0000Z 27.5N 127.5W 40 KT 45 MPH
96H 10/0000Z 31.4N 129.2W 30 KT 35 MPH...POST-TROP/REMNT LOW
120H 11/0000Z...DISSIPATED
$$
Forecaster Adams
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.
WDPN31 PGTW 060300
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL DEPRESSION 22W (KROVANH)
WARNING NR 020//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 25.9N 129.7E
INITIAL INTENSITY: 30 KTS
GEOGRAPHIC REFERENCE: 108 NM EAST-SOUTHEAST OF KADENA AB
MOVEMENT PAST 6 HOURS: NORTHEASTWARD AT 07 KTS
SIGNIFICANT WAVE HEIGHT: 14 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS THE
REEMERGENCE OF THE LOOSE, POORLY DEFINED LOW LEVEL CIRCULATION FROM
UNDER OBSCURING CONVECTION AND CIRRUS IN THE LAST FEW HOURS. IT
APPEARS THAT THE LOW-LEVEL CIRCULATION CENTER (LLCC) THAT HAD BEEN
PREVIOUSLY TRACKED HAS RECONSTITUTED ITSELF IN THE VICINITY OF
LOCALIZED DEEP CONVECTION EAST OF OKINAWA. THAT CONVECTION IS
DISSIPATING AND A NEW BURST OF CONVECTION IS BEGINNING TO WRAP
AROUND THE WESTERN SIDE OF THE ASSESSED CIRCULATION CENTER.
POLEWARD OUTFLOW HAS CONTINUED TO WEAKEN OVER THE PAST 6 HOURS,
THOUGH THE CHANNEL IS STILL PRESENT. UNFORTUNATELY, THERE HAVE BEEN
NO SCATTEROMETER PASSES DIRECTLY OVER TROPICAL DEPRESSION (TD) 22W
FOR MORE THAN 18 HOURS, SO IT'S DIFFICULT TO CONFIRM THE LOW-LEVEL
WIND STRUCTURE OR CHARACTERIZE ITS EVOLUTION. THE INITIAL POSITION
IS PLACED WITH MEDIUM CONFIDENCE BASED ON THE ROTATION OBSERVED IN
ANIMATED MSI. THE INITIAL INTENSITY OF 30 KTS IS ASSESSED WITH LOW
CONFIDENCE, HEDGED SLIGHTLY BELOW THE CONSENSUS OF AGENCY DVORAK
FIXES AND OBJECTIVE INTENSITY ESTIMATES IN LIGHT OF THE SYSTEM'S
POOR ORGANIZATION AND DISTANCE FROM ENHANCED GRADIENT WINDS. THE
ENVIRONMENT IS CHARACTERIZED AS MARGINAL FOR FURTHER DEVELOPMENT
DUE TO LOW-MODERATE VERTICAL WIND SHEAR (VWS), WEAKENING OUTFLOW
ALOFT, AND CONTINUED DRY AIR ENTRAINMENT, DESPITE WARM SEA SURFACE
TEMPERATURES.
INITIAL WIND RADII BASIS: NOT APPLICABLE (THERE ARE NO INITIAL WIND
RADII).
CURRENT STEERING MECHANISM: THE NORTHERN PERIPHERY OF A NEAR
EQUATORIAL RIDGE (NER) POSITIONED TO THE SOUTH.
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.5 - 35 KTS
RJTD: T2.0 - 30 KTS
RCTP: T2.5 - 35 KTS
CIMSS ADT: 35 KTS AT 052340Z
CIMSS AIDT: 36 KTS AT 052340Z
CIMSS D-PRINT: 28 KTS AT 060020Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL
VWS: 15-20 KTS
SST: 29-30 CELSIUS
OUTFLOW: MODERATE POLEWARD
OTHER FACTORS: DRY AIR ENTRAINMENT FROM THE WEST
ANALYSIS CONFIDENCE:
INITIAL POSITION: MEDIUM
INITIAL INTENSITY: LOW
INITIAL WIND RADII: NOT APPLICABLE
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THE FORECAST TRACK AS A WHOLE HAS
SHIFTED WESTWARD AS A RESULT OF THE 060000Z ANALYZED POSITION,
FOLLOWING THE REORGANIZATION OF THE LLCC.
FORECAST DISCUSSION: TROPICAL DEPRESSION (TD) 22W HAS GONE THROUGH
A REORGANIZATION PHASE OVER THE PAST 6 HOURS AND REEMERGED JUST
NORTHWEST OF MINAMI DAITOJIMA. THE TRACK IS FORECAST TO RESUME IN
AN EAST-NORTHEASTWARD DIRECTION FOR THE NEXT 24 HOURS UNDER THE
STEERING INFLUENCE OF THE NER TO THE SOUTH. AFTER TAU 24, A
POLEWARD TURN IS EXPECTED AS THE SYSTEM TRACKS ALONG THE WESTERN
PERIPHERY OF A SUBTROPICAL RIDGE (STR) POSITIONED SOUTHEAST OF
JAPAN. A NORTHEASTWARD TURN IS EXPECTED TO BEGIN AROUND TAU 60 AS
22W APPROACHES THE RIDGE AXIS. PERSISTENT LOW-MODERATE VWS AND
CONTINUED DRY AIR ENTRAINMENT ARE EXPECTED TO PREVENT ANY FURTHER
INTENSIFICATION OF 22W, INSTEAD RESULTING IN A GRADUAL WEAKENING
TREND AS IT APPROACHES SOUTHERN HONSHU. THE CIRCULATION WILL LIKELY
BECOME EXTREMELY STRETCHED AS IT INTERACTS WITH THE HOSTILE
UPPER-LEVEL WINDS AFTER TAU 60, RESULTING IN DISSIPATION BY TAU 96.
IT IS POSSIBLE THAT THE LLCC IS UNABLE TO REMAIN INTACT UNDER
UNFAVORABLE ENVIRONMENTAL CONDITIONS, IN WHICH CASE DISSIPATION
WOULD OCCUR SOONER.
MODEL DISCUSSION: MODEL TRACK GUIDANCE IS IN MODERATE AGREEMENT
THROUGH TAU 48 WITH A CROSS-TRACK SP…
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: SE (130°), 3.9 kt | Gust: 5.8 kt
Pressure: 29.92 | Air Temp: 85.6 °F
Water Temp: 88.2 °F | Dew Point: 79.9 °F
Swell: | Wind Wave:
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.