🚨 North Walton; Central Walton; Holmes; Washington; Jackson; Inland Bay; Calhoun; Inland Gulf; South Walton; Coastal Bay; Coastal Gulf; Coastal Franklin: Wind Advisory issued October 17 at 1:27PM EDT until October 17 at 8:00PM EDT by NWS Tallahassee FL     🚨 Carroll; Warren; Tippecanoe; Fountain; Vermillion; Parke; Putnam; Marion; Vigo; Clay; Owen; Morgan; Johnson; Sullivan; Greene; Monroe; Brown; Bartholomew; Knox; Daviess; Martin; Lawrence; Jackson; Jennings: Frost Advisory issued October 17 at 1:26PM EDT until October 18 at 9:00AM EDT by NWS Indianapolis IN     🚨 Clinton; Howard; Montgomery; Boone; Tipton; Hamilton; Madison; Delaware; Randolph; Hendricks; Hancock; Henry; Shelby; Rush; Decatur: Freeze Warning issued October 17 at 1:26PM EDT until October 18 at 9:00AM EDT by NWS Indianapolis IN     🚨 Upper Hood River Valley: Frost Advisory issued October 17 at 10:25AM PDT until October 18 at 9:00AM PDT by NWS Portland OR     🚨 Guam, GU: Flash Flood Warning issued October 18 at 3:23AM ChST until October 18 at 5:30AM ChST by NWS Tiyan GU     🚨 Lake; Ashtabula Lakeshore; Northern Erie: Frost Advisory issued October 17 at 1:21PM EDT until October 18 at 9:00AM EDT by NWS Cleveland OH     🚨 Lucas; Wood; Ottawa; Sandusky; Erie; Lorain; Cuyahoga; Geauga; Ashtabula Inland; Hancock; Seneca; Huron; Medina; Summit; Portage; Trumbull; Wyandot; Crawford; Richland; Ashland; Wayne; Stark; Mahoning; Marion; Morrow; Holmes; Knox; Southern Erie; Crawford: Freeze Warning issued October 17 at 1:21PM EDT until October 18 at 9:00AM EDT by NWS Cleveland OH     🚨 Coastal waters east of Ipswich Bay and the Stellwagen Bank National Marine Sanctuary: Small Craft Advisory issued October 17 at 1:17PM EDT until October 18 at 8:00AM EDT by NWS Boston/Norton MA     🚨 Nantucket Sound; Vineyard Sound; Buzzards Bay; Rhode Island Sound; Block Island Sound: Small Craft Advisory issued October 17 at 1:17PM EDT until October 18 at 8:00AM EDT by NWS Boston/Norton MA     🚨 Boston Harbor; Narragansett Bay: Small Craft Advisory issued October 17 at 1:17PM EDT until October 17 at 8:00PM EDT by NWS Boston/Norton MA    

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: 17 UTC 17 Oct 2026

Active storms summary

Select a Storm

TRUDY (EP212026)

Type: HU Max Wind: 80 kt Min Pressure: 979 hPa Position: 16.3, -103.7 Basin: East Pacific
ZCZC MIATCDEP1 ALL TTAA00 KNHC DDHHMM Hurricane Trudy Discussion Number 17 NWS National Hurricane Center Miami FL EP212026 900 AM CST Sat Oct 17 2026 Trudy is slowly becoming better organized. The hurricane is producing a large central dense overcast with cloud tops colder than -80C, and curved bands of overshooting tops in the CDO indicate an eyewall is present underneath it. The various satellite intensity estimates are starting to increase, but not enough yet to support raising the intensity. Thus, the initial intensity remains 80 kt. The hurricane is moving a little faster toward the northwest, 325/9 kt. A continued northwestward motion is expected during the next day or so as a weak low- to mid-level ridge builds over eastern Mexico. This general motion should continue for the next 36 h or so, bringing the center of Trudy very close to the coast of west-central Mexico. Thereafter, as Trudy weakens and becomes steered mainly by low-level flow, a turn toward the west and west-northwest is expected, taking the cyclone away from the coast. The new track forecast has only minor adjustments from the previous forecast, with the center making its closest approach to the coast of Mexico around 36-48 h. Now that Trudy is over water with a higher oceanic heat content, some strengthening is possible. However, moderate vertical shear, dry air entrainment, and increasing land interaction could limit how much strengthening may occur. After 24 h or so, increasing southwesterly shear and decreasing mid-level moisture near the cyclone are likely to cause steady to rapid weakening even when the center would be moving away from the coast of Mexico. Current expectations are that the system will stop producing convection between 72-96 h and decay to a remnant low pressure, and the global models forecast the circulation to weaken to a trough by 120 h. The new intensity forecast has some tweaks from the previous forecast, and it lies near the upper edge of the intensity guidance envelope. KEY MESSAGES: 1. Trudy could strengthen some during the next 12 hours or so as it approaches the coast of southwestern and west-central Mexico this weekend, bringing an increasing risk of storm surge, damaging winds, and flooding rain. Hurricane Warnings and Watches, as well as Tropical Storm Warnings and Watches, are currently in effect for portions of the coast, and additional watches and warnings may be required. 2. Heavy rainfall associated with Trudy will impact the southwest Mexican coast between Guerrero and Nayarit through the weekend. This rainfall may produce life-threatening flooding and mudslides this weekend along and near the southwest Mexican coast in Michoacán, Colima, and Jalisco, especially in areas along steep terrain. 3. Large swells are affecting portions of the coast of southwestern Mexico and will spread northward through the weekend, causing life-threatening surf and rip current conditions. FORECAST POSITIONS AND MAX WINDS INIT 17/1500Z 16.6N 103.9W 80 KT 90 MPH 12H 18/0000Z 17.7N 104.8W 90 KT 105 MPH 24H 18/1200Z 19.1N 105.7W 90 KT 105 MPH 36H 19/0000Z 20.1N 106.4W 85 KT 100 MPH 48H 19/1200Z 20.7N 107.0W 65 KT 75 MPH 60H 20/0000Z 20.9N 107.5W 45 KT 50 MPH 72H 20/1200Z 20.9N 108.2W 35 KT 40 MPH 96H 21/1200Z 21.7N 109.4W 25 KT 30 MPH...POST-TROP/REMNT LOW 120H 22/1200Z...DISSIPATED $$ Forecaster Beven NNNN

CHAMPI (WP292026)

Type: HU Max Wind: 120 kt Min Pressure: 945 hPa Position: 12.6, 146.1 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 171500 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TYPHOON 29W (CHAMPI) WARNING NR 013// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 12.6N 146.1E INITIAL INTENSITY: 120 KTS GEOGRAPHIC REFERENCE: 96 NM SOUTHEAST OF ANDERSEN AFB MOVEMENT PAST 6 HOURS: WESTWARD AT 12 KTS SIGNIFICANT WAVE HEIGHT: 42 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: THE OVERALL STRUCTURE OF TY 29W IN ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY HAS DETERIORATED OVER THE PAST SIX HOURS, AS THE THE PREVIOUSLY CLOUD-FREE, PINHOLE EYE HAS FILLED IN DUE TO AN ONGOING EYEWALL REPLACEMENT CYCLE (ERC). THE EYE REMAINS DETECTABLE IN EIR IMAGERY, AND APPEARS TO BE SLIGHTLY LARGER THAN SIX HOURS AGO. HOWEVER, THE EYE TEMPERATURES ARE VERY COLD (APPROXIMATELY -50C). ANIMATED RADAR IMAGERY FROM GUAM SHOWS THAT THE EYE TOOK A A TEMPORARY WEST-SOUTHWESTWARD TROCHOIDAL JOG OVER THE PAST SIX HOURS; HOWEVER, THE INTEGRATED MOTION VECTOR REMAINS STABLE AT 280 DEGREES AT 14 KNOTS BASED ON THE BEST TRACK. OVER THE PAST TWO HOURS, THE SYSTEM HAS RESUMED A WEST-NORTHWESTWARD HEADING AMID TROCHOIDAL OSCILLATION. RADAR DATA CLEARLY RESOLVES A CONCENTRIC EYEWALL MORPHOLOGY, HIGHLIGHTED BY A THICKENING INNER EYEWALL, A DISTINCT RADAR MOAT, AND A SECONDARY OUTER EYEWALL SITUATED APPROXIMATELY 30 NM DISTANT FROM THE GEOMETRIC CENTER-STRONG STRUCTURAL SIGNATURES CONFIRMING ERC PROGRESSION. THE INITIAL POSITION IS ASSESSED WITH HIGH CONFIDENCE BASED ON THE RADAR EYE FIXES. THE INITIAL INTENSITY IS ASSESSED WITH MEDIUM CONFIDENCE. ALTHOUGH THE EYE HAS FILLED WITHIN THE PAST TWO HOURS, THE SYSTEM LIKELY ATTAINED PEAK INTENSITY IMMEDIATELY PRIOR TO ERC INITIATION, WITH SURFACE WIND ENERGETICS TEMPORARILY LAGGING THE STRUCTURAL EVOLUTION. THIS IS REINFORCED BY CONCURRENT SUBJECTIVE AND OBJECTIVE SATELLITE ESTIMATES, WHICH CONVERGE AT 120 KNOTS. THE ENVIRONMENT REMAINS HIGHLY CONDUCIVE INDEPENDENT OF CORE-SCALE ERC DYNAMICS, SUPPORTED BY LOW DEEP-LAYER VWS, EXTREMELY WARM SSTS (29- 30C), AND VIGOROUS RADIAL OUTFLOW ALOFT. INITIAL WIND RADII BASIS: PERSISTENCE CURRENT STEERING MECHANISM: SOUTHERN PERIPHERY OF A DEEP-LAYER SUBTROPICAL RIDGE (STR) FAR TO THE NORTH. AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T6.5 - 127 KTS RJTD: T6.0 - 115 KTS CIMSS ADT: 112 KTS AT 171130Z CIMSS AIDT: 122 KTS AT 171130Z CIMSS D-MINT: 120 KTS AT 171033Z CIMSS D-PRINT: 122 KTS AT 171130Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: HIGHLY FAVORABLE VWS: 10-15 KTS SST: 29-30 CELSIUS OUTFLOW: STRONG RADIAL OTHER FACTORS: EQUATORWARD OUTFLOW CHANNEL; EYEWALL REPLACEMENT CYCLE (ERC). 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) 29W IS TRACKING WESTWARD IN THE AGGREGATE, ALTHOUGH ERRATIC TROCHOIDAL MOTION IS PROJECTED TO PERSIST PENDING COMPLETION OF THE ERC. THE EXACT FREQUENCY AND AMPLITUDE OF THIS MOTION, WHICH REMAIN HIGHLY UNCERTAIN, WILL GOVERN THE PRECISE CPA AND TRACK GEOMETRY WHEN PASSING GUAM. THE CYCLONE WILL TRANSIT THE SOUTHERN TIP OF GUAM WITHIN THE NEXT SIX TO EIGHT HOURS. THE CORE WILL THEN VEER PROGRESSIVELY NORTHWESTWARD AS THE STR TO THE NORTH SLIDES EASTWARD, REPLACED BY A SECONDARY HIGH-PRESSURE CELL TRANSLATING RAPIDLY WEST-TO-EAST TO THE NORTH. BY TAU 96, THE STR WILL POSITION SOUTHEAST OF HONSHU, DEVELOPING A BROAD WEAKNESS OVER THE EAST CHINA SEA. CONSEQUENTLY, TY 29W WILL DECELERATE SHARPLY WHILE MAINTAINING A GENERAL NORTHWESTWARD HEADING PAST TAU 96 AS THE STEERING GRADIENT RELAXES. REGARDING INTENSITY: THE ACTIVE ERC INTRODUCES COMPETING THERMODYNAMIC AND STRUCTURAL INFLUENCES. SP…

WATI (SH012027)

Type: TS Max Wind: 60 kt Min Pressure: 985 hPa Position: -14.4, -163.0 Basin: South 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.
WDPS31 PGTW 170900 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL CYCLONE 01P (WATI) WARNING NR 003// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 13.2S 163.2W INITIAL INTENSITY: 60 KTS GEOGRAPHIC REFERENCE: 442 NM EAST OF PAGO PAGO MOVEMENT PAST 6 HOURS: SOUTH-SOUTHEASTWARD AT 12 KTS SIGNIFICANT WAVE HEIGHT: 24 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS A COMPACT INNER CORE OF DEEP CONVECTION WITH SLIGHTLY ASYMMETRIC SPIRAL BANDING FEATURES WRAPPING CONCENTRICALLY INTO AN OBSCURED LOW-LEVEL CIRCULATION CENTER (LLCC). A 170441Z WSF-M COLOR-ENHANCED 37GHZ MICROWAVE PASS REVEALED A WELL-DEFINED MICROWAVE EYE SIGNATURE, CHARACTERIZED BY A CYAN RING ENCIRCLING THE EYE AND DEEP CONVECTIVE CORES ALONG THE WESTERN AND NORTHERN FLANKS OF THE INNER CORE. THE INITIAL POSITION IS ASSESSED WITH HIGH CONFIDENCE, DERIVED FROM A SHORT-RANGE EXTRAPOLATION OF THE MICROWAVE EYE SIGNATURE. THE INITIAL INTENSITY IS ASSESSED WITH MEDIUM CONFIDENCE, HEDGED SLIGHTLY HIGHER THAN SUBJECTIVE AGENCY DVORAK FIXES (35-55 KTS) IN DEFERENCE TO THE CIMSS D-PRINT ESTIMATE (60 KTS), WHICH IS DEEMED MORE REPRESENTATIVE OF THE CONSOLIDATED CORE. ENVIRONMENTAL CONDITIONS ARE FAVORABLE FOR CONTINUED DEVELOPMENT, CHARACTERIZED BY WEAK DEEP-LAYER VERTICAL WIND SHEAR (VWS), WARM SEA SURFACE TEMPERATURES (SSTS), AND ROBUST POLEWARD OUTFLOW ALOFT. INITIAL WIND RADII BASIS: PERSISTENCE CURRENT STEERING MECHANISM: SOUTHWESTERN PERIPHERY OF A DEEP-LAYER SUBTROPICAL RIDGE (STR) TO THE NORTHEAST. AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T3.5 - 55 KTS PHFO: T2.5 - 35 KTS NFFN: T3.5 - 55 KTS CIMSS SATCON: 54 KTS AT 170740Z CIMSS ADT: 45 KTS AT 170540Z CIMSS AIDT: 42 KTS AT 170540Z CIMSS D-MINT: 46 KTS AT 170443Z CIMSS D-PRINT: 60 KTS AT 170710Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE VWS: 0-5 KTS SST: 27-28 CELSIUS OUTFLOW: STRONG POLEWARD 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: TC 01P (WATI) EXHIBITED ERRATIC, LOOPING MOTION EARLIER IN THE DAY TODAY, BUT SINCE 00Z, HAS STEADIED UP ON A SOUTHEASTWARD TRAJECTORY BASED ON MULTIPLE MICROWAVE IMAGE PASSES. THE SYSTEM IS FORECAST TO ACCELERATE SOUTHEASTWARD ALONG THE SOUTHWESTERN FLANK OF THE STR THROUGHOUT THE ENTIRETY OF THE FORECAST PERIOD. REGARDING INTENSITY: TC 01P RESIDES WITHIN A CONDUCIVE ENVIRONMENT AND IS PROJECTED TO INTENSIFY STEADILY, REACHING A PEAK INTENSITY OF 75 KNOTS NEAR TAU 24. SHOULD INNER-CORE CONSOLIDATION ACCELERATE RAPIDLY, AN ONSET OF RAPID INTENSIFICATION (RI) REMAINS A POSSIBILITY, POTENTIALLY DRIVING PEAK SURFACE WINDS TOWARD 80-85 KNOTS. BY TAU 24, HOWEVER, DEEP-LAYER VWS IS PROJECTED TO INCREASE SHARPLY, INITIATING A WEAKENING TREND THAT WILL PERSIST THROUGH THE BALANCE OF THE FORECAST. TC 01P WILL PASS SOUTH OF THE 26C ISOTHERM WITHIN 36 HOURS, AND THIS WILL ACCELERATE THE DECAY RATE. BY TAU 60, THE CYCLONE WILL BEGIN TO INTERACT WITH A BAROCLINIC ZONE TO THE SOUTH, PHASING WITH THE POLAR JET STREAM TO INITIATE FRONTOGENESIS AND MARKING THE START OF EXTRATROPICAL TRANSITION (ETT). COMPLETED TRANSITION TO A COLD-CORE GALE IS FORECAST NLT TAU 72. MODEL DISCUSSION: TRACK GUIDANCE IS IN STRONG AGREEMENT ON THE OVERALL TRACK, WITH ALL CONSENSUS MEMBERS SUPPORTING A SOUTHEASTWARD TRACK THROUGH THE FORECAST PERIOD. CROSS-TRACK SPREAD GRADUALLY INCREASES TO 300 NM BY TAU 120. GALWEM DEFINES THE WESTERN (INNER) PERIPHERY OF THE GUIDANCE ENVELOPE, WHILE THE DETERMINISTIC GFS COVERS THE EASTERN BOUNDARY. THE AI MODELS, DETERMINISTIC ECMWF, …

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: NNE (30°), 23.3 kt   |   Gust: 27.2 kt

Pressure: 30.09 rising   |   Air Temp: 78.1 °F

Water Temp: 84.6 °F   |   Dew Point: 72.3 °F

Swell: 6.2 ft   |   Wind Wave: 7.9 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.