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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 MIATCDEP1 ALL
TTAA00 KNHC DDHHMM
Hurricane Karina Discussion Number 30
NWS National Hurricane Center Miami FL EP112026
1100 AM HST Thu Sep 03 2026
Karina's cold cloud tops around the center appear more
asymmetrical on satellite imagery, with dry air wrapping into the
system. The latest subjective Dvorak analysis from TAFB gave an
intensity estimate of 90 kt, while objective estimates from CIMSS
ranged from 90-95 kt. With Dvorak analyses continuing to trend
downward, along with Karina's degraded appearance on satellite
imagery, the initial intensity estimate was decreased to 90 kt.
Karina's initial motion was set slightly more westward at 275/9 kt.
The system continues to be guided by a subtropical ridge to its
north, but is still expected to turn more west-northwestward
into the weekend as an upper-level trough moves in and weakens the
aforementioned ridge. Another complicating factor for Karina's
track is for it to potentially interact with Lowell early next
week, which may pull Karina a bit more westward than the last
advisory had suggested. Global models seem to hint at this
possibility, so the latest official track forecast reflects a
slight westward shift, however Karina is not expected to be a
threat to the main Hawaiian Islands.
The environment surrounding Karina is becoming increasingly drier
based on latest SHIPS guidance, which should induce weakening
in the short term. Marginal SSTs and increasing vertical
wind shear are forecast to cause additional weakening over the
weekend. Karina is expected to become a post-tropical system by
Monday, before dissipating thereafter. The official NHC intensity
forecast further hastens the rate of weakening, generally falling
close to the consensus aids.
FORECAST POSITIONS AND MAX WINDS
INIT 03/2100Z 19.8N 137.6W 90 KT 105 MPH
12H 04/0600Z 20.1N 139.0W 80 KT 90 MPH
24H 04/1800Z 20.5N 140.7W 70 KT 80 MPH
36H 05/0600Z 21.0N 142.1W 65 KT 75 MPH
48H 05/1800Z 21.8N 143.3W 60 KT 70 MPH
60H 06/0600Z 22.5N 144.2W 55 KT 65 MPH
72H 06/1800Z 23.3N 145.5W 45 KT 50 MPH
96H 07/1800Z 24.7N 148.4W 35 KT 40 MPH...POST-TROPICAL
120H 08/1800Z...DISSIPATED
$$
Forecaster Evans/Brown
NNNN
ZCZC MIATCDEP3 ALL
TTAA00 KNHC DDHHMM
Hurricane Marie Discussion Number 11
NWS National Hurricane Center Miami FL EP132026
200 PM PDT Thu Sep 03 2026
The convection surrounding the center of Hurricane Marie has
fluctuated today, with some mid-level dry air now appearing to wrap
around its center. An earlier WSFM microwave pass depicted a compact
center of circulation, but north-northeasterly wind shear has
resulted in less-definition immediately north and east of the core.
The latest Dvorak intensity estimate from TAFB was 4.5/77 kt, while
objective intensity estimates have decreased a little from this
morning, and currently range from 66-81 kt. Recent wind observations
from the Mexican Navy Weather Station on Clarion Island indicated
sustained winds near 55 kt with a peak wind gust of 76 kt. Based on
these observations and the available intensity estimates, the
initial intensity is maintained at 80 kt for this advisory package.
Marie is moving westward at 280/8 kt. A westward to
west-northwestward motion at a slightly slower forward speed is
expected during the next 48-72 h as a ridge of high pressure
prevails to the northwest of the cyclone. Considerable spread
persists within the track guidance beyond 72 h, largely due to
differences in how a trough approaching the western United States
will influence the strength and position of the aforementioned
ridge. A stronger system moving into the western U.S. would erode
the ridge more substantially, resulting in a more northward track,
while a weaker system would allow the ridge to remain stronger and
favor a more west-northwestward track. Little change was made to the
track forecast through 72 h. Beyond that time, the forecast was
shifted to the right of the previous track forecast and is now
closer to the middle of the track guidance. Confidence in the track
forecast remains lower than normal.
Decreasing wind shear, warm sea surface temperatures of 28-29 C and
sufficiently moist mid-level air should support some strengthening
over the next day or so. It is worth noting that the ECMWF and GFS
SHIPS guidance maintain a small potential for rapid intensification
during this period, and because of this, the official NHC intensity
forecast remains near the upper end of the guidance envelope. The
rate at which Marie weakens will be highly dependent on its eventual
track. A more northward track would allow the hurricane to remain in
slightly warmer waters for a longer period, while a more
west-northwestward track would bring Marie over cooler waters and
likely lead to faster weakening. The official forecast calls for
slow weakening during the second half of the weekend, followed by
more steady weakening early next week.
FORECAST POSITIONS AND MAX WINDS
INIT 03/2100Z 19.3N 115.5W 80 KT 90 MPH
12H 04/0600Z 19.6N 116.6W 85 KT 100 MPH
24H 04/1800Z 20.2N 117.9W 85 KT 100 MPH
36H 05/0600Z 20.9N 119.2W 85 KT 100 MPH
48H 05/1800Z 21.7N 120.3W 80 KT 90 MPH
60H 06/0600Z 22.4N 121.3W 75 KT 85 MPH
72H 06/1800Z 22.8N 122.5W 70 KT 80 MPH
96H 07/1800Z 23.6N 125.6W 60 KT 70 MPH
120H 08/1800Z 25.0N 128.7W 50 KT 60 MPH
$$
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 032100
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 22W (KROVANH) WARNING NR
011//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 29.0N 128.2E
INITIAL INTENSITY: 40 KTS
GEOGRAPHIC REFERENCE: 151 NM NORTH OF KADENA AB
MOVEMENT PAST 6 HOURS: NORTH-NORTHWESTWARD AT 12 KTS
SIGNIFICANT WAVE HEIGHT: 20 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS A STILL
EXPOSED LOW-LEVEL CIRCULATION CENTER (LLCC) MOVING NORTHWESTWARD
INTO THE EAST CHINA SEA. DEEP CONVECTION HAS PERSISTED EAST OF THE
LLCC, SIGNIFICANTLY DISPLACED DUE TO INCREASING WESTERLY VERTICAL
SHEAR OF 25-30 KT. MODERATE UPPER-LEVEL OUTFLOW EASTWARD AND
TURNING EQUATORWARD IS OBSERVED. A DEEP-LAYER DRY AIRMASS CONTINUES
TO ENVELOPE THE WESTERN SEMICIRCLE. SURFACE SUSTAINED WIND
OBSERVATIONS FROM THE RYUKYU ISLANDS HAVE OCCASIONALLY SPIKED INTO
THE 30-35 KT RANGE IN RECENT HOURS. THE INITIAL INTENSITY OF 22W IS
HELD AT 40 KT BASED ON A BLEND OF SURFACE OBSERVATIONS, OBJECTIVE
SATELLITE INTENSITY ESTIMATES, AND PERSISTENCE OF THE SATELLITE
PRESENTATION RELATIVE TO THE PAST 12 HOURS.
INITIAL WIND RADII BASIS: PERSISTENCE
CURRENT STEERING MECHANISM: SUBTROPICAL RIDGE TO THE EAST
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: 36 KTS AT 031638Z
CIMSS ADT: 41 KTS AT 031740Z
CIMSS AIDT: 37 KTS AT 031740Z
CIMSS D-MINT: 34 KTS AT 031724Z
CIMSS D-PRINT: 38 KTS AT 031740Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL
VWS: 25-30 KTS
SST: 29-30 CELSIUS
OUTFLOW: MODERATE EASTWARD
OTHER FACTORS: DEEP-LAYER DRY AIR MASS IN THE WESTERN SEMICIRCLE
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: TROPICAL STORM 22W (KROVANH) CONTINUES TO
TRACK NORTHWESTWARD INTO THE EAST CHINA SEA. THE MOST RECENT FEW
HOURS OF MOTION SUGGEST THAT THE ANTICIPATED SLOWING PHASE HAS
BEGUN, WHICH WILL CULMINATE IN A NEAR-STALL AND REVERSAL OF THE
TRACK MOTION OVER THE NEXT 24 TO 36 HOURS. LOW- TO MID-LEVEL
RIDGING BUILDING INTO THE YELLOW SEA IS FORECAST TO TURN KROVANH
SOUTHWARD AND THEN SOUTHEASTWARD TOWARD OKINAWA, PASSING BY THE
ISLAND IN AROUND 48 HOURS. THE SLOW COUNTERCLOCKWISE LOOP IS THEN
EXPECTED TO CONTINUE AS THE MONSOON TROUGH LIFTS NORTHWARD AND
CREATES A LARGE-SCALE CYCLONIC CAULDRON SOUTH OF JAPAN. BEYOND 48
HOURS, DYNAMIC MODEL GUIDANCE GENERALLY AGREES THAT 22W WILL
GRADUALLY CURVE EASTWARD AND THEN NORTHEASTWARD IN RESPONSE TO AN
UPPER-LEVEL TROUGH TO THE NORTH OVER THE KOREAN PENINSULA IN 72
HOURS, ULTIMATELY APPROACHING MAINLAND JAPAN AT TAU 120. REGARDING
THE INTENSITY FORECAST, ENVIRONMENTAL CONDITIONS ARE CURRENTLY
BECOMING MORE HOSTILE AS 22W ENCOUNTERS STRONGER WESTERLY SHEAR IN
THE EAST CHINA SEA, WHICH IS EXPECTED TO DEGRADE THE STORM'S
STRUCTURE IN THE NEAR-TERM. A BELT OF COLD ADVECTION SETTING UP
BETWEEN KOREA AND JAPAN IS FORECAST TO SUSTAIN GALES ON THE
NORTHERN SIDE OF THE CIRCULATION, EVENTUALLY WRAPPING INTO THE
WESTERN SEMICIRCLE AS THE STORM TURNS SOUTHWARD. AS 22W PASSES
OKINAWA IN ABOUT 48 HOURS, THE JTWC FORECAST NOW DIPS BELOW
TROPICAL STORM FORCE, AS SIGNIFICANT STIRRING OF THE MID-LATITUDE
AIR MASS INTO THE STORM ENVIRONMENT APPEARS LIKELY TO MUTE
CONVECTIVE ACTIVITY FOR A PERIOD OF TIME, AND DYNAMICAL MODELS
AGREE ON BROADENING AND WEAKENING OF THE CIRCULATION. DURING
KROVANH'S REACCELERATION NORTHEASTWARD AT THE END OF THE FORECAST,
SOME REINTENSIFICATION IS POSSIBLE SHOULD A WELL-DEFINED
CIRCULATION PERSIST AND REACQUIRE DEEP CONVECTION. WHIL…
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: NE (50°), 3.9 kt | Gust: 3.9 kt
Pressure: 29.91 | Air Temp: 85.6 °F
Water Temp: 88.9 °F | Dew Point: 79.0 °F
Swell: | Wind Wave:
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.