🚨 Chuuk Coastal Waters: Special Weather Statement issued July 3 at 9:27PM ChST by NWS Tiyan GU 🚨 Koror Palau Coastal Waters; Yap Coastal Waters: Special Weather Statement issued July 3 at 9:27PM ChST by NWS Tiyan GU 🚨 Marion; Lamar; Fayette; Winston; Walker; Blount; Etowah; Calhoun; Cherokee; Pickens; Tuscaloosa; Jefferson; Shelby; St. Clair; Talladega; Sumter; Greene; Hale; Perry; Bibb; Chilton; Coosa; Tallapoosa; Marengo; Dallas; Autauga; Lowndes; Elmore; Montgomery: Heat Advisory issued July 3 at 6:26AM CDT until July 4 at 9:00PM CDT by NWS Birmingham AL 🚨 Cleburne; Clay; Randolph; Chambers; Macon; Bullock; Lee; Russell; Pike; Barbour: Heat Advisory issued July 3 at 6:26AM CDT until July 4 at 9:00PM CDT by NWS Birmingham AL 🚨 Montgomery: None 🚨 Dawson; Gosper; Phelps; Furnas; Harlan: Special Weather Statement issued July 3 at 6:21AM CDT by NWS Hastings NE 🚨 Muskogee, OK: Flood Advisory issued July 3 at 6:21AM CDT until July 6 at 7:00PM CDT by NWS Tulsa OK 🚨 Lauderdale; Colbert; Franklin; Lawrence; Limestone; Madison; Morgan; Marshall; Jackson; DeKalb; Cullman; Moore; Lincoln; Franklin: Heat Advisory issued July 3 at 6:17AM CDT until July 4 at 7:00PM CDT by NWS Huntsville AL 🚨 Decatur; Norton; Red Willow: Special Weather Statement issued July 3 at 6:16AM CDT by NWS Goodland KS 🚨 Polk; Jasper; Marion: Flood Watch issued July 3 at 6:16AM CDT until July 4 at 1:47PM CDT by NWS Des Moines IA
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 MIATCDEP4 ALL
TTAA00 KNHC DDHHMM
Post-Tropical Cyclone Douglas Discussion Number 9
NWS National Hurricane Center Miami FL EP042026
200 AM PDT Fri Jul 03 2026
Douglas is no longer a tropical cyclone. The system has not produced
organized deep convection in the last 12 hours, and its low-level
center is completely exposed in proxy-visible satellite images due
to increasing westerly shear. Recent ASCAT data showed the system is
still producing tropical-storm-force winds in its northern
semicircle, and the extent of those winds was slightly larger than
previously estimated. Since Douglas is now a post-tropical low, this
will be the final NHC advisory. The initial intensity is 35 kt based
on the scatterometer winds and more recent satellite estimates.
The scatterometer data also indicated the center of Douglas is
slightly left of our previous estimates. The system is moving toward
the north-northwest (335/7 kt), but a northwestward turn is expected
during the next day or two as the low becomes steered by the
low-level flow. Based mainly on the initial position adjustment, the
NHC forecast track has been moved to the left, which brings it
closer to the multi-model consensus. Redevelopment is not expected
due to strengthening westerly shear, increasing mid-level dry air,
and decreasing sea-surface temperatures along the forecast track.
Thus, the low is predicted to gradually weaken this weekend and then
open into a trough and dissipate by Sunday.
For additional information on this system please see High Seas
Forecasts issued by the National Weather Service, under AWIPS header
NFDHSFEPI, WMO header FZPN02 KWBC, and on the web at
ocean.weather.gov/shtml/NFDHSFEPI.php
FORECAST POSITIONS AND MAX WINDS
INIT 03/0900Z 19.4N 128.3W 35 KT 40 MPH...POST-TROPICAL
12H 03/1800Z 20.2N 128.7W 30 KT 35 MPH...POST-TROP/REMNT LOW
24H 04/0600Z 21.1N 129.4W 30 KT 35 MPH...POST-TROP/REMNT LOW
36H 04/1800Z 22.0N 130.3W 25 KT 30 MPH...POST-TROP/REMNT LOW
48H 05/0600Z 22.9N 131.4W 25 KT 30 MPH...POST-TROP/REMNT LOW
60H 05/1800Z...DISSIPATED
$$
Forecaster Reinhart
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 030900
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TYPHOON 09W (BAVI) WARNING NR 010//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 12.9N 154.2E
INITIAL INTENSITY: 105 KTS
GEOGRAPHIC REFERENCE: 545 NM EAST OF ANDERSEN AFB
MOVEMENT PAST 6 HOURS: WESTWARD AT 11 KTS
SIGNIFICANT WAVE HEIGHT: 39 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
TY 09W HAS CONTINUED TO RAPIDLY INTENSIFY, INCREASING FROM 85 KTS
TO 105 KTS OVER THE PAST 6 HOURS. ANIMATED MULTISPECTRAL IMAGERY
(MSI) DEPICTS CONTINUALLY IMPROVING SYMMETRY, WITH A WELL-DEFINED
EYEWALL IN THE VISIBLE CHANNEL. THE DVORAK-ENHANCED INFRARED CHANNEL
SHOWS A SYMMETRIC CENTRAL DENSE OVERCAST COMPLETELY SURROUNDING THE
EYE AND WARMING TEMPERATURES WITHIN THE EYE. ANIMATED WATER VAPOR
IMAGERY REVEALS ROBUST RADIAL OUTFLOW, UNINHIBITED IN THE CURRENT LOW
SHEAR ENVIRONMENT. THE INITIAL POSITION IS ASSESSED WITH HIGH
CONFIDENCE BASED ON THE WELL-DEFINED EYE FEATURE IN MSI. THE INITIAL
INTENSITY IS ASSESSED WITH MEDIUM CONFIDENCE BASED ON THE SPREAD OF
AGENCY DVORAK FIXES AND CIMSS OBJECTIVE INTENSITY AIDS. THE
ENVIRONMENT IS CHARACTERIZED AS HIGHLY FAVORABLE FOR CONTINUED RAPID
INTENSIFICATION, WITH LOW (5-10 KTS) DEEP-LAYER VERTICAL WIND SHEAR
(VWS), VERY WARM (29-30C) SEA SURFACE TEMPERATURES, HIGH OCEAN HEAT
CONTENT (OHC) EXCEEDING 110 KJ PER CM3, AND STRONG RADIAL OUTFLOW
ALOFT.
INITIAL WIND RADII BASIS: OBJECTIVE BEST TRACK
CURRENT STEERING MECHANISM: SOUTHERN PERIPHERY OF A DEEP-LAYER
SUBTROPICAL RIDGE (STR) EXTENDING FROM SOUTH OF KYUSHU EASTWARD
INTO THE NORTHERN PACIFIC
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T5.5 - 102 KTS
RJTD: T5.0 - 90 KTS
RCTP: T6.0 - 115 KTS
KNES: T6.5 - 127 KTS
CIMSS SATCON: 98 KTS AT 030530Z
CIMSS ADT: 102 KTS AT 030600Z
CIMSS AIDT: 105 KTS AT 030600Z
CIMSS D-MINT: 97 KTS AT 030329Z
CIMSS D-PRINT: 109 KTS AT 030600Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: HIGHLY FAVORABLE
VWS: 5-10 KTS
SST: 29-30 CELSIUS
OUTFLOW: STRONG RADIAL
ANALYSIS CONFIDENCE:
INITIAL POSITION: HIGH
INITIAL INTENSITY: MEDIUM
INITIAL WIND RADII: LOW
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO
THE FORECAST FROM THE PREVIOUS WARNING.
FORECAST DISCUSSION: TYPHOON (TY) 09W (BAVI) HAS CONTINUED ON A
NEARLY WESTWARD TRACK UNDER THE STEERING INFLUENCE OF AN EXTENSION
OF THE STR CENTERED TO THE NORTHWEST. A BRIEF PERIOD OF WEAKENING
IN THE STEERING RIDGE AS A LONGWAVE TROUGH TRANSITS EASTWARD WELL
TO THE NORTH OF TY 09W IS EXPECTED TO SLOW THE SYSTEM'S SPEED OF
ADVANCE OVER THE NEXT 36 HOURS. THE CPA TO SAIPAN AND ROTA REMAINS
LITTLE CHANGED FROM THE PREVIOUS FORECAST, EXPECTED AROUND 052200Z.
THE ORIENTATION OF THE STR CURRENTLY ANCHORED SOUTH OF KYUSHU AND
ITS SLOW WESTWARD MIGRATION OVER THE NEXT 120 HOURS WILL RESULT IN
A PRIMARILY WESTWARD COMPONENT TO THE TRACK THROUGH TAU 36. AFTER
TAU 36 THE TRACK TURNS WEST-NORTHWESTWARD THROUGH THE REMAINDER OF
THE FORECAST PERIOD. RAPID INTENSIFICATION IF FORECAST TO CONTINUE
THROUGH TAU 36 TO A PEAK OF 150 KTS. AFTER TAU 36, VWS IS EXPECTED
TO STEADILY INCREASE TO 20 KTS AT TAU 60 AND 30-35 KNOTS BY TAU
120, STIFLING FURTHER INTENSIFICATION. THE PROBABILITY OF AN EYEWALL
REPLACEMENT CYCLE (ERC) REMAINS HIGH, AS SUGGESTED BY HAFS-A, WHICH
INTRODUCES SOME UNCERTAINTY IN THE TIMING AND MAGNITUDE OF THE PEAK
INTENSITY. IN THE EVENT OF AN ERC, THE WIND FIELD IS EXPECTED TO
EXPAND AND FURTHER LIMIT INTENSIFICATION.
MODEL DISCUSSION: MODEL TRACK GUIDANCE REMAINS IN A TIGHT ENVELOPE
THROUGH TAU 72, WITH THE EXCEPTION OF NAVGEM WHICH SUGGESTS A TRACK
SOUTH OF ROTA. THE REMAINDER OF GUIDANCE HAS A CROSS-TRACK SPREAD
OF 60 NM AT TAU 72 AND 75 NM AT TAU 120. TRACK SPEED IS SLIGHTLY
LESS CERTAIN IN THE LATER TAUS WITH A…
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 030900
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 10W (MAYSAK) WARNING NR
007//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 17.6N 109.7E
INITIAL INTENSITY: 35 KTS
GEOGRAPHIC REFERENCE: 125 NM NORTHEAST OF DA NANG, VIETNAM
MOVEMENT PAST 6 HOURS: NORTHWESTWARD AT 05 KTS
SIGNIFICANT WAVE HEIGHT: 15 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS A SLOWLY
RECONSOLIDATING SYSTEM WITH VIGOROUS CONVECTION LIMITED TO THE
SOUTHERN SEMICIRCLE. PERSISTENT NORTHEASTERLY SHEAR HAS PREVENTED
THE CONVECTION FROM WRAPPING AROUND THE CENTRAL CORE OVER THE PAST
6 HOURS. ANIMATED RADAR IMAGERY SHOWS TS 10W SLOWLY APPROACHING THE
SOUTHERN COAST OF HAINAN ISLAND WITH PRECIPITATION LIMITED TO THE
AREA BENEATH THE DEEP CONVECTION. THE INITIAL POSITION IS PLACED WITH
MEDIUM CONFIDENCE PRIMARILY BASED ON THE CENTER OF ROTATION IN THE
ANIMATED RADAR IMAGERY. THE INITIAL INTENSITY OF 35 KTS IS ASSESSED
WITH MEDIUM CONFIDENCE BASED PRIMARILY ON THE AGENCY DVORAK FIXES OF
T2.0-T2.5, SUPPLEMENTED BY THE CIMSS OBJECTIVE INTENSITY AIDS.
ENVIRONMENTAL CONDITIONS ARE MARGINAL, WITH WARM SSTS, LOW OHC,
MODERATE NORTHEASTERLY SHEAR AND MODERATE EQUATORWARD OUTFLOW.
INITIAL WIND RADII BASIS: PERSISTENCE
CURRENT STEERING MECHANISM: SOUTHWESTERN PERIPHERY OF A DEEP-LAYER
SUBTROPICAL RIDGE (STR) CENTERED SOUTH OF KYUSHU
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.5 - 35 KTS
RJTD: T2.5 - 35 KTS
RCTP: T2.0 - 30 KTS
KNES: T2.5 - 35 KTS
CIMSS ADT: 49 KTS AT 030600Z
CIMSS AIDT: 43 KTS AT 030600Z
CIMSS D-MINT: 35 KTS AT 030559Z
CIMSS D-PRINT: 39 KTS AT 030600Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL
VWS: 15-20 KTS
SST: 29-30 CELSIUS
OUTFLOW: MODERATE EQUATORWARD
ANALYSIS CONFIDENCE:
INITIAL POSITION: MEDIUM
INITIAL INTENSITY: MEDIUM
INITIAL WIND RADII: LOW
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO
THE FORECAST FROM THE PREVIOUS WARNING.
FORECAST DISCUSSION: TROPICAL STORM (TS) 10W (MAYSAK) HAS CONTINUED
TO SLOWLY DRIFT TOWARD THE SOUTHERN COAST OF HAINAN ISLAND OVER THE
PAST 6 HOURS AS IT WORKS TO RECONSOLIDATE. A SOUTHWESTERN EXTENSION
OF THE PRIMARY STEERING RIDGE CENTERED TO THE NORTHEAST IS EXPECTED
TO WEAKEN IMMINENTLY AND OVER THE NEXT 12 HOURS AND INITIATE A
NORTHWESTWARD TRAJECTORY OVER HAINAN. SHORTLY AFTER TAU 12, 10W WILL
REEMERGE OVER THE GULF OF TONKIN ON ITS WAY TO A SECOND LANDFALL NEAR
THE SINO-VIETNAMESE BORDER REGION AROUND TAU 36. AFTER LANDFALL, THE
TRACK TURNS NORTHEASTWARD AROUND THE RIDGE AXIS AS THE SYSTEM
DISSIPATES OVER LAND. THE INTENSITY IS FORECAST TO REMAIN STEADY AS
10W CLIPS THE SOUTHWESTERN EDGE OF HAINAN, THEN BRIEFLY INCREASE TO
40 KTS AS IT TRANSITS OVER THE GULF OF TONKIN.
MODEL DISCUSSION: MODEL TRACK GUIDANCE HAS COME INTO MUCH BETTER
AGREEMENT WITH THE LATEST MODEL RUN, WITH THE EXCEPTION OF NAVGEM AS
AN EASTERN OUTLIER. THE REMAINDER OF GUIDANCE HAS A CROSS-TRACK
SPREAD OF 45 NM AT TAU 36 WHEN THE SECOND LANDFALL IS EXPECTED TO
OCCUR. THE JTWC TRACK IS PLACED CLOSE TO THE MULTI-MODEL CONSENSUS
WITH MEDIUM CONFIDENCE THROUGHOUT THE FORECAST PERIOD. INTENSITY
GUIDANCE IS IN GOOD AGREEMENT ABOUT THE PERIOD OF INTENSIFICATION
OVER THE GULF OF TONKIN, REMAINING WITHIN A 10 KT ENVELOPE UNTIL
RAPID DISSIPATION OCCURS OVER THE MAINLAND. THE JTWC INTENSITY
FORECAST IS PLACED CLOSE TO THE CONSENSUS WITH MEDIUM CONFIDENCE.
FORECAST CONFIDENCE:
TRACK 00-72 HR: MEDIUM
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: S (180°), 1.9 kt | Gust: 3.9 kt
Pressure: 30.03 | Air Temp: 84.4 °F
Water Temp: 85.8 °F | Dew Point: 77.9 °F
Swell: 1.0 ft | Wind Wave: 0.3 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.