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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 Marie Discussion Number 15
NWS National Hurricane Center Miami FL EP132026
200 PM PDT Fri Sep 04 2026
Marie is contending with dry air today, which is likely inhibiting
significant strengthening. A broad region of dry air persists
immediately west of the hurricane, and recent infrared satellite
imagery shows a dry slot wrapping from the southwest to the
northeast around the center. This dry-air intrusion has
substantially weakened the deep convection that was previously
concentrated north and east of the eye. However, recent objective
and subjective Dvorak intensity estimates range from 73-90 kt. The
initial intensity is maintained at 85 kt for this advisory.
The initial motion is 285/7 kt, with the hurricane moving along the
southeastern periphery of a weak mid-level ridge centered between
Marie and Hurricane Karina well to the west. A strong closed low
moving into the Pacific Northwest today is expected to weaken this
ridge and induce a turn toward the northwest tonight through this
weekend. Through 72 h, the updated track forecast lies near the
middle of the guidance envelope, and is closest to the Google
DeepMind and HCCA. As Marie weakens early next week, the cyclone is
expected to become increasingly steered by the low- to mid-level
environmental flow. An eventual turn toward the north is possible by
midweek as a new trough approaches the western U.S. Beyond 72 h, the
forecast has been nudged to the right of the previous advisory, and
Marie is expected to remain well offshore of the western United
States.
Marie is currently moving over warm waters of 27-28 C and through an
environment of low wind shear, but dry mid-level air continues to
take its toll on the hurricane. Increasingly unfavorable upper-level
winds are expected to support very slow weakening over the next day
or two, followed by more pronounced weakening early next week as
Marie moves over cooler waters and into an increasingly dry
mid-level environment. Simulated satellite imagery from the ECMWF
and GFS suggests that Marie may struggle to maintain organized
convection by the middle of next week. Accordingly, the latest NHC
intensity forecast calls for Marie to degenerate into a
post-tropical remnant low by day 5, with dissipation around day 6.
FORECAST POSITIONS AND MAX WINDS
INIT 04/2100Z 20.2N 118.6W 85 KT 100 MPH
12H 05/0600Z 20.9N 119.4W 80 KT 90 MPH
24H 05/1800Z 21.8N 120.5W 75 KT 85 MPH
36H 06/0600Z 22.6N 121.5W 70 KT 80 MPH
48H 06/1800Z 23.3N 122.3W 65 KT 75 MPH
60H 07/0600Z 24.0N 123.3W 60 KT 70 MPH
72H 07/1800Z 24.7N 124.5W 55 KT 65 MPH
96H 08/1800Z 26.6N 126.7W 40 KT 45 MPH
120H 09/1800Z 29.5N 128.2W 30 KT 35 MPH...POST-TROP/REMNT LOW
$$
Forecaster Adams
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 042100
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 22W (KROVANH) WARNING NR
015//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 28.4N 127.1E
INITIAL INTENSITY: 45 KTS
GEOGRAPHIC REFERENCE: 120 NM NORTH-NORTHWEST OF KADENA AB
MOVEMENT PAST 6 HOURS: SOUTH-SOUTHWESTWARD AT 06 KTS
SIGNIFICANT WAVE HEIGHT: 20 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS TROPICAL
STORM (TS) 22W WITH A PARTIALLY EXPOSED LOW-LEVEL CIRCULATION
CENTER (LLCC) OBSCURED BY PERSISTENT CONVECTION IN THE NORTHEAST
QUADRANT. THE SATELLITE PRESENTATION IN THE REMAINING QUADRANTS IS
THAT OF STABLE LOW CLOUDS WRAPPING INTO THE SLIGHTLY ELONGATED
LLCC. A ROBUST POLEWARD OUTFLOW CHANNEL SUPPORTED BY A PASSING JET
STREAK IS STILL EVIDENT IN ANIMATED WATER VAPOR IMAGERY, WHICH
CONTINUES TO SUPPORT CONVECTION IN THE NORTHEAST QUADRANT. A
041452Z OCEANSAT-3 SCATTEROMETRY IMAGE REVEALED THE HIGHLY
ASYMMETRIC WIND FIELD AROUND THE CENTER OF THE SYSTEM, WITH A SWATH
OF 45 KT WINDS IN THE NORTHERN SEMICIRCLE WHERE THE PRESSURE
GRADIENT HAS ENHANCED THE WIND SPEEDS. THE INITIAL POSITION IS
PLACED WITH MEDIUM CONFIDENCE BASED ON A COMBINATION OF THE POORLY
DEFINED LLCC IN ANIMATED EIR AND EXTRAPOLATION FROM THE CENTER IN
THE SCATTEROMETRY IMAGE. THE INITIAL INTENSITY OF 45 KTS IS
ASSESSED WITH MEDIUM CONFIDENCE BASED ON THE SCATTEROMETRY WINDS,
HOWEVER, THE PRESSURE GRADIENT IS LIKELY RELAXING AS THE SYSTEM
MOVES EQUATORWARD AND THEREFORE GRADUALLY REDUCING THE WIND SPEEDS
IN THE NORTHERN SEMICIRCLE. THE ENVIRONMENT IS CHARACTERIZED AS
MARGINAL, WITH WARM SEA SURFACE TEMPERATURES AND GOOD OUTFLOW ALOFT
BEING OFFSET BY LOW-MODERATE VERTICAL WIND SHEAR (VWS) AND THE DRY
AIR MASS SURROUNDING THE VORTEX IN ALL BUT THE NORTHEAST QUADRANT.
INITIAL WIND RADII BASIS: SCATTEROMETER DATA
CURRENT STEERING MECHANISM: SOUTHEASTERN FLANK OF A RIDGE
POSITIONED OVER NORTHEAST CHINA
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.5 - 35 KTS
RJTD: T2.0 - 30 KTS
RCTP: T2.5 - 35 KTS
KNES: T2.0 - 30 KTS
CIMSS SATCON: 37 KTS AT 041704Z
CIMSS ADT: 34 KTS AT 041750Z
CIMSS AIDT: 38 KTS AT 041750Z
CIMSS D-MINT: 35 KTS AT 041705Z
CIMSS D-PRINT: 30 KTS AT 041820Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL
VWS: 15-20 KTS
SST: 29-30 CELSIUS
OUTFLOW: STRONG POLEWARD
OTHER FACTORS: SURROUNDING STABLE AND DRY AIR MASS
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: TS 22W (KROVANH) HAS TRACKED SLOWLY
SOUTHWESTWARD OVER THE PAST 6 HOURS AS THE DEEP SUBTROPICAL RIDGE
(STR) OVER EASTERN CHINA HAS STARTED TO EXERT A STEERING INFLUENCE.
THE TRACK IS FORECAST TO CONTINUE GENERALLY SOUTHWARD AS 22W
APPROACHES OKINAWA, THEN CONTINUE AROUND A COUNTER-CLOCKWISE ARC
TOWARD MINAMI-DAITOJIMA THROUGH TAU 60. A STR BUILDING IN FROM THE
NORTHEAST IS EXPECTED TO INDUCE A POLEWARD TURN AND ACCELERATION
AFTER TAU 60. THERE REMAINS A FAIR AMOUNT OF UNCERTAINTY IN THE
TRACK DUE TO THE DYNAMIC NATURE OF THE STEERING ENVIRONMENT,
ESPECIALLY IN THE LATER TAUS. IN TERMS OF INTENSITY, A GRADUAL
DECREASE IS FORECAST THROUGHOUT THE ENTIRE PERIOD; FIRST AS A
RESULT OF THE SYSTEM'S MOTION AWAY FROM THE ENHANCED GRADIENT TO
ITS NORTH, THEN AS IT LOSES UPPER-LEVEL EXHAUST, CONTINUES TO
INGEST DRY AIR, AND REMAINS IN AN UNFAVORABLE SHEAR ENVIRONMENT.
MODEL DISCUSSION: MODEL TRACK GUIDANCE IS IN AGREEMENT ONLY INSOFAR
AS THE GENERAL SHAPE OF THE ARCING TRACK AND THE EVENTUAL POLEWARD
TURN. THE JTWC TRACK FORECAST REMAINS AMONG THE MEAN TRACK OF THE
GUIDANCE THROUGHOUT THE FORECAST WITH M…
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 042100
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL DEPRESSION 23W (TWENTYTHREE)
WARNING NR 002//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 24.0N 137.1E
INITIAL INTENSITY: 30 KTS
GEOGRAPHIC REFERENCE: 234 NM WEST OF IWO TO
MOVEMENT PAST 6 HOURS: NORTH-NORTHWESTWARD AT 17 KTS
SIGNIFICANT WAVE HEIGHT: 15 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS TROPICAL
DEPRESSION (TD) 23W A LACK OF PERSISTENT CONVECTION AROUND THE
POORLY ORGANIZED LOW-LEVEL CIRCULATION, THE REMNANTS OF WHICH ARE
NOW FULLY EXPOSED. THERE IS AN APPARENT MESOVORTEX ROTATING WITHIN
THE BROADER CYCLONIC WIND FIELD THAT MAY REPRESENT THE PREVIOUSLY
OBSERVED COMPACT ROTATION. A 041510Z OCEANSAT-3 SCATTEROMETRY IMAGE
REVEALED THE MESOVORTEX ON THE EASTERN EDGE OF THE BROADER
CIRCULATION AND DEPICTED WIND SPEEDS OF 30-35 KTS IN THE SOUTHEAST
QUADRANT. THE INITIAL POSITION IS PLACED WITH LOW CONFIDENCE BASED
ON THE AMBIGUOUS STRUCTURE OF THE LOW-LEVEL CIRCULATION. THE
INITIAL INTENSITY OF 30 KTS IS ASSESSED WITH HIGH CONFIDENCE BASED
ON THE SCATTEROMETRY DATA. THE ENVIRONMENT IS CHARACTERIZED AS
MARGINAL FOR DEVELOPMENT, WITH WARM SEA SURFACE TEMPERATURES,
LOW-MODERATE VERTICAL WIND SHEAR (VWS), AND WEAK OUTFLOW ALOFT.
INITIAL WIND RADII BASIS: NOT APPLICABLE (THERE ARE NO INITIAL WIND
RADII).
CURRENT STEERING MECHANISM: WESTERN FLANK OF A SUBTROPICAL RIDGE
CENTERED TO THE EAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T1.5 - 25 KTS
KNES: T1.5 - 25 KTS
CIMSS ADT: 41 KTS AT 041750Z
CIMSS AIDT: 41 KTS AT 041750Z
CIMSS D-PRINT: 27 KTS AT 041920Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL
VWS: 15-20 KTS
SST: 29-30 CELSIUS
OUTFLOW: WEAK EQUATORWARD
ANALYSIS CONFIDENCE:
INITIAL POSITION: LOW
INITIAL INTENSITY: HIGH
INITIAL WIND RADII: NOT APPLICABLE
3. FORECAST REASONING.
SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO
THE FORECAST FROM THE PREVIOUS WARNING.
FORECAST DISCUSSION: TD 23W HAS TRACKED NORTH-NORTHWESTWARD OVER
THE PAST 6 HOURS UNDER THE STEERING INFLUENCE OF THE STR TO THE
EAST. THE TRACK IS FORECAST TO CONTINUE NORTH-NORTHWESTWARD TOWARD
KYUSHU AT A RELATIVELY QUICK PACE FOR THE ENTIRE FORECAST PERIOD.
THERE IS NOT EXPECTED TO BE ANY INFLUENTIAL INTERACTION WITH
TROPICAL STORM 22W BASED ON THE LATEST GUIDANCE AND LACK OF
DEVELOPMENT OF 23W. THE INTENSITY IS FORECAST TO STEADILY DECREASE
AS THE SYSTEM EXITS A REGION OF ENHANCED SOUTHWESTERLY FLOW INTO AN
UNFAVORABLE REGION FOR CONVECTIVE DEVELOPMENT.
MODEL DISCUSSION: AVAILABLE MODEL TRACK GUIDANCE IS IN GOOD
AGREEMENT ABOUT THE TRACK SPEED AND DIRECTION FOR THE ENTIRE
FORECAST PERIOD. THE JTWC TRACK FORECAST IS PLACED CLOSE TO THE
MULTI-MODEL CONSENSUS WITH HIGH CONFIDENCE. MODEL INTENSITY
GUIDANCE FALLS WITHIN A 5 KT ENVELOPE AND DEPICTS A GRADUAL
WEAKENING TREND, WITH THE EXCEPTION OF GFS, WHICH DEPICTS A BRIEF
SPIKE TO 35 KTS. THE JTWC INTENSITY FORECAST FOLLOWS THE
MULTI-MODEL CONSENSUS WITH HIGH CONFIDENCE.
FORECAST CONFIDENCE:
TRACK 00-72 HR: HIGH
INTENSITY 00-72 HR: HIGH//
NNNN
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 (210°), 5.8 kt | Gust: 7.8 kt
Pressure: 29.92 steady | Air Temp: 86.4 °F
Water Temp: 88.3 °F | Dew Point: 80.1 °F
Swell: 1.0 ft | Wind Wave: 0.3 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.