🚨 Montgomery: None 🚨 Otero, NM: Flash Flood Warning issued October 25 at 11:24PM MDT until October 26 at 2:30AM MDT by NWS El Paso Tx/Santa Teresa NM 🚨 Lake Okeechobee; Coastal waters from Chokoloskee to Bonita Beach FL out 20 NM; Coastal waters from East Cape Sable to Chokoloskee FL out 20 NM; Waters from Chokoloskee to Bonita Beach FL from 20 to 60 NM: Small Craft Advisory issued October 26 at 1:24AM EDT until October 28 at 8:00PM EDT by NWS Miami FL 🚨 Biscayne Bay; Coastal waters from Jupiter Inlet to Deerfield Beach FL out 20 NM; Coastal waters from Deerfield Beach to Ocean Reef FL out 20 NM; Waters from Jupiter Inlet to Deerfield Beach FL from 20 to 60 NM; Waters from Deerfield Beach to Ocean Reef FL from 20 to 60 NM excluding the territorial waters of Bahamas: Gale Warning issued October 26 at 1:24AM EDT until October 28 at 8:00AM EDT by NWS Miami FL 🚨 Biscayne Bay; Coastal waters from Jupiter Inlet to Deerfield Beach FL out 20 NM; Coastal waters from Deerfield Beach to Ocean Reef FL out 20 NM; Waters from Jupiter Inlet to Deerfield Beach FL from 20 to 60 NM; Waters from Deerfield Beach to Ocean Reef FL from 20 to 60 NM excluding the territorial waters of Bahamas: Small Craft Advisory issued October 26 at 1:24AM EDT until October 28 at 8:00PM EDT by NWS Miami FL 🚨 Hartley: Special Weather Statement issued October 26 at 12:21AM CDT by NWS Amarillo TX 🚨 Coastal Palm Beach County: Coastal Flood Warning issued October 26 at 1:20AM EDT until October 28 at 8:00PM EDT by NWS Miami FL 🚨 Coastal Palm Beach County: Coastal Flood Advisory issued October 26 at 1:20AM EDT until October 26 at 2:00AM EDT by NWS Miami FL 🚨 Coastal Palm Beach County: Rip Current Statement issued October 26 at 1:20AM EDT until October 28 at 8:00PM EDT by NWS Miami FL 🚨 Coastal Broward County; Coastal Miami Dade County: Rip Current Statement issued October 26 at 1:20AM EDT until October 28 at 8:00PM EDT by NWS Miami FL
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 19
NWS National Hurricane Center Miami FL EP222026
900 PM CST Sun Oct 25 2026
Vance's structure continues to degrade as seen in visible satellite
imagery and the GPM and AMSR3 microwave passes, due to strong
vertical wind shear and relatively dry mid-level air. Convection
continues to develop to the northeast of the center, but it is
mostly limited to that quadrant. The TAFB Dvorak fix was T3.5/55 kt
and the objective intensity estimates from UW-CIMSS are in 37-52 kt
range. Based on that data, the initial intensity has been lowered
to 55 kt.
Vance is currently moving toward the northwest, 305/6 kt. The
tropical storm is being steered by a mid-level ridge centered over
the south-central United States, along with a closed upper-level low
moving across the southwestern United States. The cyclone is
expected to continue to move toward the northwest to west-northwest
with a decrease in forward speed as the steering currents weaken. A
turn back to the north is expected by the middle of the week as an
amplified mid to upper-level trough moves over the eastern Pacific.
The current NHC track forecast has been adjusted a little to the
west of the previous one. Future adjustments to the west are likely
if the guidance trends continue.
The combination of southwesterly wind shear and relatively dry
mid-level air are expected to continue to gradually weaken the
storm. By the middle of this week, an upper-level trough will
further enhance the wind shear, resulting in additional weakening.
Both the GFS and ECMWF simulated satellite imagery suggest that
Vance will struggle to hold on to organized deep convection by late
this week. The current intensity forecast still calls for Vance
to become post-tropical at 96 h and degenerate into a remnant low by
120 h. However, the current intensity forecast is on the upper end
of the guidance envelope, as most of the guidance shows the rate of
weakening much faster than what is currently forecast. It is
certainly possible that the cyclone could weaken faster, which will
mean that it could become a remnant low sooner than what is
forecasted.
Key Messages:
1. Although the threat to southwest Mexico is decreasing
as the forecast track shifts westward away from the coast,
interests there should continue to monitor Vance's progress.
2. 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 Colima, Nayarit, and
Sinaloa, along with western portions of Michoacán, Jalisco, and
Durango, especially in areas along steep terrain.
FORECAST POSITIONS AND MAX WINDS
INIT 26/0300Z 15.0N 104.7W 55 KT 65 MPH
12H 26/1200Z 15.3N 105.3W 50 KT 60 MPH
24H 27/0000Z 15.7N 106.0W 45 KT 50 MPH
36H 27/1200Z 16.5N 106.8W 40 KT 45 MPH
48H 28/0000Z 17.4N 107.3W 40 KT 45 MPH
60H 28/1200Z 18.5N 107.6W 40 KT 45 MPH
72H 29/0000Z 20.0N 107.7W 40 KT 45 MPH
96H 30/0000Z 22.0N 107.8W 35 KT 40 MPH...POST-TROPICAL
120H 31/0000Z 24.0N 107.9W 30 KT 35 MPH...POST-TROP/REMNT LOW
$$
Forecaster Katz/Cangialosi
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×
TWO
(IO022026)
Type: TSMax Wind: 35 ktMin Pressure: 1002 hPaPosition: 16.0, 89.1Basin: 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.
WDIO31 PGTW 260300
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL CYCLONE 02B (TWO) WARNING NR
001//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 16.0N 89.1E
INITIAL INTENSITY: 35 KTS
GEOGRAPHIC REFERENCE: 398 NM SOUTH OF KOLKATA, INDIA
MOVEMENT PAST 6 HOURS: WESTWARD AT 05 KTS
SIGNIFICANT WAVE HEIGHT: 12 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS TROPICAL
CYCLONE (TC) 02B AS A CONSOLIDATING SYSTEM WITH STRONG DEEP CONVECTION
WHICH IS BEGINNING TO WRAP AROUND THE CENTER. THE BULK OF THE DEEP
CONVECTION IS LOCATED WEST OF CENTER, LEAVING LOW-LEVEL CLOUD BANDS
PARTIALLY EXPOSED IN THE EASTERN HEMISPHERE. ENVIRONMENTAL ANALYSIS
REVEALS A FAVORABLE ENVIRONMENT, CHARACTERIZED BY LOW (5-10 KTS)
VERTICAL WIND SHEAR (VWS), WARM (29-30 C) SEA SURFACE TEMPERATURES
(SST), AND STRONG WESTWARD OUTFLOW. THE INITIAL POSITION IS PLACED
WITH LOW CONFIDENCE BASED ON LOW-LEVEL CLOUD BANDING IN ANIMATED MSI.
THE INITIAL INTENSITY OF 35 KTS IS ASSESSED WITH MEDIUM CONFIDENCE
BASED ON THE PGTW DVORAK FIX AND AUTOMATED PRINT AND DMINT INTENSITY
ESTIMATES LISTED BELOW.
INITIAL WIND RADII BASIS: OBJECTIVE BEST TRACK
CURRENT STEERING MECHANISM: THE EASTERN EXTENSION OF A SUBTROPICAL
RIDGE (STR) CENTERED OVER SOUTHEAST ASIA
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.0 - 30 KTS
CIMSS D-MINT: 33 KTS AT 252209Z
CIMSS D-PRINT: 32 KTS AT 260100Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE
VWS: 0-5 KTS
SST: 29-30 CELSIUS
OUTFLOW: STRONG WESTWARD
ANALYSIS CONFIDENCE:
INITIAL POSITION: HIGH
INITIAL INTENSITY: HIGH
INITIAL WIND RADII: MEDIUM
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THIS INITIAL PROGNOSTIC REASONING
MESSAGE ESTABLISHES THE FORECAST PHILOSOPHY.
FORECAST DISCUSSION: TC 02B IS FORECAST TO CONTINUE TRACKING
GENERALLY WESTWARD WHILE IT IS STEERED BY THE EXTENSION OF A STR
CENTERED OVER SOUTHEAST ASIA. 02B IS EXPECTED TO MAKE LANDFALL
SOUTHEAST OF VISAKHAPATNAM AROUND TAU 48, WITH DISSIPATION
ANTICIPATED NO EARLIER THAN TAU 72. REGARDING INTENSITY, 02B IS
EXPECTED TO REMAIN IN A FAVORABLE ENVIRONMENT FOR THE NEXT 12-24
HOURS, WITH VWS REMAINING LOW. AFTER TAU 24, VWS IS EXPECTED TO
STEADILY INCREASE AND INDUCE DRY AIR ENTRAINMENT, HINDERING
DEVELOPMENT AND WEAKENING THE STORM PRIOR TO LANDFALL.
MODEL DISCUSSION: DETERMINISTIC MODEL TRACK GUIDANCE IS IN STRONG
AGREEMENT THROUGH LANDFALL, SUPPORTING THE JTWC TRACK FORECAST WITH
HIGH CONFIDENCE. RELIABLE INTENSITY AIDS ARE IN POOR AGREEMENT
THROUGH TAU 48. SEVERAL JTWC RAPID INTENSIFICATION (RI) AIDS MET
TRIGGER CRITERIA, INDICATING THE POSSIBILITY OF RI WITHIN THE NEXT
48 HOURS, WHICH COULD RESULT IN A SIGNIFICANTLY HIGHER PEAK THAN
CURRENTLY FORECAST. THE PEAK INTENSITY RANGES FROM 55 KTS (GFS) TO
105 KTS (FRIA AND RIDE). THE JTWC INTENSITY FORECAST HEDGES ON THE
CONSERVATIVE SIDE, ACCOUNTING FOR THE DEGRADING ENVIRONMENT AFTER
TAU 24. THE JTWC INTENSITY FORECAST IS IN CLOSE AGREEMENT WITH
COAMPS-TC AND THE MULTI-MODEL CONSENSUS WITH OVERALL LOW
CONFIDENCE.
FORECAST CONFIDENCE:
TRACK 00-72 HR: HIGH
INTENSITY 00-72 HR: LOW//
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.
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 260300
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TYPHOON 30W (IN-FA) WARNING NR 011//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 13.8N 163.2E
INITIAL INTENSITY: 85 KTS
GEOGRAPHIC REFERENCE: 1014 NM EAST OF SAIPAN
MOVEMENT PAST 6 HOURS: NORTHWESTWARD AT 08 KTS
SIGNIFICANT WAVE HEIGHT: 30 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS TYPHOON (TY)
30W AS A MUCH-IMPROVED SYSTEM WHEN COMPARED TO 6 HOURS AGO. THE UPPER-
LEVEL CONVECTION IS FINALLY MAINTAINING PATCHES OF SUB-NEGATIVE 80 C
CLOUD TOP TEMPERATURES, WHICH ARE WRAPPED AROUND THE CENTRAL AXIS. A
NASCENT RAGGED EYE FEATURE IS FORMING IN THE ANIMATED BRIGHTNESS
TEMPERATURES, WITH A CORRELATING DIMPLE IN THE ANIMATED MSI. THE
252230Z ASCAT PASS REVEALS A VERY COMPACT WIND FIELD, WITH TYPHOON-
FORCE WINDS CONFINED TO WITHIN APPROXIMATELY 20 NM OF THE CORE.
ENVIRONMENTAL ANALYSIS REVEALS A HIGHLY FAVORABLE ENVIRONMENT,
CHARACTERIZED BY LOW (10-15 KTS) VERTICAL WIND SHEAR (VWS), WARM (29-
30 C) SEA SURFACE TEMPERATURES (SST), GOOD (100-125 KJ PER CM SQUARED)
OCEAN HEAT CONTENT (OHC), AND STRONG POLEWARD OUTFLOW. THE INITIAL
POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE NASCENT RAGGED
EYE FORMING IN ANIMATED MSI. THE INITIAL INTENSITY OF 80 KTS IS
ASSESSED WITH MEDIUM CONFIDENCE BASED ON THE AGENCY DVORAK FIXES AND
AUTOMATED CIMMS INTENSITY ESTIMATES LISTED BELOW.
INITIAL WIND RADII BASIS: 262230Z ASCAT DATA
CURRENT STEERING MECHANISM: A COMPETING STEERING ENVIRONMENT
BETWEEN THE NORTHWESTERN FLANK OF A DEEP-LAYER NEAR-EQUATORIAL
RIDGE (NER) TO THE SOUTHEAST AND A SUBTROPICAL RIDGE (STR) CENTERED
TO THE NORTHWEST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T5.0 - 90 KTS
RJTD: T4.5 - 77 KTS
RCTP: T4.5 - 77 KTS
PHFO: T5.0 - 90 KTS
CIMSS SATCON: 65 KTS AT 252200Z
CIMSS ADT: 74 KTS AT 252330Z
CIMSS AIDT: 73 KTS AT 260030Z
CIMSS D-MINT: 70 KTS AT 252228Z
CIMSS D-PRINT: 80 KTS AT 260000Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: HIGHLY FAVORABLE
VWS: 10-15 KTS
SST: 28-29 CELSIUS
OUTFLOW: STRONG POLEWARD
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: TS 30W (IN-FA) IS FORECAST TO CONTINUE TRACKING
FOR THE NEXT 12 HOURS WHILE IT REMAINS ON THE NORTHWESTERN PERIPHERY
OF THE NER CENTERED TO ITS SOUTHEAST. THE SUBTROPICAL RIDGE (STR) TO
THE NORTHWEST HAS STRETCHED EASTWARD, WHICH CREATED A COMPETING
STEERING ENVIRONMENT, INDUCING A SLIGHT SLOWDOWN IN IN-FA'S
NORTHWESTWARD TRACK. THE STR IS EXPECTED TO BUILD AND GAIN STEERING
AUTHORITY BY TAU 24, WHICH IS EXPECTED TO CAUSE 30W TO ACCELERATE
WEST-NORTHWESTWARD THROUGH THE TAU 72. BETWEEN TAU 48-60, AN UPPER-
LEVEL TROUGH IS EXPECTED TO PASS NORTH OF THE STR, FORCING THE RIDGE
TO RETREAT EASTWARD AND INDUCING A NORTHWESTWARD TRACK FOR 30W BETWEEN
TAU 96-120 AS IT BEGINS TO CURL AROUND THE RIDGE'S SOUTHEASTERN
PERIPHERY. REGARDING INTENSITY, 30W IS ASSESSED TO BE RAPIDLY
INTENSIFYING, AND IS FORECAST TO CONTINUE RI THROUGH TAU 12. AT AROUND
TAU 12, THE COMPETING STEERING ENVIRONMENT IS ANTICIPATED TO
TEMPORARILY HALT INTENSIFICATION AS THE PROBABILITY FOR ADVERSE
IMPACTS OF UPWELLING INCREASES. ONCE 30W TRANSITIONS STEERING
ENVIRONMENTS AND BEGINS TRACKING WEST-NORTHWESTWARD, THE ENVIRONMENT
WILL REMAIN FAVORABLE, SUPPORTING A SECOND ROUND OF INTENSIFICATION.
AS 30W GAINS INTENSITY, IT MAY UNDERGO AN EYEWALL REPLACEMENT CYCLE
(ERC), WHICH WOULD INDUCE TEMPORARY WEAKENING AND EXPAND THE WIND
FIELD. AT LEAST ONE ERC IS DEPICTED IN THE HAFS-A MODEL GUIDANCE
BETWEEN TAU 24-60, BUT MORE ARE…
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 (50°), 25.3 kt | Gust: 29.1 kt
Pressure: 30.12 steady | Air Temp: 79.0 °F
Water Temp: 80.4 °F | Dew Point: 71.8 °F
Swell: 3.6 ft | Wind Wave: 7.2 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.