🚨 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.
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
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
9999%
9999.0×
ARNAB
(IO022026)
Type: TDMax Wind: 25 ktMin Pressure: 1005 hPaPosition: 20.1, 82.1Basin: 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.
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.
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: 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.
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.