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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 15
NWS National Hurricane Center Miami FL EP182026
200 PM MST Wed Sep 30 2026
Data from a NOAA Hurricane Hunter aircraft along with conventional
and microwave satellite imagery shows that Rachel has been
re-organizing for the past several hours. Microwave data near 13Z
indicated that the cyclone had a ragged inner core with no
organized eyewall. During the time that the aircraft has been in the
storm, the eyewall has gotten better defined in the southeastern
semicircle and the radius of maximum winds is getting smaller. The
maximum 700-mb flight-level winds reported by the aircraft has been
82 kt, and the central pressure is currently near 978 mb. Based
mainly on the aircraft data, the initial intensity is held at 75
kt. It should be noted that shear analyses show that the hurricane
is still be affected by about 20 kt of northeasterly vertical wind
shear.
The initial motion is still northwestward or 315/7 kt. Rachel
continues to move along the southwestern side of a mid-tropospheric
ridge over northern and central Mexico. This ridge is weakening
due to the effects of a large mid- to upper-level trough seen in
water vapor imagery over the southwestern United States and
northwestern Mexico. As this trough moves northeastward and
weakens during the next couple of days, this should allow another
ridge to build to the north of the tropical cyclone. As a result,
Rachel is forecast to turn west-northwest and pass well south of
the Baja California Peninsula before continuing westward away from
land. The new forecast track is a little to the north of the
previous track for the first 60 h, and thereafter is similar to the
previous track.
Environmental conditions appear favorable for strengthening through
at least 48 h, and rapid strengthening is a possibility if the
tighter inner core that Rachel is trying to develop maintains
itself. Thus, the early portion of the intensity forecast keeps the
same rate of intensification to a major hurricane as the previous
forecasts. However, there remains two possible negative influences
including the ongoing shear and Rachel crossing a track of cooler
water left by Polo. Later on the forecast period, decreasing sea
surface temperatures under the forecast track and dry air
entrainment could cause some weakening. The new intensity forecast
is again an update of the previous forecast, and it lies near the
upper edge of the intensity guidance.
Key Messages:
1. Although the core of Rachel is forecast to remain offshore of
Mexico, wind gusts of tropical-storm force are possible along
portions of the coast of southwestern Mexico through tonight.
2. Outer bands from Rachel will continue to produce locally heavy
rainfall across portions of coastal southwest Mexico. This rainfall
may produce life-threatening flooding and mudslides, especially in
areas of steep terrain.
3. Large waves could produce life-threatening surf and rip current
conditions along the southwestern and west-central coast of Mexico
and the southern Baja California Peninsula during the next several
days.
FORECAST POSITIONS AND MAX WINDS
INIT 30/2100Z 18.8N 108.0W 75 KT 85 MPH
12H 01/0600Z 19.1N 108.6W 90 KT 105 MPH
24H 01/1800Z 19.6N 109.2W 100 KT 115 MPH
36H 02/0600Z 19.9N 109.9W 105 KT 120 MPH
48H 02/1800Z 20.0N 110.8W 105 KT 120 MPH
60H 03/0600Z 20.1N 111.8W 100 KT 115 MPH
72H 03/1800Z 20.3N 113.0W 90 KT 105 MPH
96H 04/1800Z 20.5N 115.3W 90 KT 105 MPH
120H 05/1800Z 20.6N 117.8W 85 KT 100 MPH
$$
Forecaster Beven
NNNN
ZCZC MIATCDEP4 ALL
TTAA00 KNHC DDHHMM
Tropical Depression Nineteen-E Discussion Number 6
NWS National Hurricane Center Miami FL EP192026
200 PM PDT Wed Sep 30 2026
Although the depression has a well-defined circulation, convection
has fallen apart this afternoon, with the low-level circulation
almost totally exposed. Satellite intensity estimates are falling
again, so the initial wind speed is set to 25 kt using a blend of
the objective and subjective values.
The depression is moving eastward at about 12 kt. This general
motion is expected during the next couple of days as the depression
moves south of the remnants of Odalys and eventually starts to move
on the southwestern side of Rachel's much larger circulation. The
track forecast is shifted a little to the north, mostly based on
a more precise initial positions from visible satellite images.
Little change in intensity is shown for the depression due to
moderate shear and plentiful dry mid-level air, somewhat countered
by warming SSTs. The shear is forecast to increase somewhat along
with a bit drier mid-level environment, which is likely to bring an
end to any organized convection. Thus, the depression is forecast
to become a remnant low in about 24 hours, similar to the latest
global models simulated satellite data. I will just mention some
of the guidance is showing some re-intensification on Thursday, but
that is deemed unlikely due to the unfavorable environmental
factors listed above.
FORECAST POSITIONS AND MAX WINDS
INIT 30/2100Z 14.9N 127.0W 25 KT 30 MPH
12H 01/0600Z 15.2N 125.3W 25 KT 30 MPH
24H 01/1800Z 15.3N 123.1W 25 KT 30 MPH...POST-TROP/REMNT LOW
36H 02/0600Z 15.3N 120.5W 25 KT 30 MPH...POST-TROP/REMNT LOW
48H 02/1800Z...DISSIPATED
$$
Forecaster Blake
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 300900
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 25W (SURIGAE) WARNING NR
029//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 31.2N 138.3E
INITIAL INTENSITY: 35 KTS
GEOGRAPHIC REFERENCE: 256 NM SOUTH-SOUTHWEST OF YOKOSUKA, JAPAN
MOVEMENT PAST 6 HOURS: NORTHEASTWARD AT 13 KTS
SIGNIFICANT WAVE HEIGHT: 16 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS A
FULLY EXPOSED LOW-LEVEL CIRCULATION, WITH THE ONLY REMAINING
ASSOCIATED PATCH OF DEEP CONVECTION SHEARED TO THE EASTERN
PERIPHERY. THE INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE
BASED ON THE EXPOSED CENTER AND RECENT SATELLITE FIXES FROM MULTIPLE
AGENCIES. THE INITIAL INTENSITY OF 35 KTS IS ASSESSED WITH HIGH
CONFIDENCE BASED ON A CONSENSUS OF AVAILABLE SUBJECTIVE DVORAK AND
AUTOMATED INTENSITY ESTIMATES LISTED BELOW, WITH FURTHER SUPPORT
FROM A 300347Z OCEANSAT-3 PASS.
INITIAL WIND RADII BASIS: PERSISTENCE AND SCATTEROMETER DATA FROM A
300347Z OCEANSAT-3 PASS
CURRENT STEERING MECHANISM: LOW TO MID-LEVEL FLOW ASSOCIATED WITH A
DEEP-LAYER SUBTROPICAL RIDGE (STR) TO THE SOUTHEAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.5 - 35 KTS
RJTD: T3.0 - 45 KTS
RCTP: T2.0 - 30 KTS
CIMSS SATCON: 35 KTS AT 300407Z
CIMSS ADT: 25 KTS AT 300540Z
CIMSS AIDT: 34 KTS AT 300540Z
CIMSS D-MINT: 31 KTS AT 300408Z
CIMSS D-PRINT: 29 KTS AT 300740Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: HIGHLY UNFAVORABLE
VWS: 25-30 KTS
SST: 28-29 CELSIUS
OUTFLOW: MODERATE EASTWARD
OTHER FACTORS: DRY AIR ENTRAINMENT
ANALYSIS CONFIDENCE:
INITIAL POSITION: HIGH
INITIAL INTENSITY: HIGH
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 25W WILL ACCELERATE NORTHEASTWARD AND
COMPLETE EXTRATROPICAL TRANSITION DURING THE FORECAST PERIOD. THE
SYSTEM IS EXPECTED TO BEGIN MERGING WITH AN UPPER-LEVEL SHORTWAVE
TROUGH BY TAU 12, WHICH WILL INITIATE THE TRANSITION PROCESS. BY
TAU 24 THE SYSTEM WILL FULLY MERGE WITH THE TROUGH AND BECOME
EMBEDDED IN THE MID-LATITUDE WESTERLY FLOW PATTERN. TS 25W IS
EXPECTED TO MAINTAIN INTENSITY DUE TO STRONG DIVERGENT FLOW ALOFT
AND PASSAGE OVER WARM WATER FOR THE NEXT 12 HOURS AND HOLD STEADY
OR INCREASE SLIGHTLY IN INTENSITY THEREAFTER DUE TO FAVORABLE
BAROCLINIC SUPPORT.
MODEL DISCUSSION: NUMERICAL MODEL TRACK AND INTENSITY FORECAST
GUIDANCE ARE IN VERY TIGHT AGREEMENT ON THE CURRENT CYCLE, BUT HAVE
SHIFTED SLIGHTLY POLEWARD FROM THE PREVIOUS CYCLE. THE TRACK
FORECAST IS CORRESPONDINGLY NUDGED POLEWARD AND IS CONSISTENT WITH
MULTI-MODEL CONSENSUS GUIDANCE WITH HIGH CONFIDENCE. MODELS AGREE
ON A GENERAL STEADY INTENSITY WITH THE POSSIBILITY OF SLIGHT
INTENSIFICATION DURING THE FORECAST PERIOD, AND THE CURRENT
FORECAST STAYS THE COURSE WITH HIGH CONFIDENCE.
FORECAST CONFIDENCE:
TRACK 00-72 HR: HIGH
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.
WDPN32 PGTW 302100
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 26W (CHOI-WAN) WARNING NR
004//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 16.2N 150.0E
INITIAL INTENSITY: 35 KTS
GEOGRAPHIC REFERENCE: 331 NM EAST-NORTHEAST OF ANDERSEN AFB
MOVEMENT PAST 6 HOURS: WEST-NORTHWESTWARD AT 08 KTS
SIGNIFICANT WAVE HEIGHT: 15 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
TROPICAL STORM (TS) 26W IS GRADUALLY INTENSIFYING. ANIMATED
ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS CURVED BANDING
DISPLACED WEST OF A PARTIALLY OBSCURED, ELONGATED LOW-LEVEL
CIRCULATION CENTER (LLCC). THE ASSOCIATED CONVECTION IS
PARTICULARLY DEEP, WITH CLOUD TOP TEMPERATURES AS COLD AS -90
DEGREES CELSIUS, WHILE THE CURVATURE OF THE CONVECTIVE BANDING
CONTINUES TO IMPROVE. A 301448Z AMSR3 PASS INDICATES THAT THE
VORTEX IS TILTED WESTWARD WITH HEIGHT. THIS STRUCTURE IS CONSISTENT
WITH EASTERLY MID-LEVEL SHEAR OF NEAR 20 KTS, WHICH IS PREVENTING
THE SYSTEM FROM BECOMING VERTICALLY ALIGNED. DESPITE THE SHEAR, THE
ENVIRONMENT IS FAVORABLE, CHARACTERIZED BY VERY WARM SEA SURFACE
TEMPERATURES (SST) OF 30 DEGREES CELSIUS AND VERY HIGH OHC NEAR 140
KJ PER CM2, MODERATE RADIAL OUTFLOW ALOFT, AND PLENTIFUL DEEP-LAYER
MOISTURE. THE INITIAL POSITION IS PLACED WITH LOW CONFIDENCE,
HEDGED EAST OF THE MID-LEVEL CIRCULATION CENTER TO ACCOUNT FOR
VORTEX TILT. AN AGED 301015Z ASCAT-B PASS REVEALED A COMPACT PATCH
OF GALE-FORCE WINDS ISOLATED TO THE NORTHWEST QUADRANT, EMBEDDED
WITHIN A MUCH BROADER 20- TO 25-KT WIND FIELD ACROSS THE REMAINING
QUADRANTS. GIVEN THE GAP SINCE THAT PASS AND SUBSEQUENT
CONSOLIDATION, IT REMAINS UNCERTAIN WHETHER THE OBSERVED STRUCTURAL
IMPROVEMENT HAS ONLY EXPANDED THE AREAL FOOTPRINT OF GALES OR ALSO
INCREASED THE MAXIMUM SUSTAINED WINDS. ACCORDINGLY, THE INITIAL
INTENSITY HAS BEEN HELD AT 35 KTS WITH MEDIUM CONFIDENCE, SUPPORTED
BY AIDT AND THE T2.5 DVORAK ESTIMATE FROM PGTW.
INITIAL WIND RADII BASIS: SCATTEROMETER DATA
CURRENT STEERING MECHANISM: SOUTHERN PERIPHERY OF A LOW- TO
MID-LEVEL SUBTROPICAL RIDGE CENTERED FAR TO THE NORTHEAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.5 - 35 KTS
RJTD: T1.5 - 25 KTS
RCTP: T2.0 - 30 KTS
CIMSS ADT: 41 KTS AT 301430Z
CIMSS AIDT: 35 KTS AT 301430Z
CIMSS D-MINT: 26 KTS AT 301540Z
CIMSS D-PRINT: 30 KTS AT 301710Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE
VWS: 15-20 KTS
SST: 30-31 CELSIUS
OUTFLOW: MODERATE RADIAL
ANALYSIS CONFIDENCE:
INITIAL POSITION: LOW
INITIAL INTENSITY: MEDIUM
INITIAL WIND RADII: MEDIUM
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THE FORECAST WIND RADII HAVE BEEN
SIGNIFICANTLY EXPANDED BEYOND TAU 48.
FORECAST DISCUSSION: TS 26W IS MOVING WEST-NORTHWESTWARD ALONG THE
SOUTHERN PERIPHERY OF A LOW- TO MID-LEVEL STR CENTERED NEAR 31N
169E. THIS MOTION WILL CONTINUE FOR THE NEXT 24 HOURS. AFTER THAT
TIME, A PROGRESSIVE SHORTWAVE TROUGH RACING DOWNSTREAM OF NORTHERN
HONSHU AND HOKKAIDO WILL ERODE THE STR. THE PRIMARY STEERING
INFLUENCE WILL WEAKEN MARKEDLY, AND TS 26W WILL BECOME NEARLY
STATIONARY. THE SYSTEM WILL THEN TURN POLEWARD NEAR TAU 36 AS THE
DEEP-LAYER STR REORIENTS, AND THE WESTERN FLANK OF THE RIDGE
BECOMES THE DOMINANT STEERING MECHANISM. TOWARD THE END OF THE
FORECAST PERIOD, THE TRAJECTORY WILL NUDGE WESTWARD AS THE RIDGE
BUILDS SLIGHTLY WESTWARD. THE FORECAST CALLS FOR GRADUAL TO STEADY
INTENSIFICATION FOR THE FIRST 24 HOURS, GIVING TIME FOR THE STORM
TO BECOME VERTICALLY ALIGNED AND MORE SYMMETRIC. AFTER TAU 24, THE
PERSISTENT MID-LEVEL SHEAR WILL EASE. COUPLED WITH VERY WARM SST
AND VERY HIGH OHC, THE LOWER SHEAR AND RICH DEEP-LAYER MOISTURE
WILL ENABLE TS 26W TO UNDERGO SIGNIFICANT INTENSIFICATION. BETWEEN
TAU 72 AND TAU 96, THE SYSTEM WILL MOVE OVER LOWER OHC, WHICH WILL
LIMIT CONTIN…
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: ESE (120°), 15.5 kt | Gust: 19.4 kt
Pressure: 29.87 steady | Air Temp: 85.3 °F
Water Temp: 86.9 °F | Dew Point: 77.7 °F
Swell: 0.0 ft | Wind Wave: 2.3 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.