🚨 Montgomery: None 🚨 Susquehanna; Northern Wayne; Pike; Southern Wayne: Frost Advisory issued October 6 at 1:13PM EDT until October 7 at 9:00AM EDT by NWS Binghamton NY 🚨 Central Interior Cumberland; Androscoggin: Freeze Warning issued October 6 at 1:12PM EDT until October 7 at 8:00AM EDT by NWS Gray ME 🚨 Kennebec; Interior Waldo; Coastal York; Coastal Cumberland; Sagadahoc; Lincoln; Knox; Coastal Waldo; Strafford; Eastern Hillsborough; Interior Rockingham: Frost Advisory issued October 6 at 1:12PM EDT until October 7 at 8:00AM EDT by NWS Gray ME 🚨 Union; Snyder; Montour; Northumberland; Columbia; Schuylkill: Frost Advisory issued October 6 at 1:06PM EDT until October 7 at 9:00AM EDT by NWS State College PA 🚨 Western Franklin; Eastern Franklin; Western Hampshire; Eastern Hampshire: Freeze Warning issued October 6 at 12:56PM EDT until October 7 at 9:00AM EDT by NWS Boston/Norton MA 🚨 Western Essex; Southern Worcester; Northwest Providence; Western Kent; Washington: Frost Advisory issued October 6 at 12:56PM EDT until October 7 at 9:00AM EDT by NWS Boston/Norton MA 🚨 Hartford; Tolland; Windham; Northern Worcester; Central Middlesex County; Western Hampden; Eastern Hampden; Western Norfolk; Northern Bristol; Western Plymouth; Southern Bristol; Southern Plymouth; Northwest Middlesex County: Frost Advisory issued October 6 at 12:56PM EDT until October 7 at 9:00AM EDT by NWS Boston/Norton MA 🚨 Parker Valley; Gila River Valley; Palo Verde Valley; Chuckwalla Valley: Extreme Heat Warning issued October 6 at 9:47AM MST until October 8 at 8:00PM MST by NWS Phoenix AZ 🚨 Imperial County West; Imperial Valley: Extreme Heat Warning issued October 6 at 9:47AM MST until October 9 at 8:00PM MST by NWS Phoenix AZ
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 38
NWS National Hurricane Center Miami FL EP182026
800 AM PDT Tue Oct 06 2026
Satellite imagery this morning shows that Rachel's inner core has
degraded, with the system now featuring a large, ragged eye. The
deepest cold convection is confined mainly to the southern eyewall
as the cyclone continues to encounter northeasterly wind shear and a
drier mid-level environment. The latest subjective Dvorak intensity
estimate from TAFB held steady at T4.5/77 kt, while objective
intensity estimates from UW-CIMSS range between 77 and 82 kt. Based
on these satellite trends and intensity estimates, the initial
intensity is held at 75 kt for this advisory.
The initial motion is westward, or 275/7 kt. A general west to
west-northwestward motion is expected during the next several days
while the system is steered by a subtropical ridge to its north. In
a few days, a mid- to upper-level trough is forecast to approach the
west coast of the United States, which will weaken the ridge. This
should cause Rachel to slow down, make a sharp turn toward the
northeast, and increase in forward speed. The latest NHC track
forecast is very similar to the previous advisory and remains in
good agreement with the HCCA and Google DeepMind aids.
The surrounding environment is starting to take its toll on Rachel,
with a drier, more stable airmass and moderate northeasterly wind
shear. Sea surface temperatures along the forecast track will also
cool below 26C in about a day or so, which should induce a steady
weakening trend. Simulated infrared imagery from the global models
shows Rachel struggling to produce deep, organized convection later
this week. As a result, the latest NHC forecast now indicates that
Rachel will become a post-tropical cyclone by 96 h. The official NHC
intensity forecast is similar to the previous one, with gradual
weakening near the upper end of the guidance suite in the short
term, and then a faster weakening trend toward the consensus aids at
the end of the period.
FORECAST POSITIONS AND MAX WINDS
INIT 06/1500Z 20.5N 119.5W 75 KT 85 MPH
12H 07/0000Z 20.6N 120.4W 75 KT 85 MPH
24H 07/1200Z 21.0N 121.7W 70 KT 80 MPH
36H 08/0000Z 21.5N 123.0W 60 KT 70 MPH
48H 08/1200Z 22.0N 124.3W 55 KT 65 MPH
60H 09/0000Z 22.4N 125.4W 50 KT 60 MPH
72H 09/1200Z 22.8N 125.8W 45 KT 50 MPH
96H 10/1200Z 24.2N 123.5W 40 KT 45 MPH...POST-TROPICAL
120H 11/1200Z 27.7N 119.3W 35 KT 40 MPH...POST-TROPICAL
$$
Forecaster Kelly
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 061500
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TYPHOON 15E (NOLO) WARNING NR 064//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 25.4N 169.1E
INITIAL INTENSITY: 100 KTS
GEOGRAPHIC REFERENCE: 391 NM NORTH-NORTHEAST OF WAKE ISLAND
MOVEMENT PAST 6 HOURS: WESTWARD AT 18 KTS
SIGNIFICANT WAVE HEIGHT: 42 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTED THE
SUDDEN AND DRAMATIC COLLAPSE OF TYPHOON (TY) 15E'S CENTRAL EYE JUST
A FEW HOURS AGO. ADDITIONALLY, THE POLEWARD OUTFLOW CHANNEL IS
COMPLETELY SUPPRESSED BY THE MODERATE TO HIGH (20-25 KTS) NORTHERLY
VERTICAL WIND SHEAR (VWS). THE EQUATORWARD OUTFLOW CHANNEL REMAINS
AVAILABLE, BUT INCREASINGLY WEAK. THE 061015Z ASCAT DATA REVEALS
A TIGHT INNER CORE WITH AN ASYMMETRIC WIND FIELD. A THIN BAND OF
STORM- AND TYPHOON-FORCE WINDS IS PRESENT ALONG THE SOUTHWESTERN
SEMICIRCLE, CONTRASTED BY THE EXPANSIVE RANGE OF ELEVATED WINDS
WITHIN THE NORTHEAST SEMICIRCLE. ENVIRONMENTAL ANALYSIS REVEALS A
MARGINALLY UNFAVORABLE ENVIRONMENT, CHARACTERIZED BY MODERATE TO
HIGH VWS, SIGNIFICANT DRY AIR ENTRAINMENT, MARGINAL (0-20 KJ PER CM
SQUARED) OCEAN HEAT CONTENT (OHC), AND POOR OUTFLOW, OFFSET
SLIGHTLY BY WARM (27-28 C) SEA SURFACE TEMPERATURES (SST). THE
INITIAL POSITION IS PLACED WITH MEDIUM CONFIDENCE BASED ON THE
COLLAPSED EYE IN ANIMATED EIR AND EXTRAPOLATION FROM THE 061015Z
ASCAT DATA. THE INITIAL INTENSITY OF 100 KTS IS ASSESSED WITH
MEDIUM CONFIDENCE BASED ON THE AGENCY DVORAK FIXES AND THE CIMSS
AUTOMATED INTENSITY ESTIMATES LISTED BELOW.
INITIAL WIND RADII BASIS: ADJUSTED WIND RADII USING THE 061015Z
ASCAT DATA
CURRENT STEERING MECHANISM: DEEP-LAYER SUBTROPICAL RIDGE (STR)
CENTERED TO THE NORTHWEST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T5.0 - 90 KTS
RJTD: T5.5 - 102 KTS
RCTP: T5.5 - 102 KTS
PHFO: T5.0 - 90 KTS
CIMSS ADT: 97 KTS AT 061200Z
CIMSS AIDT: 95 KTS AT 061200Z
CIMSS D-PRINT: 90 KTS AT 061200Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINALLY
UNFAVORABLE
VWS: 20-25 KTS
SST: 27-28 CELSIUS
OUTFLOW: WEAK EQUATORWARD
OTHER FACTORS: DRY AIR ENTRAINMENT
ANALYSIS CONFIDENCE:
INITIAL POSITION: MEDIUM
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: TY 15E (NOLO) IS FORECAST TO CONTINUE TRACKING
WESTWARD TO WEST-NORTHWESTWARD WHILE IT REMAINS ON THE EQUATORWARD
PERIPHERY OF THE STR CENTERED TO THE NORTHEAST. BEGINNING AROUND
TAU 48, 15E WILL TURN POLEWARD INTO A WEAK STEERING ENVIRONMENT
CREATED BY A BREAK BETWEEN THE ROBUST STEERING STR AND A BUILDING
LOW- TO MID-LEVEL RIDGE CENTERED OVER JAPAN. DURING THIS PERIOD,
15E IS FORECAST TO SLOW ITS TRANSLATIONAL SPEED. ULTIMATELY, 15E IS
FORECAST TO DRIFT POLEWARD AND RECURVE ABOUT THE STEERING RIDGE
THROUGH THE REMAINDER OF THE FORECAST PERIOD. TRANSITION INTO AN
EXTRATROPICAL CYCLONE WILL BEGIN NO LATER THAN TAU 120.
REGARDING INTENSITY, 15E IS FORECAST TO STEADILY WEAKEN THROUGH TAU
36-48 AS THE ENVIRONMENT REMAINS MARGINALLY UNFAVORABLE. BY ABOUT
TAU 48, VWS IS EXPECTED TO ABATE SLIGHTLY, CONCURRENT WITH THE
POLEWARD OUTFLOW CHANNEL STRENGTHENING AS THE STORM ENTERS THE
WEAKNESS BETWEEN RIDGES. AS A RESULT, 15E IS ANTICIPATED TO
REINTENSIFY SLIGHTLY BETWEEN TAU 60-72. AFTER TAU 72, VWS IS
EXPECTED TO INCREASE, STIFLING THE POLEWARD OUTFLOW CHANNEL AND
FORCING EXCESSIVE AMOUNTS OF DRY AIR INTO THE CORE. THE
ENVIRONMENT WILL CONTINUE TO DETERIORATE AS NOLO TRACKS POLEWARD,
ALONG WITH THE WEAK OUTFLOW, VWS, AND DRY AIR, IT IS EXPECTED TO
CROSS THE 26C ISOTHERM AROUND TAU 96. BETWEEN TAU 96-120, 15E IS
FORECAST TO BEGIN INTERACTION WITH THE UPPER-LEVEL WESTERLIE…
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 061500
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TYPHOON 26W (CHOI-WAN) WARNING NR 027//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 33.7N 147.6E
INITIAL INTENSITY: 80 KTS
GEOGRAPHIC REFERENCE: 402 NM EAST-SOUTHEAST OF YOKOSUKA, JAPAN
MOVEMENT PAST 6 HOURS: NORTH-NORTHEASTWARD AT 23 KTS
SIGNIFICANT WAVE HEIGHT: 42 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS A
GRADUALLY DEGRADING CONVECTIVE STRUCTURE ASSOCIATED WITH TYPHOON
(TY) 26W. WHILE THE CENTRAL DENSE OVERCAST (CDO) AND CLOUD-FILLED
EYE REMAIN EVIDENT, CLOUD TOP TEMPERATURES SURROUNDING THE CORE
CONTINUE TO WARM, AND THE CONVECTIVE STRUCTURE OVER THE SOUTHWEST
QUADRANT IS BEGINNING TO ERODE. A 061010Z GMI PASS REVEALED AN
INTACT LOWER-LEVEL EYEWALL, WHILE INDICATING WEAKENING IN THE
SOUTHERN PORTION OF THE UPPER-LEVEL EYEWALL. THE ENVIRONMENT IS
LARGELY UNFAVORABLE AS THE SYSTEM CROSSES THE 26-DEGREE CELSIUS
ISOTHERM INTO PROGRESSIVELY COOLER WATERS AND ENCOUNTERS HIGH
VERTICAL WIND SHEAR (VWS). THESE DETRIMENTAL CONDITIONS OUTWEIGH
THE FAVORABLE INFLUENCE OF STRONG POLEWARD OUTFLOW ALOFT. THE
INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE
OUTLINE OF THE CLOUD-FILLED EYE IN THE SHORTWAVE INFRARED IMAGERY.
THE INITIAL INTENSITY HAS BEEN LOWERED TO 80 KTS WITH MEDIUM
CONFIDENCE, REFLECTING THE DETERIORATING SATELLITE PRESENTATION.
THIS ASSESSMENT IS SUPPORTED BY THE T4.5 DVORAK CLASSIFICATION FROM
PGTW AND THE DECREASING OBJECTIVE INTENSITY ESTIMATES LISTED BELOW.
INITIAL WIND RADII BASIS: SCATTEROMETER DATA
CURRENT STEERING MECHANISM: NORTHWESTERN PERIPHERY OF A SUBTROPICAL
RIDGE (STR) CENTERED EAST OF HONSHU
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T4.5 - 77 KTS
RJTD: T5.0 - 90 KTS
RCTP: T5.0 - 90 KTS
CIMSS ADT: 63 KTS AT 061140Z
CIMSS AIDT: 67 KTS AT 061140Z
CIMSS D-MINT: 73 KTS AT 061008Z
CIMSS D-PRINT: 81 KTS AT 061210Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: UNFAVORABLE
VWS: 30-40 KTS
SST: 25-27 CELSIUS
OUTFLOW: STRONG POLEWARD
ANALYSIS CONFIDENCE:
INITIAL POSITION: HIGH
INITIAL INTENSITY: MEDIUM
INITIAL WIND RADII: LOW
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THE FORECAST HAS BEEN TRUNCATED FROM
36 HOURS TO 24 HOURS.
FORECAST DISCUSSION: TY 26W IS NOW RACING NORTHEASTWARD AT 23 KTS
ALONG THE NORTHWESTERN PERIPHERY OF THE STR. THE SYSTEM WILL
CONTINUE TO ACCELERATE NORTHEASTWARD THROUGH TAU 24 AS IT BECOMES
INCREASINGLY EMBEDDED IN STRONG DEEP-LAYER WESTERLY FLOW. THE
ENVIRONMENT WILL BECOME INCREASINGLY HOSTILE TO THE TROPICAL
CYCLONE, WITH VWS INCREASING TO 40-50 KTS AND SST DECREASING TO
14-16 DEGREES CELSIUS BY TAU 24. THESE FACTORS WILL CONTINUE TO
ERODE THE INNER CORE, RESULTING IN STEADY WEAKENING. BAROCLINIC
FORCING WILL ALSO INCREASE AS TY 26W INTERACTS WITH A MID-LEVEL
TROUGH EJECTING EASTWARD FROM HONSHU AND BECOMES COUPLED WITH THE
JET STREAM TO THE NORTH. THEREFORE, TY 26W WILL RAPIDLY COMPLETE
EXTRATROPICAL TRANSITION BY TAU 24 WHILE MAINTAINING TYPHOON-FORCE
WINDS. THE EXPANSIVE, POTENT WIND FIELD WILL PRODUCE VERY HIGH
SEAS.
MODEL DISCUSSION: TRACK GUIDANCE REMAINS IN EXCELLENT AGREEMENT,
WITH MINIMAL CROSS-TRACK AND ALONG-TRACK SPREAD. THE JTWC FORECAST
TRACK IS SET WITH HIGH CONFIDENCE NEAR THE MULTI-MODEL CONSENSUS
(CONW) DUE TO THE TIGHT CLUSTERING OF THE GUIDANCE. INTENSITY
GUIDANCE IS ALSO IN VERY GOOD AGREEMENT. ALL AVAILABLE AIDS DEPICT
STEADY WEAKENING THROUGH TAU 24, AND THE JTWC INTENSITY FORECAST IS
SET SLIGHTLY ABOVE THE CONSENSUS AT TAU 24, NEAR THE GFS SOLUTION.
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.
WDPN33 PGTW 061500
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 27W (KOGUMA) WARNING NR
007//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 14.0N 165.8E
INITIAL INTENSITY: 45 KTS
GEOGRAPHIC REFERENCE: 321 NM SOUTH OF WAKE ISLAND
MOVEMENT PAST 6 HOURS: NORTHWESTWARD AT 08 KTS
SIGNIFICANT WAVE HEIGHT: 17 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS A SMALL
CENTRAL COLD COVER (CCC) COMPLETELY OBSCURING THE LOW-LEVEL
CIRCULATION CENTER (LLCC). THE BURST OF CONVECTION HAS PERSISTED
FOR AT LEAST SIX HOURS, AND CLOUD TOP TEMPERATURES HAVE BEEN AS
COLD AS -92 DEGREES CELSIUS. THE CCC PATTERN IS CONSISTENT WITH
ARRESTED DEVELOPMENT, SUPPORTING THE ASSESSMENT THAT THE INTENSITY
HAS REMAINED NEARLY STEADY WHILE THE PATTERN PERSISTS. A 060649Z
WSF-M MWI PASS INDICATED A VERTICALLY TILTED VORTEX AND A LACK OF A
COHERENT INNER CORE. DESPITE TRAVERSING VERY WARM SEA SURFACE
TEMPERATURES (SST) NEAR 30 DEGREES CELSIUS AND HIGH OCEAN HEAT
CONTENT (OHC), TS 27W CONTINUES TO CONTEND WITH DRY AIR WRAPPING
INTO THE CIRCULATION FROM THE SOUTHWEST AND MODERATE VERTICAL WIND
SHEAR (VWS) OF NEAR 20 KTS. THE INITIAL POSITION IS PLACED WITH
MEDIUM CONFIDENCE BASED ON A TIGHT CLUSTER OF FIXES FROM PGTW AND
PHFO. THE INITIAL INTENSITY HAS BEEN HELD AT 45 KTS WITH MEDIUM
CONFIDENCE, CONSISTENT WITH THE CCC CLOUD PATTERN AND SUPPORTED BY
THE STEADY SUBJECTIVE AND LOWER-END OBJECTIVE ESTIMATES. THE HIGHER
ADT ESTIMATE IS DISCOUNTED DUE TO THE TILTED VORTEX AND LACK OF A
COHERENT INNER CORE. THE HIGH D-MINT ESTIMATE IS BASED ON A
PARTIAL, LOW-RESOLUTION MICROWAVE IMAGE AND IS ALSO DISCOUNTED.
INITIAL WIND RADII BASIS: PERSISTENCE
CURRENT STEERING MECHANISM: SOUTHERN EXTENSION OF A MID-LEVEL
SUBTROPICAL RIDGE (STR) BUILDING WESTWARD
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.5 - 35 KTS
RJTD: T2.5 - 35 KTS
RCTP: T3.0 - 45 KTS
PHFO: T2.5 - 35 KTS
CIMSS ADT: 53 KTS AT 061140Z
CIMSS AIDT: 41 KTS AT 061140Z
CIMSS D-MINT: 62 KTS AT 061045Z
CIMSS D-PRINT: 45 KTS AT 061220Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINALLY FAVORABLE
VWS: 15-20 KTS
SST: 29-30 CELSIUS
OUTFLOW: MODERATE WESTWARD
OTHER FACTORS: DRY AIR ENTRAINMENT
ANALYSIS CONFIDENCE:
INITIAL POSITION: MEDIUM
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 27W WILL CONTINUE ON A NORTHWESTWARD
TRAJECTORY THROUGH TAU 12, STEERED BY THE SOUTHERN EXTENSION OF THE
STR. THEREAFTER, THE SYSTEM WILL TURN WEST-NORTHWESTWARD AS THE
MID-LEVEL RIDGE BUILDS WESTWARD. TOWARD THE END OF THE FORECAST
PERIOD, A TROUGH TRAVELING EASTWARD FROM HONSHU WILL INTERACT WITH
TYPHOON (TY) 15E TO CREATE A WEAKNESS IN THE STR, ALLOWING TS 27W
TO TURN NORTHWESTWARD ON A MORE POLEWARD TRACK. THE EVOLUTION OF
THE TROUGH, TY 15E, AND THE STR INTRODUCES SIGNIFICANT UNCERTAINTY
REGARDING THE DEGREE OF THE POLEWARD TURN LATE IN THE FORECAST
PERIOD. THE FORECAST CALLS FOR LIMITED DEVELOPMENT THROUGH TAU 12
DUE TO THE ONGOING CCC PATTERN, VWS, AND DRY AIR ENTRAINMENT.
DESPITE TRAVERSING VERY WARM SST AND HIGH OHC, THE SYSTEM WILL
INTENSIFY SLOWLY THROUGH TAU 36 AS MODERATE VWS PERSISTS. AFTER TAU
36, EASING SHEAR WILL ALLOW TS 27W TO RAPIDLY INTENSIFY TO A PEAK
OF 110 KTS BY TAU 72. BY TAU 120, THE SYSTEM WILL WEAKEN SLIGHTLY
DUE TO LOWER OHC. TS 27W HAS A COMPACT CIRCULATION AND IS PRONE TO
SIGNIFICANT FLUCTUATIONS IN INTENSITY. IF THE VWS EASES SOONER AND
TS 27W DEVELOPS A COHERENT INNER CORE MORE QUICKLY, THEN RAPID
INTENSIFICATION (RI) COULD COMMENCE EARLIER AND LEAD TO A HIGHER
PEAK INTENSITY THAN FORECAST.
MODEL DISCUSSION: TRACK GUIDANCE …
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: SSW (200°), 5.8 kt | Gust: 7.8 kt
Pressure: 29.88 | Air Temp: 85.3 °F
Water Temp: 86.4 °F | Dew Point: 79.7 °F
Swell: 1.0 ft | Wind Wave: 0.7 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.