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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
Tropical Storm Douglas Discussion Number 6
NWS National Hurricane Center Miami FL EP042026
800 AM PDT Thu Jul 02 2026
Geostationary and microwave satellite imagery shows that while
Douglas continues to produce bursts of convection, the convection
is poorly organized and located mainly in a nearly linear band to
the north of the center. The various subjective and objective
satellite intensity estimates are in the 35-40 kt range, and given
the rather ragged appearance the initial intensity is held at 35
kt.
The initial motion is 355/5 kt. A northward motion should continue
for the next 12 h or so as the storm moves around the western
periphery of a mid-level ridge. After that, the guidance generally
agrees that Douglas should turn generally northwestward as the
weakening cyclone is steered more by the low-level flow. The new
forecast track is similar to the previous track and lies close to
the HCCA corrected consensus model.
Douglas is now passing over the 26C isotherm and is experiencing
10-15 kt of southwesterly vertical shear. The shear is expected to
increase as the cyclone moves over colder water, and dry air is
likely to entrain into the circulation. Based on this, the
intensity guidance agrees that Douglas should weaken during the
forecast period, becoming a depression sometime tonight, a remnant
low sometime on Friday, and dissipating by 96 h. The new intensity
forecast has only minor tweaks from the previous forecast.
FORECAST POSITIONS AND MAX WINDS
INIT 02/1500Z 17.4N 127.1W 35 KT 40 MPH
12H 03/0000Z 18.2N 127.3W 35 KT 40 MPH
24H 03/1200Z 19.5N 127.7W 30 KT 35 MPH
36H 04/0000Z 20.6N 128.3W 25 KT 30 MPH...POST-TROP/REMNT LOW
48H 04/1200Z 21.5N 129.1W 25 KT 30 MPH...POST-TROP/REMNT LOW
60H 05/0000Z 22.3N 130.1W 20 KT 25 MPH...POST-TROP/REMNT LOW
72H 05/1200Z 23.1N 131.1W 20 KT 25 MPH...POST-TROP/REMNT LOW
96H 06/1200Z...DISSIPATED
$$
Forecaster Beven
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 021500
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 09W (BAVI) WARNING NR
007//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 12.3N 158.0E
INITIAL INTENSITY: 55 KTS
GEOGRAPHIC REFERENCE: 770 NM EAST OF ANDERSEN AFB
MOVEMENT PAST 6 HOURS: WEST-NORTHWESTWARD AT 11 KTS
SIGNIFICANT WAVE HEIGHT: 26 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS PERSISTENT
CONVECTIVE BANDING WRAPPING INTO THE CONSOLIDATING CENTRAL CORE OF TS
09W. ALTHOUGH THE LOW-LEVEL CIRCULATION CENTER IS FULLY OBSCURED, THE
SLACKENING VERTICAL WIND SHEAR (VWS) OVER THE PAST 6 HOURS SUGGESTS
THAT THE VORTEX HAS BECOME BETTER ALIGNED VERTICALLY. ROBUST POLEWARD
AND EQUATORWARD OUTFLOW IS EVIDENT IN ANIMATED WATER VAPOR IMAGERY,
ALONG WITH IMPROVING RADIAL OUTFLOW OVER THE PAST FEW HOURS. A 020704Z
WSFM 37 GHZ MICROWAVE IMAGE REVEALED A NASCENT MICROWAVE EYE WITH
IMPROVED SYMMETRY OF THE CONVECTIVE BANDING SURROUNDING THE CENTRAL
CORE. THE INITIAL POSITION IS PLACED WITH MEDIUM CONFIDENCE BASED ON
THE CENTER OF ROTATION IN ANIMATED EIR AND EXTRAPOLATION FROM THE
EARLIER MICROWAVE IMAGERY. THE INITIAL INTENSITY OF 55 KTS IS ASSESSED
WITH MEDIUM CONFIDENCE BASED ON A BLEND OF THE AGENCY DVORAK FIXES AND
CIMSS OBJECTIVE INTENSITY ESTIMATES. THE ENVIRONMENT IS CHARACTERIZED
AS HIGHLY FAVORABLE WITH VERY WARM (29-30 C) SEA SURFACE TEMPERATURES,
HIGH OCEAN HEAT CONTENT, AND STRONG OUTFLOW ALOFT. THE ONLY LIMITING
ENVIRONMENTAL FACTOR IN THE SHORT TERM IS THE 10-15 KTS OF EASTERLY
VWS.
INITIAL WIND RADII BASIS: OBJECTIVE BEST TRACK
CURRENT STEERING MECHANISM: SOUTHWESTERN FLANK OF AN EXTENSION OF
THE SUBTROPICAL RIDGE (STR) SITUATED TO THE NORTHEAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T3.5 - 55 KTS
RJTD: T3.0 - 45 KTS
RCTP: T3.0 - 45 KTS
KNES: T3.5 - 55 KTS
CIMSS SATCON: 55 KTS AT 021030Z
CIMSS ADT: 59 KTS AT 021200Z
CIMSS AIDT: 49 KTS AT 021200Z
CIMSS D-MINT: 52 KTS AT 020840Z
CIMSS D-PRINT: 57 KTS AT 021200Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: HIGHLY FAVORABLE
VWS: 10-15 KTS
SST: 29-30 CELSIUS
OUTFLOW: STRONG POLEWARD AND 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) 09W (BAVI) HAS CONTINUED
ON A NORTHWESTWARD TRACK OVER THE PAST 6 HOURS UNDER THE STEERING
INFLUENCE OF AN EXTENSION OF THE STR POSITIONED TO THE NORTHEAST.
THE SYSTEM IS EXPECTED TO ASSUME A WESTWARD TRAJECTORY THROUGH TAU
48 AS A STR CENTERED NEAR KYUSHU BUILDS IN FROM THE WEST AND TAKES
OVER AS THE PRIMARY STEERING MECHANISM. THE TRACK SPEED IS EXPECTED
TO SLOW BETWEEN TAU 24 AND TAU 72 UNDER THIS STEERING INFLUENCE AS
A LONGWAVE TROUGH PROPAGATES EASTWARD TO THE NORTH, TEMPORARILY
WEAKENING THE STEERING GRADIENT. AFTER TAU 60, TS 09W RETURNS TO A
WEST-NORTHWESTWARD TRACK AS IT APPROACHES THE NORTHERN MARIANA
ISLANDS, WITH A CPA TO SAIPAN AROUND 052300Z. INTENSIFICATION OVER
THE NEXT 12 HOURS IS EXPECTED TO REMAIN STEADY AS THE SYSTEM
CONSOLIDATES AND MOVES INTO A LOWER SHEAR ENVIRONMENT. AFTER TAU 12,
ENVIRONMENTAL CONDITIONS FAVOR AN EXTENDED PERIOD OF RAPID
INTENSIFICATION (RI) THROUGH TAU 60. HAFS-A CONTINUES TO DEPICT AN
EYEWALL REPLACEMENT CYCLE (EWRC) STARTING BETWEEN TAU 48 AND 60,
CONTINUING THROUGH PASSAGE TROUGH THE NORTHERN MARIANAS. AS A RESULT,
THE INTENSITY IS FORECAST TO LEVEL OFF AT A PEAK OF 135 KTS FROM TAU
72 THROUGH THE REMAINDER OF THE FORECAST PERIOD.
MODEL DISCUSSION: WITH THE EXCEPTION OF THE UKMET ENSEMBLE MEAN AS
A SOUTHERN OUTLIER AND EC-AIFS AS THE NORTHERN OUTLIER, MO…
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 021500
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL DEPRESSION 10W (TEN) WARNING
NR 004//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 17.6N 111.0E
INITIAL INTENSITY: 30 KTS
GEOGRAPHIC REFERENCE: 182 NM EAST-NORTHEAST OF DA NANG, VIETNAM
MOVEMENT PAST 6 HOURS: WEST-SOUTHWESTWARD AT 06 KTS
SIGNIFICANT WAVE HEIGHT: 15 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS THE
PREVIOUSLY EXPOSED LOW-LEVEL CIRCULATION CENTER INCORPORATING WITH
FLARING CONVECTION IN THE SOUTHWEST QUADRANT AS THE SYSTEM APPEARS
TO BE REORGANIZING AROUND THE BROADER SURROUNDING CYCLONIC
CIRCULATION. LACKING ANY RECENT SCATTEROMETER DATA TO FURTHER
ILLUMINATE THE NATURE OF THE BROADER CIRCULATION, THE INITIAL
POSITION IS PLACED WITH LOW CONFIDENCE NEAR THE CENTER OF THE
LOW-LEVEL WIND FIELD EXPOSED IN THE ANIMATED EIR. WITH THE
REORGANIZATION UNDERWAY, THE INITIAL INTENSITY IS HELD AT 30 KTS
WITH MEDIUM CONFIDENCE, SUPPORTED BY THE AGENCY DVORAK FIXES AND
CIMSS OBJECTIVE INTENSITY ESTIMATES. THE ENVIRONMENT IS
CHARACTERIZED AS MARGINAL WITH WARM (29-30 C) SEA SURFACE
TEMPERATURES AND MODERATE EQUATORWARD OUTFLOW BEING OFFSET BY 15-20
KTS OF NORTHEASTERLY VERTICAL WIND SHEAR (VWS).
INITIAL WIND RADII BASIS: NOT APPLICABLE (THERE ARE NO INITIAL WIND
RADII).
CURRENT STEERING MECHANISM: SOUTHWESTERN PERIPHERY OF A DEEP-LAYER
SUBTROPICAL RIDGE (STR) CENTERED SOUTHEAST OF KYUSHU
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.0 - 30 KTS
RJTD: T1.5 - 25 KTS
KNES: T2.0 - 30 KTS
CIMSS ADT: 35 KTS AT 021140Z
CIMSS AIDT: 33 KTS AT 021140Z
CIMSS D-MINT: 28 KTS AT 021118Z
CIMSS D-PRINT: 25 KTS AT 021140Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL
VWS: 20-25 KTS
SST: 29-30 CELSIUS
OUTFLOW: MODERATE EQUATORWARD
ANALYSIS CONFIDENCE:
INITIAL POSITION: LOW
INITIAL INTENSITY: MEDIUM
INITIAL WIND RADII: NOT APPLICABLE
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO
THE FORECAST FROM THE PREVIOUS WARNING.
FORECAST DISCUSSION: TROPICAL DEPRESSION (TD) 10W HAS SLOWED ITS
TRACK SPEED OVER THE PAST 6 HOURS AS THE LOW-LEVEL CIRCULATION
REORGANIZES. THE TRACK IS EXPECTED TO RESUME A NORTHWESTWARD
TRAJECTORY TOWARD HAINAN ISLAND WITHIN THE NEXT 12 HOURS UNDER THE
STEERING INFLUENCE OF THE STR TO THE NORTHEAST. INITIAL LANDFALL
ALONG THE SOUTHEASTERN COAST OF HAINAN IS FORECAST SHORTLY BEFORE
TAU 18, THEN 10W IS EXPECTED TO REEMERGE OVER WATER IN THE GULF OF
TONKIN JUST BEFORE TAU 30, WITH A SECOND LANDFALL NEAR THE
SINO-VIETNAMESE BORDER REGION SHORTLY BEFORE TAU 48. THE DECAYING
REMNANTS WILL THEN TRACK INLAND OVER MAINLAND CHINA ON A
NORTH-NORTHEASTERLY TRACK FOR THE REMAINDER OF THE FORECAST PERIOD.
THERE IS EXPECTED TO BE A BRIEF WINDOW OF OPPORTUNITY FOR THE
SYSTEM TO INTENSIFY BEFORE TRACKING OVER HAINAN, THEN ANOTHER BRIEF
PERIOD OF INTENSIFICATION OVER THE GULF OF TONKIN, REACHING A PEAK
OF 40 KTS JUST BEFORE THE SECOND LANDFALL.
MODEL DISCUSSION: MODEL TRACK GUIDANCE IS IN OVERALL AGREEMENT
ABOUT THE EVENTUAL NORTHWESTWARD TRAJECTORY OVER HAINAN ISLAND AND
A SECOND LANDFALL NEAR THE SINO-VIETNAMESE BORDER REGION, WITH A
CROSS-TRACK SPREAD OF 95 NM AT TAU 48. THE GFS DETERMINISTIC AND
THE GFS ENSEMBLE MEAN COMPRISE THE EASTERNMOST SOLUTIONS WHILE THE
EXPERIMENTAL GOOGLE DEEPMIND IS THE WESTERNMOST SOLUTION. THE JTWC
TRACK FORECAST IS PLACED SLIGHTLY TO THE WEST OF THE MULTI-MODEL
CONSENSUS, HEDGED CLOSER TO THE GOOGLE DEEPMIND WITH MEDIUM
CONFIDENCE THROUGHOUT THE FORECAST PERIOD. MODEL INTENSITY GUIDANCE
DEPICTS A CONTINUOUS INTENSIFICATION UNTIL THE SECOND LANDFALL,
THEN RAPID WEAKENING OVER LAND. THE JTWC INTENSITY FORECAST IS
PLACED BELOW THE MULTI-MODEL CONSENSUS FOR THE PERIOD OF TIME THAT
T…
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: E (80°), 3.9 kt | Gust: 3.9 kt
Pressure: 30.05 rising | Air Temp: 85.3 °F
Water Temp: 85.5 °F | Dew Point: 78.3 °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.