🚨 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.
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
Threshold
Probability
× Climatology
20kt/12hr
0%
0.0×
25kt/24hr
0%
0.0×
30kt/24hr
0%
0.0×
35kt/24hr
0%
0.0×
40kt/24hr
0%
0.0×
45kt/36hr
0%
0.0×
55kt/48hr
0%
0.0×
65kt/72hr
0%
0.0×
ARNAB
(IO022026)
Type: HUMax Wind: 70 ktMin Pressure: 977 hPaPosition: 16.4, 81.4Basin: 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
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.
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: 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.
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.