🚨 Lake, IL; Kenosha, WI: Flood Warning issued October 3 at 6:28AM CDT until October 4 at 1:00PM CDT by NWS Milwaukee/Sullivan WI     🚨 Montgomery: None     🚨 Clinton, IA; Scott, IA: Flood Warning issued October 3 at 6:22AM CDT by NWS Quad Cities IA IL     🚨 Tinian Coastal Waters; Saipan Coastal Waters: Gale Warning issued October 3 at 9:13PM ChST until October 4 at 4:00PM ChST by NWS Tiyan GU     🚨 Guam Coastal Waters; Rota Coastal Waters: Hazardous Seas Warning issued October 3 at 9:13PM ChST until October 4 at 5:00AM ChST by NWS Tiyan GU     🚨 Orange County Inland: Extreme Heat Warning issued October 3 at 4:01AM PDT until October 8 at 8:00PM PDT by NWS San Diego CA     🚨 San Bernardino and Riverside County Valleys-The Inland Empire: Wind Advisory issued October 3 at 4:01AM PDT until October 3 at 6:00PM PDT by NWS San Diego CA     🚨 Santa Ana Mountains and Foothills: Extreme Heat Warning issued October 3 at 4:01AM PDT until October 8 at 8:00PM PDT by NWS San Diego CA     🚨 Riverside County Mountains; San Diego County Mountains; San Gorgonio Pass Near Banning: Wind Advisory issued October 3 at 4:01AM PDT until October 3 at 6:00PM PDT by NWS San Diego CA     🚨 San Bernardino and Riverside County Valleys-The Inland Empire: Extreme Heat Warning issued October 3 at 4:01AM PDT until October 8 at 8:00PM PDT by NWS San Diego CA    

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.

Summary & NHC 7-Day Formation Outlook

Valid: 11 UTC 03 Oct 2026

Active storms summary

Select a Storm

NOLO (EP152026)

Type: HU Max Wind: 90 kt Min Pressure: 967 hPa Position: 23.3, -169.0 Basin: East Pacific

RACHEL (EP182026)

Type: HU Max Wind: 85 kt Min Pressure: 968 hPa Position: 19.3, -111.6 Basin: East Pacific
ZCZC MIATCDEP3 ALL TTAA00 KNHC DDHHMM Hurricane Rachel Discussion Number 25 NWS National Hurricane Center Miami FL EP182026 200 AM MST Sat Oct 03 2026 Rachel has become less organized during the past several hours. The associated convection is now occurring only over the southern semicircle, and the latest microwave imagery indicates that there is no longer any eyewall. Satellite intensity estimates are in the 70-90 kt range and are trending downward. Based on the trend, the initial intensity is lowered to 80 kt. The initial motion is 275/4 kt. A mid-level anticyclone over the western United States has a ridge extending southwest to the west of Rachel, and this anticyclone is expected to build westward during the next 72 h. This evolution should steer the cyclone slowly west-northwestward for the next day or two, followed by a more westward motion. By 96-120 h, a west-northwestward motion is likely to resume as Rachel approaches the western end of the ridge. The new forecast track is close to the previous forecast for 48-60 h, and then is nudged a little south based on a southward shift in the guidance envelope. Additional slow weakening is forecast during the next 24-36 h as Rachel continues to experience northeasterly shear and crosses the cold water wake of Hurricane Polo. After that, the sea surface temperatures increase slightly at a time where the hurricane is likely to entrain dry air. These competing factors are expected to result in little net change in strength between 36-72 h. After 72 h, Rachel should move over progressively colder water and continue to entrain dry air, which should cause a steady weakening. FORECAST POSITIONS AND MAX WINDS INIT 03/0900Z 19.4N 111.8W 80 KT 90 MPH 12H 03/1800Z 19.6N 112.4W 80 KT 90 MPH 24H 04/0600Z 19.9N 113.2W 75 KT 85 MPH 36H 04/1800Z 20.1N 114.1W 70 KT 80 MPH 48H 05/0600Z 20.2N 115.2W 70 KT 80 MPH 60H 05/1800Z 20.4N 116.7W 70 KT 80 MPH 72H 06/0600Z 20.6N 118.4W 70 KT 80 MPH 96H 07/0600Z 21.2N 121.7W 65 KT 75 MPH 120H 08/0600Z 22.2N 125.0W 55 KT 65 MPH $$ Forecaster Beven NNNN

CHOI-WAN (WP262026)

Type: HU Max Wind: 80 kt Min Pressure: 969 hPa Position: 19.4, 145.9 Basin: West Pacific
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 TYPHOON 26W (CHOI-WAN) WARNING NR 014// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 19.4N 145.9E INITIAL INTENSITY: 80 KTS GEOGRAPHIC REFERENCE: 252 NM NORTH OF SAIPAN MOVEMENT PAST 6 HOURS: NORTH-NORTHEASTWARD AT 09 KTS SIGNIFICANT WAVE HEIGHT: 32 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS TYPHOON 26W (CHOI-WAN) WITH A CLOUD-FILLED EYE AND A MORE DISORGANIZED CONVECTIVE STRUCTURE COMPARED TO 6 HOURS AGO. THE MSI ALSO SHOWS SOME DRY AIR BEING PULLED INTO THE CORE OF 26W ALONG THE WESTERN PERIPHERY, WHICH COULD BE THE CAUSE FOR THE HALTED DEVELOPMENT. A 030228Z AMSR3 37 GHZ MICROWAVE IMAGE REVEALED AN ELLIPTIC MICROWAVE EYE FEATURE WITH A SLIGHT WEAKNESS IN THE WESTERN SEMICIRCLE. THE 89 GHZ VERSION OF THE SAME PASS SHOWED THE STRONGEST CONVECTION CONFINED TO THE SOUTHEASTERN QUADRANT OF THE SYSTEM. THE INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE ANIMATED MSI AND EXTRAPOLATION FROM THE AMSR3 MICROWAVE IMAGE SUITE. THE INITIAL INTENSITY OF 80 KTS IS ASSESSED WITH MEDIUM CONFIDENCE BASED ON A COMBINATION OF THE AGENCY DVORAK FIXES OF T5.0 AND THE LOWER CIMSS INTENSITY ESTIMATES. INITIAL WIND RADII BASIS: PERSISTENCE FROM THE 022345Z METOP-B ASCAT PASS WITH MINOR ADJUSTMENTS BASED ON THE OBJECTIVE BEST TRACK CURRENT STEERING MECHANISM: THE WESTERN EXTENSION OF A SUBTROPICAL RIDGE (STR) POSITIONED TO THE NORTHEAST AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T5.0 - 90 KTS RJTD: T5.0 - 90 KTS RCTP: T5.0 - 90 KTS CIMSS SATCON: 77 KTS AT 030600Z CIMSS ADT: 59 KTS AT 030600Z CIMSS AIDT: 63 KTS AT 030600Z CIMSS D-PRINT: 76 KTS AT 030600Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE VWS: 5-10 KTS SST: 29-30 CELSIUS OUTFLOW: STRONG POLEWARD AND EQUATORWARD OTHER FACTORS: SLIGHT DRY AIR ENTRAINMENT ALONG THE WESTERN PERIPHERY ANALYSIS CONFIDENCE: INITIAL POSITION: HIGH INITIAL INTENSITY: MEDIUM INITIAL WIND RADII: MEDIUM 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. FORECAST DISCUSSION: THE STEERING MECHANISM FOR 26W HAS SHIFTED FROM THE NEAR EQUATORIAL RIDGE TO THE SUBTROPICAL RIDGE TO THE NORTHEAST. THIS HAS CAUSED THE TRAJECTORY TO BECOME SLIGHTLY MORE NORTHWARD OVER PAST 6 HOURS. 26W IS FORECAST TO TURN FURTHER NORTHWARD AS IT TRACKS ALONG THE WESTERN PERIPHERY OF THE STR THROUGH TAU 72. AFTER TAU 72, THE SYSTEM WILL ACCELERATE NORTHEASTWARD AS IT ROUNDS THE RIDGE AXIS AND BEGINS TO INTERACT WITH THE STRONG UPPER-LEVEL FLOW. EXTRATROPICAL TRANSITION IS EXPECTED TO BE COMPLETE AROUND TAU 96, SOUTH OF THE KAMCHATKA PENINSULA, ONCE THE SYSTEM BECOMES EMBEDDED UNDERNEATH THE JET. IN TERMS OF INTENSITY, 26W IS FORECAST TO INTENSIFY OVER THE NEXT 24 HOURS TO A PEAK INTENSITY OF AROUND 105 KTS AS THE ENVIRONMENT REMAINS FAVORABLE WITH LOW SHEAR, VERY WARM SST, AND ROBUST OUTFLOW. THE PRIMARY LIMITING FACTOR WILL BE THE DRY AIR TO THE WEST. AROUND TAU 36, OCEAN HEAT CONTENT WILL START TO DROP AND EQUATORWARD OUTFLOW WILL BECOME RESTRICTED, CAUSING 26W TO WEAKEN THROUGH TAU 72. FOLLOWING TAU 72, THE SYSTEM WILL TAP INTO AN EXTREME POLEWARD OUTFLOW CHANNEL, SUPPORTED BY A VERY STRONG JET MAX TO THE NORTH. THIS WILL OFFSET THE COOL SST AND HIGH SOUTHWESTERLY VERTICAL WIND SHEAR, ALLOWING FOR 26W TO LIKELY MAINTAIN TYPHOON INTENSITY THROUGH THE INITIAL STAGES OF FRONTOGENESIS. MODEL DISCUSSION: MODEL TRACK GUIDANCE IS IN MODERATE AGREEMENT THROUGH TAU 72 WITH MOST OF THE UNCERTAINTY REVOLVING AROUND THE SPEED OF ADVANCE AROUND THE RIDGE. WHILE CROSS-TRACK SPREAD IS ONLY AROUND 100 NM AT TAU 72, ALONG-TRACK SPREAD IS ABOUT 250 NM. GFS AND NAVGEM ARE THE SLOWEST TRA…

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.

Streamline Wind Map

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.

TC Drift Path Map

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°), 15.5 kt   |   Gust: 19.4 kt

Pressure: 29.85   |   Air Temp: 83.5 °F

Water Temp: 85.8 °F   |   Dew Point: 80.2 °F

Swell: 3.6 ft   |   Wind Wave: 2.6 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.

US National Radar Loop

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.

Satellite

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.

GOES IR Band 13

Most recent GOES Band 13 image. Provided by NOAA/NESDIS/STAR.