🚨 San Juan, NM: Flood Warning issued October 23 at 11:31PM MDT until October 25 at 12:00PM MDT by NWS Albuquerque NM 🚨 North Oregon Coast Range Lowlands; North Oregon Coast Range; West Central Willamette Valley; East Central Willamette Valley; Benton County Lowlands; Linn County Lowlands; Lane County Lowlands; Cascade Foothills of Marion and Linn Counties; Lane County Cascade Foothills: Freeze Warning issued October 23 at 10:30PM PDT until October 24 at 10:00AM PDT by NWS Portland OR 🚨 Clatsop County Coast; Tillamook County Coast; Central Coast of Oregon; Central Oregon Coast Range Lowlands; Central Oregon Coast Range; Lower Columbia River; Tualatin Valley; Inner Portland Metro; East Portland Metro; Outer Southeast Portland Metro; West Columbia River Gorge of Oregon above 500 ft; Clackamas County Cascade Foothills; Willapa Hills; Cowlitz County Lowlands; North Clark County Lowlands; Inner Vancouver Metro; East Clark County Lowlands; South Washington Cascade Foothills: Frost Advisory issued October 23 at 10:30PM PDT until October 24 at 10:00AM PDT by NWS Portland OR 🚨 San Juan, NM: Flood Warning issued October 23 at 11:27PM MDT until October 24 at 12:00PM MDT by NWS Albuquerque NM 🚨 Montgomery: None 🚨 Clarence Strait: Small Craft Advisory issued October 23 at 9:23PM AKDT until October 24 at 5:00PM AKDT by NWS Juneau AK 🚨 Southern Chatham Strait: Small Craft Advisory issued October 23 at 9:23PM AKDT until October 24 at 5:00PM AKDT by NWS Juneau AK 🚨 Northern Lynn Canal: Small Craft Advisory issued October 23 at 9:23PM AKDT until October 24 at 5:00PM AKDT by NWS Juneau AK 🚨 Archuleta, CO: Flood Warning issued October 23 at 11:21PM MDT until October 24 at 3:00PM MDT by NWS Grand Junction CO 🚨 Lewiston Area; Lower Garfield and Asotin Counties; Moses Lake Area: Freeze Warning issued October 23 at 10:20PM PDT until October 24 at 10:00AM PDT by NWS Spokane WA
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
Hurricane Vance Discussion Number 11
NWS National Hurricane Center Miami FL EP222026
900 PM CST Fri Oct 23 2026
Correction: Updated to emphasize that Vance briefly reached major
hurricane intensity earlier this evening before weakening to
Category 2 strength.
Satellite imagery indicates that Vance became better organized
earlier this evening, with cloud-top temperatures cooling and deep
convection expanding around a warming eye. However, the eye has
become less distinct during the past hour or two, with some warming
of the cloud tops in the eyewall, possibly due to moderate southerly
vertical wind shear. The subjective Dvorak intensity estimate from
TAFB was T5.5/102 kt, although recent objective intensity estimates
have trended downward toward 95 kt. Vance briefly reached major
hurricane intensity earlier this evening before the recent
deterioration in its satellite presentation. Given the recent
degradation in satellite presentation and the latest objective
estimates, the initial intensity is set at 95 kt.
Vance is moving north-northwestward, or 345/6 kt. This general
motion is expected to continue during the next couple of days as a
broad mid- to upper-level trough evolves over the western portion of
the United States, weakening the subtropical ridge over Mexico.
Although the track guidance remains in relatively good agreement
through 24 to 36 h, forecast confidence decreases thereafter as the
trough shifts eastward and Vance enters a region of weaker steering
currents. Significant cross-track spread persists among the guidance
solutions, partly due to differences in how well Vance maintains its
vertical structure as increasing shear affects the cyclone. A
weaker, more vertically tilted system could be steered farther
westward, while a stronger, vertically coupled hurricane would be
more likely to continue northward toward the southwestern or
west-central coast of Mexico. Given these persistent differences,
the NHC track forecast remains largely unchanged from the previous,
lying close to the HCCA and GDMI aids.
Vance may have reached its peak intensity earlier this evening after
rapidly intensifying from 60 to 100 kt over the preceding 24 h.
Although some additional strengthening is possible in the short
term, recent satellite trends suggest that the hurricane may be
beginning to feel the effects of a less favorable environment.
Cooler sea surface temperatures associated with the wakes of recent
tropical cyclones have reduced the ocean heat content along portions
of Vance's forecast track. These cooler waters, combined with
increasing vertical wind shear, should contribute to a weakening
trend during the next day or two. However, the magnitude of
weakening remains uncertain and will depend partly on how long Vance
remains over the cooler waters. The aforementioned differences in
the track guidance have also contributed to considerable spread
among the intensity solutions, with the possibility of more
substantial weakening than currently forecast. Vance could move
beyond the cooler waters after 48 h, allowing for some
restrengthening. Thereafter, increasing vertical wind shear,
decreasing mid-level moisture, and possible land interaction should
lead to another weakening trend late in the forecast period. The NHC
intensity forecast remains similar to the previous prediction and
lies near the upper end of the guidance envelope through much of the
forecast period.
FORECAST POSITIONS AND MAX WINDS
INIT 24/0300Z 12.0N 102.6W 95 KT 110 MPH
12H 24/1200Z 12.8N 102.8W 105 KT 120 MPH
24H 25/0000Z 13.8N 103.1W 100 KT 115 MPH
36H 25/1200Z 14.8N 103.4W 90 KT 105 MPH
48H 26/0000Z 15.8N 103.8W 85 KT 100 MPH
60H 26/1200Z 16.3N 104.0W 90 KT 105 MPH
72H 27/0000Z 16.8N 104.2W 95 KT 110 MPH
96H 28/0000Z 17.6N 104.3W 85 KT 100 MPH
120H 29/0000Z 18.4N 104.4W 70 KT 80 MPH
$$
Forecaster Pierce/Gibbs
NNNN
Threshold
Probability
× Climatology
20kt/12hr
13%
2.1×
25kt/24hr
17%
1.4×
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×
98I
(IO982026)
Type: TDMax Wind: 25 ktMin Pressure: 1004 hPaPosition: 16.0, 89.3Basin: 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.
WDPN32 PGTW 240300
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TYPHOON 29W (CHAMPI) WARNING NR 039//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 24.8N 123.3E
INITIAL INTENSITY: 65 KTS
GEOGRAPHIC REFERENCE: 100 NM EAST OF TAIPEI, TAIWAN
MOVEMENT PAST 6 HOURS: EAST-NORTHEASTWARD AT 10 KTS
SIGNIFICANT WAVE HEIGHT: 30 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
TY 29W HAS RAPIDLY WEAKENED OVER THE PAST SIX HOURS DUE PRIMARILY
TO LAND INTERACTION WITH TAIWAN. THE SYSTEM HAS COMPLETED A LOOP TO
THE EAST OF TAIWAN AND IS RETURNING TO A POLEWARD TRAJECTORY.
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS A PARTIALLY
EXPOSED LOW-LEVEL CIRCULATION WITH LIMITED AND RELATIVELY SHALLOW
CONVECTION ALONG THE EASTERN PERIPHERY. THE INITIAL POSITION IS
PLACED WITH MEDIUM CONFIDENCE BASED ON A GROUPING OF SUBJECTIVE
GEOSTATIONARY SATELLITE POSITION AND RADAR FIXES FROM VARIOUS
REPORTING AGENCIES. THE INITIAL INTENSITY OF 65 KTS IS ASSESSED
WITH MEDIUM CONFIDENCE BASED ON THE LOW END OF SUBJECTIVE DVORAK
AND AUTOMATED INTENSITY ESTIMATES LISTED BELOW, AS WELL AS A 232143Z
SENTINEL-1 SAR PASS INDICATING A LARGE BAND OF 60-65 KNOT WINDS
SOUTHEAST OF THE CIRCULATION CENTER.
INITIAL WIND RADII BASIS: OBJECTIVE BEST TRACK
CURRENT STEERING MECHANISM: DEEP-LAYER SUBTROPICAL RIDGE (STR) TO
THE EAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T4.5 - 77 KTS
RJTD: T4.5 - 77 KTS
RCTP: T4.0 - 65 KTS
CIMSS ADT: 92 KTS AT 232330Z
CIMSS AIDT: 77 KTS AT 232330Z
CIMSS D-MINT: 70 KTS AT 232053Z
CIMSS D-PRINT: 60 KTS AT 232330Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: UNFAVORABLE
VWS: 10-15 KTS
SST: 26-27 CELSIUS
OUTFLOW: STRONG POLEWARD
ANALYSIS CONFIDENCE:
INITIAL POSITION: MEDIUM
INITIAL INTENSITY: MEDIUM
INITIAL WIND RADII: MEDIUM
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: FORECAST INTENSITIES HAVE DECREASED
AND THE INITIAL PORTION OF THE FORECAST TRACK HAS SHIFTED EASTWARD
SLIGHTLY FROM THE PREVIOUS FORECAST DUE TO OBSERVED POSITION AND
STRUCTURAL CHANGES.
FORECAST DISCUSSION: AFTER INITIALLY POLEWARD MOTION, TY 29W WILL
TURN NORTH-NORTHEASTWARD AROUND THE PERIPHERY OF THE CURRENT
SUBTROPICAL STEERING RIDGE THROUGH THE FORECAST PERIOD. EXTRATROPICAL
TRANSITION WILL BEGIN BY TAU 36 AS THE SYSTEM INTERACTS WITH A
DEVELOPING MID-LATITUDE TROUGH TO THE NORTHWEST. TY 29W WILL MERGE
WITH THE TROUGH AND BECOME FULLY EMBEDDED BY TAU 60. STEADY WEAKENING
WILL OCCUR PRIOR TO EXTRATROPICAL TRANSITION DUE TO ONGOING
ENTRAINMENT OF DRIER AIR FROM THE WEST, PASSAGE OVER MARGINAL (25-26C)
SEA SURFACE TEMPERATURES, AND INCREASING VERTICAL WIND SHEAR.
MODEL DISCUSSION: NUMERICAL MODEL TRACK FORECAST GUIDANCE REMAINS
IN GOOD AGREEMENT REGARDING THE OVERALL SCENARIO. THE PHYSICS-BASED
AND AI MODEL CONSENSUSES ARE SPREAD BY ABOUT 50 NM FROM TAU 24
ONWARD, WITH THE AI CONSENSUS SITUATED TO THE SOUTH AND BOTH DEPICTING
SIMILAR TRACK SPEEDS. THE CURRENT JTWC FORECAST MAINLY SPLITS THE
DIFFERENCE BETWEEN THE TWO CONSENSUS SOLUTIONS AND, ALTHOUGH LYING
A BIT TO THE EAST EARLY ON DUE TO RECENT STORM MOTION, IS
CONSISTENT WITH THE PREVIOUS JTWC TRACK FORECAST AFTER TAU 24.
INTENSITY FORECAST GUIDANCE IS IN VERY GOOD AGREEMENT REGARDING A
CONTINUED STEADY WEAKENING TREND AND FLATLINE TREND FOLLOWING
EXTRATROPICAL TRANSITION AS THE SYSTEM MERGES INTO A MID-LATITUDE
TROUGH AND LIKELY BECOMES INDISTINGUISHABLE AS A SEPARATE
CIRCULATION.
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 240300
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 30W (IN-FA) WARNING NR
003//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 10.4N 166.2E
INITIAL INTENSITY: 45 KTS
GEOGRAPHIC REFERENCE: 139 NM NORTHWEST OF KWAJALEIN
MOVEMENT PAST 6 HOURS: SOUTH-SOUTHWESTWARD AT 02 KTS
SIGNIFICANT WAVE HEIGHT: 15 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
TS 30W HAS INTENSIFIED WHILE REMAINING QUASI-STATIONARY OVER THE
PAST SIX HOURS. ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI)
DEPICTS INCREASINGLY ORGANIZED DEEP CONVECTIVE BANDING WRAPPING
INTO A LOW-LEVEL CIRCULATION EVIDENT IN A 232132Z METOP-B ASCAT
SCATTEROMETER PASS. THE INITIAL POSITION IS PLACED WITH HIGH
CONFIDENCE BASED ON THE ASCAT DATA AND SATELLITE POSITION FIXES
FROM MULTIPLE REPORTING AGENCIES. THE INITIAL INTENSITY OF 45 KTS
IS ASSESSED WITH MEDIUM CONFIDENCE ABOVE THE SUBJECTIVE DVORAK AND
AUTOMATED INTENSITY ESTIMATES LISTED BELOW BASED ON SMALL AREA OF
NEAR-CENTER 40 TO 45 KNOT WINDS EVIDENT IN THE ASCAT DATA.
INITIAL WIND RADII BASIS: 232132Z METOP-B ASCAT SCATTEROMETER DATA
CURRENT STEERING MECHANISM: COMPETING STEERING ENVIRONMENT
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.5 - 35 KTS
RJTD: T2.5 - 35 KTS
RCTP: T2.5 - 35 KTS
PHFO: T2.5 - 35 KTS
CIMSS ADT: 35 KTS AT 232340Z
CIMSS AIDT: 34 KTS AT 232340Z
CIMSS D-MINT: 34 KTS AT 232254Z
CIMSS D-PRINT: 37 KTS AT 240010Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE
VWS: 5-10 KTS
SST: 29-30 CELSIUS
OUTFLOW: MODERATE POLEWARD AND EQUATORWARD
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: TS 30W WILL REMAIN QUASI-STATIONARY OVER
THE NEXT FEW HOURS IN A COMPETING STEERING ENVIRONMENT BETWEEN
NEAR-EQUATORIAL RIDGING TO THE SOUTHEAST AND A SOUTHWARD EXTENSION
OF SUBTROPICAL RIDGING TO THE WEST. BY TAU 12, THE NEAR-EQUATORIAL
RIDGE WILL BUILD THE SOUTHEAST, BECOME THE DOMINANT STEERING
MECHANISM, AND PUSH TS 30W TOWARD A NORTH-NORTHWESTWARD TRAJECTORY.
A BUILDING SUBTROPICAL RIDGE TO THE NORTH WILL EXERT AN INCREASING
INFLUENCE ON STORM MOTION AFTER TAU 48, INDUCING A TEMPORARY
SLOWDOWN. AFTER TAU 72, THE SUBTROPICAL RIDGE WILL BECOME THE
DOMINANT STEERING MECHANISM AND PUSH THE SYSTEM WESTWARD. RAPID
NEAR-TERM INTENSIFICATION IS EXPECTED UNDER THE FAVORABLE
INFLUENCES OF LOW VERTICAL WIND SHEAR AND SUPPORTIVE POLEWARD AND
EQUATORWARD UPPER-LEVEL OUTFLOW BOOSTED BY A TROPICAL UPPER
TROPOSPHERIC TROUGH TO THE NORTH. IN THE EXTENDED RANGE, ADDITIONAL
INTENSIFICATION IS EXPECTED, BUT THE RATE SHOULD SLOW A BIT AS THE
OUTFLOW PATTERN BECOMES LESS FAVORABLE.
MODEL DISCUSSION: NUMERICAL MODEL GUIDANCE CONTINUES TO TIGHTEN IN
DIRECTION AND SPEED, WITH ALL MODELS DEPICTING A SIMILAR EVOLUTION
OF THE STEERING PATTERN. THE CURRENT JTWC TRACK FORECAST LIES AT
THE MIDPOINT OF AN ENVELOPE OF NEARLY ALL SOLUTIONS THAT IS
BRACKETED BY THE AI GFS ON THE SOUTHERN SIDE AND ECMWF
DETERMINISTIC MODEL ON THE NORTHERN SIDE. SOLUTIONS FAN OUT EVENLY
FROM THE START ACROSS THE DISTRIBUTION, PEAKING AT ABOUT 320 NM OF
SEPARATION BY TAU 120. THE CURRENT TRACK FORECAST IS GENERALLY
CONSISTENT WITH THE PREVIOUS ONE. INTENSITY GUIDANCE IS IN FAIRLY
GOOD AGREEMENT THROUGH THE FORECAST CYCLE, WITH COAMPS-TC A BIT
MORE AGGRESSIVE AND HAFS A BIT LESS AGGRESSIVE IN THE NEAR-TERM.
RAPID INTENSIFICATION AIDS HAVE TRIGGERED ON THE LATEST CYCLE, AND
THE NEAR-TERM INTENSITY FORECAST HAS BEEN INCREASED SLIGHTLY IN
RESPONSE. OTHERWISE, THE CURRENT FORECAST IS CONSISTENT WITH THE
PREVIOUS JTWC INTENSITY FORECAST AND LIES NEAR THE COAMPS-TC, HAFS,
AND GOOGLE DEEPMIND INTENSITIES …
AGUEDA
(SH022027)
Type: TDMax Wind: 30 ktMin Pressure: 1009 hPaPosition: -5.5, 46.7Basin: South 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.
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°), 13.6 kt | Gust: 17.5 kt
Pressure: 30.11 steady | Air Temp: 79.0 °F
Water Temp: 81.1 °F | Dew Point: 63.0 °F
Swell: 1.6 ft | Wind Wave: 3.3 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.