🚨 Coastal waters from Sandy Hook to Manasquan Inlet NJ out 20 NM; Coastal waters from Manasquan Inlet to Little Egg Inlet NJ out 20 NM: Small Craft Advisory issued October 29 at 1:27PM EDT until October 31 at 2:00AM EDT by NWS Mount Holly NJ     🚨 Lower St. Bernard; Southeast St. Tammany; Eastern Orleans; Lower Plaquemines: Coastal Flood Advisory issued October 29 at 12:25PM CDT until October 30 at 7:00AM CDT by NWS New Orleans LA     🚨 Southern Hancock: Coastal Flood Advisory issued October 29 at 12:25PM CDT until October 30 at 7:00AM CDT by NWS New Orleans LA     🚨 Montgomery: None     🚨 Coastal Collier County; Mainland Monroe; Far South Miami-Dade County: Coastal Flood Statement issued October 29 at 1:18PM EDT until October 30 at 8:00AM EDT by NWS Miami FL     🚨 Coastal Palm Beach County: Coastal Flood Advisory issued October 29 at 1:18PM EDT until October 30 at 8:00PM EDT by NWS Miami FL     🚨 Coastal Palm Beach County: Rip Current Statement issued October 29 at 1:18PM EDT until October 30 at 8:00PM EDT by NWS Miami FL     🚨 Coastal Broward County; Coastal Miami Dade County: Coastal Flood Advisory issued October 29 at 1:18PM EDT until October 30 at 8:00PM EDT by NWS Miami FL     🚨 Tinian; Saipan: High Surf Warning issued October 30 at 3:16AM ChST until October 30 at 4:00PM ChST by NWS Tiyan GU     🚨 Tinian; Saipan: Coastal Flood Statement issued October 30 at 3:16AM ChST until October 30 at 4:00PM ChST by NWS Tiyan GU    

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 29 Oct 2026

Active storms summary

Select a Storm

VANCE (EP222026)

Type: TS Max Wind: 35 kt Min Pressure: 1004 hPa Position: 21.4, -108.7 Basin: East Pacific
ZCZC MIATCDEP2 ALL TTAA00 KNHC DDHHMM Tropical Storm Vance Discussion Number 33 NWS National Hurricane Center Miami FL EP222026 800 AM MST Thu Oct 29 2026 Deep convection near the center yesterday evening produced tropical-storm-force winds in Vance's northern and eastern semicircles. Strong (50 kt) west-southwesterly vertical wind shear has been pushing the deep convection farther and farther away from the center over the past 9 to 12 hours, and now the convection is located more than 90 n mi east and northeast of the center. Recent surface observations from Islas Marias are 20 kt gusting to 30 kt while located underneath some of the deepest convection for the past few hours, so the winds are likely decreasing, but it is still possible that a small area of winds to tropical-storm-force exists in that convection, so Vance will be held at 35 kt for this advisory. Scatterometer passes expected within the next couple of hours should give us a better assessment of Vance's strength. The UW-CIMSS shear analysis and the latest SHIPS guidance are both analyzing about 50 kt of west-southwesterly vertical wind shear currently impacting Vance. The shear is forecast to increase to around 55 kt over the next 6 h or so. Vance is also located within a drier environment than it was yesterday, with mid-level relative humidity values in the 40 to 50 percent range. Therefore, deep convection, which is currently located well east of the center and moving farther away, is unlikely to return, and the GFS and ECMWF simulated satellite products do not forecast any new convection to form near the center. Therefore, the timing of post-tropical transition has been moved up to hour 12 in the official forecast. Most of the models then show the remnant low dissipating in about 18 to 24 hours over the southern Gulf of California. Although gradual weakening is forecast until dissipation, gusts to tropical-storm-force are still likely today within the deep convection well east of the center. Vance has been moving northward, or 350/7 kt. A generally northward motion at about the same speed is expected until Vance degenerates into a trough of low pressure over the southern Gulf of California in about 18 to 24 hours. The new NHC forecast is nudged a bit to the left of the previous one and is near the latest HCCA and GDMI. It should be emphasized that the main threat with Vance is the very heavy rainfall and high rain rates near the areas of very deep convection near the Islas Marias and west-central Mexico. Key Messages: 1. Periods of heavy rainfall associated with Vance will impact portions of western Mexico during the next day or two. This rainfall may produce flooding and mudslides across central and southern Sinaloa, far southwestern Durango, and far northwestern Nayarit, especially in areas along steep terrain. 2. Moisture carried northeastward from Vance will produce heavy rain across portions of the U.S. Southern Plains and New Mexico today into Friday. FORECAST POSITIONS AND MAX WINDS INIT 29/1500Z 21.6N 108.8W 35 KT 40 MPH 12H 30/0000Z 22.9N 108.5W 25 KT 30 MPH...POST-TROP/REMNT LOW 24H 30/1200Z...DISSIPATED $$ Forecaster Hagen NNNN

ARNAB (IO022026)

Type: TD Max Wind: 25 kt Min Pressure: 1005 hPa Position: 20.1, 82.1 Basin: North Indian
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.

IN-FA (WP302026)

Type: HU Max Wind: 120 kt Min Pressure: 945 hPa Position: 16.3, 152.9 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.
WDPN31 PGTW 291500 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR SUPER TYPHOON 30W (IN-FA) WARNING NR 025// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 16.6N 151.3E INITIAL INTENSITY: 130 KTS GEOGRAPHIC REFERENCE: 328 NM EAST-NORTHEAST OF SAIPAN MOVEMENT PAST 6 HOURS: WESTWARD AT 16 KTS SIGNIFICANT WAVE HEIGHT: 60 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: IN-FA IS LIKELY AT OR VERY NEAR SUPER TYPHOON (STY) STRENGTH. ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS CONTINUED COOLING OF CLOUD-TOP TEMPERATURES AND WARMING OF THE 40-NM WIDE EYE. THE EYE HAS WARMED TO +21.8 DEGREES CELSIUS FROM +17 DEGREES CELSIUS SIX HOURS AGO. THE DISTRIBUTION OF CLOUD-TOP TEMPERATURES IS VERY UNIFORM. AT 291200Z, THE NARROWEST WIDTHS OF THE BD-CURVE BLACK AND WHITE SHADES MEASURED APPROXIMATELY 60 NM AND 30 NM, RESPECTIVELY. A 291013Z METOP-B MHS PASS REVEALED A THICK RING SURROUNDING THE CENTER THAT LACKED DISTINCT BANDING FEATURES, SUPPORTING THE ASSESSMENT THAT THE SYSTEM HAS SOME ANNULAR CHARACTERISTICS. THE ACCOMPANYING ASCAT-B IMAGE INDICATED THAT THE CORE OF STORM- AND TYPHOON-FORCE WINDS IS RATHER LARGE WITH RESPECT TO THE EXTENT OF GALE-FORCE WINDS. A 290755Z SENTINEL-1C SAR PASS ESTIMATED SIMILAR WIND RADII WITH MAXIMUM WINDS NEAR 120 KTS. SINCE THAT TIME, THE STORM'S SATELLITE APPEARANCE HAS CONTINUED TO IMPROVE. THE DVORAK EIR EYE TECHNIQUE YIELDED A DATA T-NUMBER OF 7.0 BY 291300Z. HOWEVER, GIVEN THE EYE SIZE, THE ACTUAL INTENSITY WOULD LIKELY BE LOWER THAN 140 KTS. THEREFORE, THE INITIAL INTENSITY HAS BEEN RAISED TO 130 KTS WITH MEDIUM CONFIDENCE, WHICH IS CLOSEST TO D-MINT AND D-PRINT. THE INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE WELL-DEFINED EYE IN SHORTWAVE IR IMAGERY. THE ENVIRONMENT REMAINS FAVORABLE, WITH LOW VERTICAL WIND SHEAR (VWS) AND HIGH OCEAN HEAT CONTENT (OHC). INITIAL WIND RADII BASIS: SCATTEROMETER AND SAR DATA CURRENT STEERING MECHANISM: SOUTHWESTERN FLANK OF A DEEP-LAYER SUBTROPICAL RIDGE (STR) CENTERED NEAR 28N 165E AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T6.0 - 115 KTS RJTD: T6.5 - 127 KTS RCTP: T6.0 - 115 KTS CIMSS SATCON: 120 KTS AT 290510Z CIMSS ADT: 112 KTS AT 291130Z CIMSS AIDT: 124 KTS AT 291130Z CIMSS D-MINT: 129 KTS AT 291329Z CIMSS D-PRINT: 129 KTS AT 291130Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE VWS: 10-15 KTS SST: 29-30 CELSIUS OUTFLOW: MODERATE RADIAL ANALYSIS CONFIDENCE: INITIAL POSITION: HIGH INITIAL INTENSITY: MEDIUM INITIAL WIND RADII: HIGH 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. FORECAST DISCUSSION: STY 30W WILL CONTINUE WEST-NORTHWESTWARD ALONG THE SOUTHWESTERN PERIPHERY OF THE STR THROUGH TAU 36. A BROAD, LONGWAVE TROUGH PASSING OVER HONSHU WILL INDUCE A LARGE WEAKNESS IN THE STR, ALLOWING STY 30W TO TURN POLEWARD AND SLOW DOWN. THE PROGRESSIVE TROUGH WILL RACE DOWNSTREAM, AND A SEPARATE DEEP-LAYER STR TO THE WEST WILL BUILD EASTWARD, CLOSING OFF THE WEAKNESS AND CAUSING THE SYSTEM TO DEFLECT WESTWARD. BY THE END OF THE FORECAST PERIOD, ANOTHER TROUGH PASSING TO THE NORTH MAY CREATE ANOTHER OPENING, AND THE SYSTEM SHOULD SLOW DOWN AND TURN POLEWARD ONCE AGAIN. THERE REMAINS A GREAT DEAL OF UNCERTAINTY IN THE TRACK BEYOND TAU 36. THE INTERACTION OF THE LONGWAVE TROUGH WITH BOTH RIDGES WILL INFLUENCE THE POLEWARD EXTENT OF THE TRACK PRIOR TO THE WESTWARD DEFLECTION AND THE TIMING OF THE WESTWARD TURN. IF THE TROUGH PASSES MORE SLOWLY OR THE STR TO THE EAST CLOSES THE WEAKNESS MORE SLOWLY, STY 30W COULD TURN NORTHEASTWARD PRIOR TO DEFLECTING WESTWARD. AN ADDITIONAL SCENARIO EMERGES BY TAU 120. IF THE SECOND TROUGH IS WEAKER THAN PREDICTED OR THE WESTERN RIDGE BUILDS MORE STRONGLY, THE SYSTEM COULD CO…

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: NE (40°), 17.5 kt   |   Gust: 21.4 kt

Pressure: 30.05 steady   |   Air Temp: 79.7 °F

Water Temp: 80.2 °F   |   Dew Point: 75.0 °F

Swell: 4.9 ft   |   Wind Wave: 3.9 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.