🚨 Graham, AZ; Greenlee, AZ: Severe Thunderstorm Warning issued October 21 at 5:32PM MST until October 21 at 6:00PM MST by NWS Tucson AZ 🚨 Northern Outer Banks: High Surf Advisory issued October 21 at 8:28PM EDT until October 22 at 8:00PM EDT by NWS Newport/Morehead City NC 🚨 Ocracoke Island: Beach Hazards Statement issued October 21 at 8:28PM EDT until October 22 at 8:00PM EDT by NWS Newport/Morehead City NC 🚨 East Carteret: Beach Hazards Statement issued October 21 at 8:28PM EDT until October 22 at 8:00PM EDT by NWS Newport/Morehead City NC 🚨 Hatteras Island: Beach Hazards Statement issued October 21 at 8:28PM EDT until October 22 at 8:00PM EDT by NWS Newport/Morehead City NC 🚨 Hatteras Island: Coastal Flood Warning issued October 21 at 8:28PM EDT until October 22 at 8:00PM EDT by NWS Newport/Morehead City NC 🚨 Northern Outer Banks: Coastal Flood Advisory issued October 21 at 8:28PM EDT until October 22 at 8:00PM EDT by NWS Newport/Morehead City NC 🚨 Northern Outer Banks: Beach Hazards Statement issued October 21 at 8:28PM EDT until October 22 at 8:00PM EDT by NWS Newport/Morehead City NC 🚨 Hatteras Island: High Surf Advisory issued October 21 at 8:28PM EDT until October 22 at 8:00PM EDT by NWS Newport/Morehead City NC 🚨 Ocracoke Island: Coastal Flood Advisory issued October 21 at 8:28PM EDT until October 22 at 8:00AM EDT by NWS Newport/Morehead City NC
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 MIATCDAT5 ALL
TTAA00 KNHC DDHHMM
Subtropical Storm Josephine Discussion Number 1
NWS National Hurricane Center Miami FL AL102026
500 PM AST Wed Oct 21 2026
The non-tropical area of low pressure (Invest AL93) that we have
been monitoring this week has acquired enough subtropical
characteristics to be considered a subtropical storm.
Scatterometer data showed that fronts near the cyclone had
dissipated, with a smaller radius-of-maximum wind than yesterday.
Additionally moderate-to-deep convection has been organizing near
and west of the warm-core center. Thus, advisories have been
initiated on a subtropical storm, and 55 kt is shown as the initial
intensity based on the scatterometer data.
Josephine has been moving slowly northward today as a shortwave
ridge passes across the northeastern United States. The storm
should accelerate northeastward tomorrow as a mid-latitude trough
digs into the Great Lakes and Northeastern United States, taking
the system away from the US. By Friday, the low should turn
eastward, to the south of Newfoundland. Model guidance is in good
agreement on this path, and the new forecast is close to a blend of
the global model consensus and the NOAA corrected-consensus aid
HCCA.
The subtropical storm will likely intensify during the next day or
so through a favorable trough interaction while it remains near the
north wall of the Gulf Stream. Global models are in good agreement
on a band of hurricane-force winds developing tomorrow on the back
side of the low as it undergoes extratropical transition. A slow
weakening is anticipated by late Friday with the loss of forcing
from the trough while the system moves over cold water. The NHC
intensity forecast is similar to a blend of the GFS/ECMWF global
model solutions. The cyclone should become absorbed in about 4
days within a much larger low over the North Atlantic.
Since the coastal wind hazards with this system have been covered
for the last several days through non-tropical products issued by
local National Weather Service offices, and the system is forecast
to move away from the coast, those products will remain in effect
until the threat diminishes.
FORECAST POSITIONS AND MAX WINDS
INIT 21/2100Z 37.4N 69.5W 55 KT 65 MPH...SUBTROPICAL
12H 22/0600Z 38.1N 69.0W 60 KT 70 MPH...SUBTROPICAL
24H 22/1800Z 39.6N 66.2W 65 KT 75 MPH...POST-TROP/EXTRATROP
36H 23/0600Z 41.4N 61.6W 70 KT 80 MPH...POST-TROP/EXTRATROP
48H 23/1800Z 43.3N 56.9W 60 KT 70 MPH...POST-TROP/EXTRATROP
60H 24/0600Z 44.1N 53.5W 50 KT 60 MPH...POST-TROP/EXTRATROP
72H 24/1800Z 44.4N 50.4W 45 KT 50 MPH...POST-TROP/EXTRATROP
96H 25/1800Z 43.5N 37.5W 40 KT 45 MPH...POST-TROP/EXTRATROP
120H 26/1800Z...DISSIPATED
$$
Forecaster Blake
NNNN
ZCZC MIATCDEP2 ALL
TTAA00 KNHC DDHHMM
Tropical Storm Vance Discussion Number 2
NWS National Hurricane Center Miami FL EP222026
300 PM CST Wed Oct 21 2026
Satellite imagery shows that the system continues to produce deep
convection in improved banding features, as depicted in recent
microwave images. An earlier scatterometer pass shortly after the
previous advisory showed that the low-level center was slightly
farther south and had a peak wind of 27 kt. The latest satellite
intensity estimates from UW-CIMSS and TAFB are 32-35 kt, and using
these estimates, the initial intensity is raised to 35 kt for this
advisory, making the system Tropical Storm Vance.
The initial motion is estimated at 265/6 kt. A generally slow
forward motion is expected with a turn toward the northwest and then
north-northwest as the cyclone is steered along the southern and
western periphery of a mid-level ridge located over Mexico. There
continues to be some disagreement in the short term over when the
turn toward the northwest will occur The GFS and hurricane regional
models continue to show a southwest motion, while the HCCA and GDMI
show the system slowing and turning sooner. The latest NHC track
forecast is closest to the HCCA and GDMI, the best-performing models
this season, and was shifted slightly to the right compared to the
previous one.
Vance is within a conducive environment for steady to rapid
intensification (RI), with warm sea surface temperatures near
29-30C, low wind shear, and favorable upper-level divergence. RI
SHIPS and DTOPS guidance remains very bullish, showing RI over the
next 12-60 hours. The NHC intensity forecast follows suit and the
peak intensity was increased slightly from the previous one,
although it remains slightly below the GDMI and HCCA aids. In 72
hours, wind shear is forecast to increase and the system will move
into a slightly drier mid-level air mass. Thus, a weakening trend is
shown at that time.
FORECAST POSITIONS AND MAX WINDS
INIT 21/2100Z 9.4N 99.8W 35 KT 40 MPH
12H 22/0600Z 9.5N 100.5W 45 KT 50 MPH
24H 22/1800Z 9.8N 101.3W 60 KT 70 MPH
36H 23/0600Z 10.4N 102.1W 80 KT 90 MPH
48H 23/1800Z 11.2N 102.7W 95 KT 110 MPH
60H 24/0600Z 11.9N 103.1W 105 KT 120 MPH
72H 24/1800Z 12.8N 103.5W 100 KT 115 MPH
96H 25/1800Z 14.5N 104.3W 90 KT 105 MPH
120H 26/1800Z 15.8N 105.2W 85 KT 100 MPH
$$
Forecaster Kelly
NNNN
Threshold
Probability
× Climatology
20kt/12hr
18%
2.9×
25kt/24hr
62%
5.0×
30kt/24hr
46%
5.4×
35kt/24hr
36%
5.8×
40kt/24hr
22%
5.2×
45kt/36hr
60%
8.9×
55kt/48hr
73%
12.4×
65kt/72hr
52%
11.1×
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°), 13.6 kt | Gust: 17.5 kt
Pressure: 30.03 | Air Temp: 79.0 °F
Water Temp: 81.5 °F | Dew Point: 67.8 °F
Swell: 2.0 ft | Wind Wave: 2.0 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.