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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 MIATCDEP3 ALL
TTAA00 KNHC DDHHMM
Hurricane Rachel Discussion Number 25
NWS National Hurricane Center Miami FL EP182026
200 AM MST Sat Oct 03 2026
Rachel has become less organized during the past several hours. The
associated convection is now occurring only over the southern
semicircle, and the latest microwave imagery indicates that there
is no longer any eyewall. Satellite intensity estimates are in the
70-90 kt range and are trending downward. Based on the trend, the
initial intensity is lowered to 80 kt.
The initial motion is 275/4 kt. A mid-level anticyclone over the
western United States has a ridge extending southwest to the west
of Rachel, and this anticyclone is expected to build westward
during the next 72 h. This evolution should steer the cyclone
slowly west-northwestward for the next day or two, followed by a
more westward motion. By 96-120 h, a west-northwestward motion is
likely to resume as Rachel approaches the western end of the ridge.
The new forecast track is close to the previous forecast for 48-60
h, and then is nudged a little south based on a southward shift in
the guidance envelope.
Additional slow weakening is forecast during the next 24-36 h as
Rachel continues to experience northeasterly shear and crosses the
cold water wake of Hurricane Polo. After that, the sea surface
temperatures increase slightly at a time where the hurricane is
likely to entrain dry air. These competing factors are expected to
result in little net change in strength between 36-72 h. After 72
h, Rachel should move over progressively colder water and continue
to entrain dry air, which should cause a steady weakening.
FORECAST POSITIONS AND MAX WINDS
INIT 03/0900Z 19.4N 111.8W 80 KT 90 MPH
12H 03/1800Z 19.6N 112.4W 80 KT 90 MPH
24H 04/0600Z 19.9N 113.2W 75 KT 85 MPH
36H 04/1800Z 20.1N 114.1W 70 KT 80 MPH
48H 05/0600Z 20.2N 115.2W 70 KT 80 MPH
60H 05/1800Z 20.4N 116.7W 70 KT 80 MPH
72H 06/0600Z 20.6N 118.4W 70 KT 80 MPH
96H 07/0600Z 21.2N 121.7W 65 KT 75 MPH
120H 08/0600Z 22.2N 125.0W 55 KT 65 MPH
$$
Forecaster Beven
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.
WDPN32 PGTW 030900
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TYPHOON 26W (CHOI-WAN) WARNING NR 014//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 19.4N 145.9E
INITIAL INTENSITY: 80 KTS
GEOGRAPHIC REFERENCE: 252 NM NORTH OF SAIPAN
MOVEMENT PAST 6 HOURS: NORTH-NORTHEASTWARD AT 09 KTS
SIGNIFICANT WAVE HEIGHT: 32 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS TYPHOON 26W
(CHOI-WAN) WITH A CLOUD-FILLED EYE AND A MORE DISORGANIZED
CONVECTIVE STRUCTURE COMPARED TO 6 HOURS AGO. THE MSI ALSO SHOWS
SOME DRY AIR BEING PULLED INTO THE CORE OF 26W ALONG THE WESTERN
PERIPHERY, WHICH COULD BE THE CAUSE FOR THE HALTED DEVELOPMENT. A
030228Z AMSR3 37 GHZ MICROWAVE IMAGE REVEALED AN ELLIPTIC MICROWAVE
EYE FEATURE WITH A SLIGHT WEAKNESS IN THE WESTERN SEMICIRCLE. THE
89 GHZ VERSION OF THE SAME PASS SHOWED THE STRONGEST CONVECTION
CONFINED TO THE SOUTHEASTERN QUADRANT OF THE SYSTEM. THE INITIAL
POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE ANIMATED MSI
AND EXTRAPOLATION FROM THE AMSR3 MICROWAVE IMAGE SUITE. THE INITIAL
INTENSITY OF 80 KTS IS ASSESSED WITH MEDIUM CONFIDENCE BASED ON A
COMBINATION OF THE AGENCY DVORAK FIXES OF T5.0 AND THE LOWER CIMSS
INTENSITY ESTIMATES.
INITIAL WIND RADII BASIS: PERSISTENCE FROM THE 022345Z METOP-B
ASCAT PASS WITH MINOR ADJUSTMENTS BASED ON THE OBJECTIVE BEST TRACK
CURRENT STEERING MECHANISM: THE WESTERN EXTENSION OF A SUBTROPICAL
RIDGE (STR) POSITIONED TO THE NORTHEAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T5.0 - 90 KTS
RJTD: T5.0 - 90 KTS
RCTP: T5.0 - 90 KTS
CIMSS SATCON: 77 KTS AT 030600Z
CIMSS ADT: 59 KTS AT 030600Z
CIMSS AIDT: 63 KTS AT 030600Z
CIMSS D-PRINT: 76 KTS AT 030600Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE
VWS: 5-10 KTS
SST: 29-30 CELSIUS
OUTFLOW: STRONG POLEWARD AND EQUATORWARD
OTHER FACTORS: SLIGHT DRY AIR ENTRAINMENT ALONG THE WESTERN
PERIPHERY
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 STEERING MECHANISM FOR 26W HAS SHIFTED
FROM THE NEAR EQUATORIAL RIDGE TO THE SUBTROPICAL RIDGE TO THE
NORTHEAST. THIS HAS CAUSED THE TRAJECTORY TO BECOME SLIGHTLY
MORE NORTHWARD OVER PAST 6 HOURS. 26W IS FORECAST TO TURN FURTHER
NORTHWARD AS IT TRACKS ALONG THE WESTERN PERIPHERY OF THE STR
THROUGH TAU 72. AFTER TAU 72, THE SYSTEM WILL ACCELERATE
NORTHEASTWARD AS IT ROUNDS THE RIDGE AXIS AND BEGINS TO INTERACT
WITH THE STRONG UPPER-LEVEL FLOW. EXTRATROPICAL TRANSITION IS
EXPECTED TO BE COMPLETE AROUND TAU 96, SOUTH OF THE KAMCHATKA
PENINSULA, ONCE THE SYSTEM BECOMES EMBEDDED UNDERNEATH THE JET. IN
TERMS OF INTENSITY, 26W IS FORECAST TO INTENSIFY OVER THE NEXT 24
HOURS TO A PEAK INTENSITY OF AROUND 105 KTS AS THE ENVIRONMENT
REMAINS FAVORABLE WITH LOW SHEAR, VERY WARM SST, AND ROBUST
OUTFLOW. THE PRIMARY LIMITING FACTOR WILL BE THE DRY AIR TO THE
WEST. AROUND TAU 36, OCEAN HEAT CONTENT WILL START TO DROP AND
EQUATORWARD OUTFLOW WILL BECOME RESTRICTED, CAUSING 26W TO WEAKEN
THROUGH TAU 72. FOLLOWING TAU 72, THE SYSTEM WILL TAP INTO AN
EXTREME POLEWARD OUTFLOW CHANNEL, SUPPORTED BY A VERY STRONG JET
MAX TO THE NORTH. THIS WILL OFFSET THE COOL SST AND HIGH
SOUTHWESTERLY VERTICAL WIND SHEAR, ALLOWING FOR 26W TO LIKELY
MAINTAIN TYPHOON INTENSITY THROUGH THE INITIAL STAGES OF
FRONTOGENESIS.
MODEL DISCUSSION: MODEL TRACK GUIDANCE IS IN MODERATE AGREEMENT
THROUGH TAU 72 WITH MOST OF THE UNCERTAINTY REVOLVING AROUND THE
SPEED OF ADVANCE AROUND THE RIDGE. WHILE CROSS-TRACK SPREAD IS ONLY
AROUND 100 NM AT TAU 72, ALONG-TRACK SPREAD IS ABOUT 250 NM. GFS
AND NAVGEM ARE THE SLOWEST TRA…
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: SE (130°), 15.5 kt | Gust: 19.4 kt
Pressure: 29.85 | Air Temp: 83.5 °F
Water Temp: 85.8 °F | Dew Point: 80.2 °F
Swell: 3.6 ft | Wind Wave: 2.6 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.