🚨 Montgomery: None     🚨 SW Kenai Peninsula; NW Kenai Peninsula; Skilak Lake: Dense Fog Advisory issued October 27 at 9:17PM AKDT until October 28 at 10:00AM AKDT by NWS Anchorage AK     🚨 Upper Slopes of the Eastern Washington Cascades Crest: Winter Weather Advisory issued October 27 at 10:14PM PDT until October 28 at 5:00PM PDT by NWS Pendleton OR     🚨 Southern Hancock: Coastal Flood Advisory issued October 28 at 12:09AM CDT until October 29 at 4:00AM CDT by NWS New Orleans LA     🚨 Coastal waters from Cape Mendocino to Pt. Arena CA out 10 nm: Small Craft Advisory issued October 27 at 9:53PM PDT until October 29 at 3:00AM PDT by NWS Eureka CA     🚨 Waters from Cape Mendocino to Pt. Arena CA from 10 to 60 nm: Small Craft Advisory issued October 27 at 9:53PM PDT until October 29 at 3:00AM PDT by NWS Eureka CA     🚨 Tampa Bay waters; Charlotte Harbor and Pine Island Sound; Coastal waters from Tarpon Springs to Suwannee River FL out 20 NM; Coastal waters from Englewood to Tarpon Springs FL out 20 NM; Coastal waters from Bonita Beach to Englewood FL out 20 NM; Waters from Tarpon Springs to Suwannee River FL out 20 to 60 NM; Waters from Englewood to Tarpon Springs FL out 20 to 60 NM; Waters from Bonita Beach to Englewood FL out 20 to 60 NM: Small Craft Advisory issued October 28 at 12:50AM EDT until October 29 at 8:00AM EDT by NWS Tampa Bay Ruskin FL     🚨 San Diego County Coastal Areas; Orange County Coastal: Coastal Flood Warning issued October 27 at 9:34PM PDT until October 29 at 1:00PM PDT by NWS San Diego CA     🚨 Western Chelan County; Western Okanogan County: Winter Weather Advisory issued October 27 at 9:31PM PDT until October 28 at 5:00PM PDT by NWS Spokane WA     🚨 Sheboygan to Port Washington WI: Small Craft Advisory issued October 27 at 11:15PM CDT until October 29 at 7:00AM CDT by NWS Milwaukee/Sullivan WI    

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: 05 UTC 28 Oct 2026

Active storms summary

Select a Storm

VANCE (EP222026)

Type: TS Max Wind: 35 kt Min Pressure: 1003 hPa Position: 16.9, -108.3 Basin: East Pacific
ZCZC MIATCDEP2 ALL TTAA00 KNHC DDHHMM Tropical Storm Vance Discussion Number 27 NWS National Hurricane Center Miami FL EP222026 800 PM MST Tue Oct 27 2026 The structure of Vance continues to be heavily sheared and ragged based on the current visible satellite imagery. Some of the most recent images have shown that a small convective burst has occurred near the center, however it is also being blown away by the westerly wind shear at this point. In addition to the shear, there is dry air that is getting into the core of the storm, which is keeping the center of Vance fully exposed. The most recent objective intensity estimates from UW-CIMSS are in the range of 28-33 kt, while the latest TAFB Dvorak fix is a T2.0/30 kt. Given the available data the initial intensity has been held at 35 kt for this advisory. Vance is moving northwestward at 310/07 kt, as the storm is being steered by a low-level ridge centered over the south-central United States. A gradual turn toward the north is forecast over the next few days due to a strong mid-level trough moving across the U.S. West Coast. As a result, Vance should move toward the Gulf of California by Thursday. The current NHC track forecast is very similar to the previous one, with some minor adjustments being made based on the latest HCCA and GDMI forecast aids. The intensity portion of the forecast has plenty of uncertainties due to a variety of variables. The cyclone is over warm waters of 29-30 C for the next several days, but the wind shear is expected to be around 40 kt based on the GFS and ECMWF SHIPS guidance. This could allow for convection to develop near the center, but that convection will then be blown away by the shear. This could also mean that there could be brief fluctuations in intensity at times due to the convection. The most recent GFS and ECMWF simulated satellite guidance shows that there could be one or two more convective bursts from Vance due to some upper-level divergence sometime tomorrow. However, the impacts that this convection could have on the storm are still uncertain. At this point, the cyclone is still expected to become post-tropical around 36 h. By 60 h, it is expected to be a post-tropical remnant low, and finally by 72 h the circulation of Vance is forecast to dissipate. If the storm cannot maintain organized deep convection, it is possible that Vance could transition to a post-tropical cyclone sooner than currently forecast. Key Messages: 1. Periods of heavy rainfall associated with Vance will impact portions of western Mexico during much of this week. This rainfall may produce flooding and mudslides across central and southern Sinaloa, western Durango, and northwestern Nayarit, especially in areas along steep terrain. 2. Interests along the southwestern and west-central coasts of Mexico and the southern Baja California Peninsula should monitor the progress of Vance. FORECAST POSITIONS AND MAX WINDS INIT 28/0300Z 17.3N 108.4W 35 KT 40 MPH 12H 28/1200Z 18.5N 108.7W 35 KT 40 MPH 24H 29/0000Z 20.2N 108.5W 35 KT 40 MPH 36H 29/1200Z 21.7N 108.1W 35 KT 40 MPH...POST-TROPICAL 48H 30/0000Z 23.5N 107.7W 35 KT 40 MPH...POST-TROPICAL 60H 30/1200Z 25.3N 107.0W 30 KT 35 MPH...POST-TROP/REMNT LOW 72H 31/0000Z...DISSIPATED $$ Forecaster Katz/Beven NNNN

ARNAB (IO022026)

Type: HU Max Wind: 70 kt Min Pressure: 977 hPa Position: 16.4, 81.4 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.
WDIO31 PGTW 280300 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL CYCLONE 02B (ARNAB) WARNING NR 009// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 16.2N 81.6E INITIAL INTENSITY: 65 KTS GEOGRAPHIC REFERENCE: 543 NM SOUTHWEST OF KOLKATA, INDIA MOVEMENT PAST 6 HOURS: SOUTHWARD AT 02 KTS SIGNIFICANT WAVE HEIGHT: 20 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS A MASS OF CONVECTION ALONG THE COAST OF SOUTHEASTERN INDIA FULLY OBSCURING THE LOW-LEVEL CIRCULATION (LLCC) OF TROPICAL CYCLONE (TC) 02B. A FORTUITOUS 280030 SENTINEL-1D SAR PASS CAPTURED THE COMPACT LLCC JUST OFFSHORE. THE SAME SAR PASS REVEALED A PEAK VMAX OF 67 KTS IN THE SOUTHEAST QUADRANT. THE INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE SAR DATA. THE INITIAL INTENSITY OF 65 KTS IS ASSESSED WITH HIGH CONFIDENCE BASED ON THE SAME DATA. THE ENVIRONMENT IS UNFAVORABLE FOR FURTHER DEVELOPMENT WITH MODERATE TO HIGH VERTICAL WIND SHEAR AND THE PROXIMITY TO LAND. INITIAL WIND RADII BASIS: SAR DATA CURRENT STEERING MECHANISM: WEAK STEERING ENVIRONMENT CHARACTERIZED BY A WEAK DISTURBANCE (INVEST 90B) TEMPORARILY IMPEDING THE INFLUENCE OF A DEEP-LAYER SUBTROPICAL RIDGE (STR) CENTERED OVER EXTREME SOUTHERN CHINA. AGENCY DVORAK AND AUTOMATED FIXES: PGTW: NO CURRENT ESTIMATE DEMS: T4.0 - 65 KTS CIMSS AIDT: 88 KTS AT 272300Z CIMSS D-MINT: 79 KTS AT 272321Z CIMSS D-PRINT: 69 KTS AT 280000Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: UNFAVORABLE VWS: 20-25 KTS SST: 29-30 CELSIUS OUTFLOW: STRONG POLEWARD OTHER FACTORS: LAND INTERACTION ANALYSIS CONFIDENCE: INITIAL POSITION: HIGH INITIAL INTENSITY: HIGH INITIAL WIND RADII: HIGH 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. FORECAST DISCUSSION: TC 02B MANAGED TO WANDER BACK OFFSHORE OVER THE PAST 6 HOURS AS A WEAK DISTURBANCE (INVEST 90B) IMPEDED THE STEERING INFLUENCE OF THE STR TO ITS NORTHEAST. THE DISTURBANCE IS EXPECTED TO TRANSIT INLAND IMMINENTLY, WHICH SHOULD ALLOW THE STEERING RIDGE TO INDUCE A NORTHWARD TRAJECTORY TO 02B OVER THE NEXT 12 HOURS. THE NORTHWARD TRACK OVER LAND WILL RESULT IN RAPID DECAY OF THE SYSTEM, WITH DISSIPATION BY TAU 36. MODEL DISCUSSION: MODEL TRACK GUIDANCE HAS BEEN INSISTENT ABOUT THE NORTHWARD TURN AND CONTINUES TO DEPICT A DIRECT NORTHWARD TRACK. SURFACE FIELDS IN GFS AND ECMWF HAVE CORRECTLY DEPICTED A QUASI- STATIONARY PERIOD NEAR THE INDIAN COAST. THE JTWC TRACK FORECAST BLENDS THE TWO MODEL SOLUTIONS WITH A SLIGHTLY SLOWER TRACK THROUGH TAU 12, THEN FOLLOWS THE CONSENSUS. THE INTENSITY GUIDANCE IS IN UNANIMOUS AGREEMENT ABOUT THE RAPID DECAY OVER LAND. FORECAST CONFIDENCE: TRACK 00-72 HR: MEDIUM INTENSITY 00-72 HR: HIGH// NNNN

IN-FA (WP302026)

Type: HU Max Wind: 120 kt Min Pressure: 945 hPa Position: 14.9, 159.9 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 280300 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TYPHOON 30W (IN-FA) WARNING NR 019// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 14.9N 159.9E INITIAL INTENSITY: 120 KTS GEOGRAPHIC REFERENCE: 817 NM EAST OF SAIPAN MOVEMENT PAST 6 HOURS: WEST-NORTHWESTWARD AT 09 KTS SIGNIFICANT WAVE HEIGHT: 35 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS TYPHOON (TY) 30W WITH AN IMPRESSIVE 40 NM DIAMETER EYE THAT HAS ALMOST COMPLETELY CLEARED OUT AND WARMED TO 19 DEGREES CELSIUS OVER THE PAST 6 HOURS. THE SURROUNDING CENTRAL DENSE OVERCAST IS HIGHLY SYMMETRIC WITH UNIFORM COLD CLOUD TOPS. A 271859Z RCM-3 SAR PASS REVEALED THAT THE SYMMETRY IS ALSO REFLECTED IN THE RELATIVELY COMPACT SURFACE WIND FIELD. THE INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE CENTER OF THE EYE IN THE MSI. THE INITIAL INTENSITY OF 120 KTS IS ASSESSED WITH MEDIUM CONFIDENCE BASED ON A BLEND OF THE AGENCY DVORAK FIXES AND CIMSS INTENSITY ESTIMATES, ALTHOUGH THERE IS SOME UNCERTAINTY IN THOSE ESTIMATES GIVEN THE LARGE EYE. THE ENVIRONMENT IS CHARACTERIZED AS FAVORABLE, WITH WARM SEA SURFACE TEMPERATURES, GOOD RADIAL OUTFLOW ALOFT, AND LOW VERTICAL WIND SHEAR. INITIAL WIND RADII BASIS: SAR DATA CURRENT STEERING MECHANISM: SOUTHERN FLANK OF A SUBTROPICAL RIDGE EXTENSION TO THE NORTH AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T6.0 - 115 KTS RJTD: T6.5 - 127 KTS RCTP: T6.0 - 115 KTS PHFO: T6.5 - 127 KTS CIMSS SATCON: 130 KTS AT 280000Z CIMSS ADT: 129 KTS AT 280000Z CIMSS AIDT: 122 KTS AT 280000Z CIMSS D-MINT: 121 KTS AT 272315Z CIMSS D-PRINT: 133 KTS AT 280000Z 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: MEDIUM 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. FORECAST DISCUSSION: THE TRACK SPEED OF TY 30W HAS INCREASED TO 8 KTS OVER THE PAST 6 HOURS AS IT ACCELERATES WEST-NORTHWESTWARD UNDER THE STEERING INFLUENCE OF THE RIDGE EXTENSION TO THE NORTH. THE TRACK IS FORECAST TO CONTINUE WEST-NORTHWESTWARD AND CURVE POLEWARD THROUGH TAU 72 IN THIS ENVIRONMENT. A SECONDARY STR WILL BUILD IN FROM THE WEST, CREATING A COL REGION AND WEAK STEERING ENVIRONMENT FROM TAU 72 ONWARDS. THE SYSTEM IS EXPECTED TO HAVE A PERIOD OF ERRATIC AND SOMETIMES QUASI STATIONARY MOTION DURING THAT TIME, ALTHOUGH THAT CANNOT BE EXPLICITLY REPRESENTED IN THE TRACK FORECAST. THE TRACK FORECAST INSTEAD PLACES THE POSITION AT TAU 96 AND 120 IN THE GENERAL AREA OF THE MEAN MOTION VECTOR. THE INTENSITY OF TY 30W HAS REBOUNDED OVER THE PAST 12 HOURS AND IS FORECAST TO CONTINUE INCREASING TO A PEAK AROUND 130 KTS BEFORE LEVELING OFF. THE LARGE DIAMETER EYE AND SOME ATTEMPTS AT EYEWALL REPLACEMENT CYCLES ARE EXPLICITLY DEPICTED IN THE HAFS-A MODEL FIELDS WHICH WILL CONTRIBUTE TO THE INTENSITY CAP AND LATER GRADUAL WEAKENING. AFTER TAU 96, COLD WATER UPWELLING RESULTING FROM THE SLOW TRACK SPEED IS EXPECTED TO FURTHER CONTRIBUTE TO THE WEAKENING TREND. MODEL DISCUSSION: MODEL TRACK GUIDANCE IS IN VERY GOOD AGREEMENT THROUGH TAU 72, WITH A CROSS-TRACK SPREAD OF 65 NM AT THAT TIME AND MINIMAL ALONG-TRACK SPREAD. AFTER TAU 72 THE GUIDANCE SUITE DEPICTS A VARIETY OF SOLUTIONS WITH A FAIRLY WIDE SPREAD, BUT GENERALLY WITH WESTWARD AND SOUTHWARD COMPONENTS. THE JTWC TRACK FORECAST IS PLACED NEAR THE CONSENSUS THROUGH TAU 72, THEN AT A SUBJECTIVE MEAN AMONG THE SPREAD OF GUIDANCE FOR THE LATE TAUS. THE LATEST INTENSITY GUIDANCE HAS COME INTO CLOSER AGREEMENT WITHIN A 20 KT ENVELOPE, WITH THE EXCEPTION OF …

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: ENE (60°), 15.5 kt   |   Gust: 19.4 kt

Pressure: 30.08   |   Air Temp: 78.6 °F

Water Temp: 81.0 °F   |   Dew Point: 70.3 °F

Swell: 0.0 ft   |   Wind Wave: 5.2 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.