🚨 Montgomery: None 🚨 Inland Worcester; Maryland Beaches; Accomack; Northampton: Wind Advisory issued September 25 at 8:33PM EDT until September 26 at 11:00AM EDT by NWS Wakefield VA 🚨 Coastal Horry; Coastal Georgetown: Coastal Flood Advisory issued September 25 at 8:32PM EDT until September 25 at 9:00PM EDT by NWS Wilmington NC 🚨 Coastal Pender; Coastal New Hanover: Coastal Flood Advisory issued September 25 at 8:32PM EDT until September 25 at 9:00PM EDT by NWS Wilmington NC 🚨 Coastal Brunswick: Coastal Flood Advisory issued September 25 at 8:32PM EDT until September 25 at 9:00PM EDT by NWS Wilmington NC 🚨 Coastal Pender; Coastal New Hanover: Rip Current Statement issued September 25 at 8:32PM EDT until September 26 at 8:00PM EDT by NWS Wilmington NC 🚨 Inland New Hanover: Coastal Flood Advisory issued September 25 at 8:32PM EDT until September 26 at 12:00AM EDT by NWS Wilmington NC 🚨 Lower Rio Grande Valley; South Central Highlands; San Agustin Plains and Adjacent Lowlands: Special Weather Statement issued September 25 at 6:31PM MDT by NWS Albuquerque NM 🚨 Northern El Paso County/Monument Ridge/Rampart Range Below 7500 Ft; Colorado Springs Vicinity/Southern El Paso County/Rampart Range Below 7400 Ft: Special Weather Statement issued September 25 at 6:19PM MDT by NWS Pueblo CO 🚨 Central Highlands; Northeast Highlands; Eastern San Miguel County; Guadalupe County: Special Weather Statement issued September 25 at 6:17PM MDT by NWS Albuquerque NM
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 MIATCDAT1 ALL
TTAA00 KNHC DDHHMM
Tropical Storm Fay Discussion Number 23
NWS National Hurricane Center Miami FL AL062026
900 PM GMT Fri Sep 25 2026
The convective organization for Fay has taken a turn downward as
wind shear and dry air have started to impact the system. The most
recent TAFB Dvorak fix was a 2.5/35 kt and the objective intensity
from UW-CIMSS is in the range of 37-47 kt. Therefore, the initial
intensity has been lowered to 45 kt for this advisory.
The cyclone is expected to gradually weaken as the shear and dry
air build over the cyclone. The statistical GFS/ECMWF SHIPS
intensity guidance indicates that the northerly shear will continue
to increase over the next several hours. The wind shear will make
it easier for the dry air to penetrate the core of the cyclone and
hinder the development of convection. The simulated ECMWF and GFS
satellite imagery show that Fay loses its convection towards the
end of the weekend, at which point it would become a post-tropical
remnant low. However it is possible that this could occur sooner
given the intensity of the wind shear being over 20 kt and mid-level
relative humidity less than 40 percent. The current NHC intensity
forecast is in line with the guidance suite including the HCCA and
GDMI forecast aids.
Fay's initial motion is estimated to be west-southwest, or 250/4 kt
as the storm is being steered by a subtropical ridge over the
central Atlantic. The cyclone is expected to continue on a
west-southwest to southwest heading through the the forecast period
as the storm continues to weaken and become a vertically shallow
remnant low steered by the low-level flow. The latest NHC track
forecast is similar to the previous forecast, however the forward
speed has been increased. The current forecast is still in good
agreement with the GDMI ensemble mean and HCCA corrected consensus
aids.
FORECAST POSITIONS AND MAX WINDS
INIT 25/2100Z 29.8N 43.0W 45 KT 50 MPH
12H 26/0600Z 29.7N 43.5W 40 KT 45 MPH
24H 26/1800Z 29.5N 44.1W 35 KT 40 MPH
36H 27/0600Z 29.1N 44.6W 30 KT 35 MPH
48H 27/1800Z 28.5N 45.0W 30 KT 35 MPH...POST-TROP/REMNT LOW
60H 28/0600Z 27.6N 45.4W 25 KT 30 MPH...POST-TROP/REMNT LOW
72H 28/1800Z 26.9N 46.2W 25 KT 30 MPH...POST-TROP/REMNT LOW
96H 29/1800Z 26.1N 47.2W 25 KT 30 MPH...POST-TROP/REMNT LOW
120H 30/1800Z...DISSIPATED
$$
Forecaster Katz/Beven
NNNN
ZCZC MIATCDAT2 ALL
TTAA00 KNHC DDHHMM
Tropical Storm Gonzalo Discussion Number 4
NWS National Hurricane Center Miami FL AL072026
800 PM CVT Fri Sep 25 2026
The overall structure of Gonzalo has changed little today. The
circulation is elongated from the north-northeast to south-southwest
with the advisory position set as a mean between a couple of
low-level vorticity centers on either end of the elongated center.
Deep convection remains displaced well to the northeast of the
estimated center due to moderate to strong southwesterly shear.
Objective and subjective satellite intensity estimates have not
changed much, therefore the initial intensity remains 45 kt, in line
with the earlier scatterometer data.
Gonzalo has been moving more northward today with an initial motion
estimate of 350/10 kt. The storm is expected to be steered
northward to north-northwestward during the next couple of days
between a mid-level trough to its north and a ridge over western
Africa. Gonzalo's forward speed is expected to decrease as the
system becomes increasingly shallow and is steered by the weaker
low-level flow. The new official track forecast is similar to the
previous advisory and lies closest to the latest Google Deep Mind
ensemble prediction.
The vertical shear over Gonzalo is forecast to increase
significantly on Saturday and with gradually decreasing sea surface
temperatures along the forecast track, weakening should begin by
Saturday morning. Simulated satellite imagery from the global
models indicate that Gonzalo will lose organized deep convection in
24 to 36 hours, and the new NHC forecast shows the system becoming a
post-tropical remnant low by Sunday morning. The intensity forecast
is in best agreement with the typically reliable consensus aids.
Key Messages:
1. Tropical storm conditions will continue across portions of the
Cabo Verde Islands tonight.
2. Heavy rains from Gonzalo could affect the eastern portions of
the Cabo Verde Islands and the western coast of Africa between
Guinea-Bissau to Senegal through Saturday. Areas of flash flooding
will be possible along the Africa coast with some isolated flash
flood concerns for the eastern islands of Cabo Verde.
FORECAST POSITIONS AND MAX WINDS
INIT 25/2100Z 16.2N 22.7W 45 KT 50 MPH
12H 26/0600Z 17.6N 22.9W 45 KT 50 MPH
24H 26/1800Z 19.0N 23.3W 35 KT 40 MPH
36H 27/0600Z 20.0N 23.5W 30 KT 35 MPH...POST-TROP/REMNT LOW
48H 27/1800Z 20.6N 23.9W 25 KT 30 MPH...POST-TROP/REMNT LOW
60H 28/0600Z 21.2N 24.3W 20 KT 25 MPH...POST-TROP/REMNT LOW
72H 28/1800Z 21.7N 24.6W 20 KT 25 MPH...POST-TROP/REMNT LOW
96H 29/1800Z 22.0N 25.0W 20 KT 25 MPH...POST-TROP/REMNT LOW
120H 30/1800Z...DISSIPATED
$$
Forecaster Brown
NNNN
ZCZC MIATCDEP1 ALL
TTAA00 KNHC DDHHMM
Hurricane Odalys Discussion Number 24
NWS National Hurricane Center Miami FL EP162026
200 PM PDT Fri Sep 25 2026
Satellite imagery shows Odalys is still a powerful major hurricane,
though the satellite presentation is not quite as impressive as
earlier today. The ragged eye of Odalys is surrounded by a ring of
deep convection with cold cloud tops of -65 to -75 deg C. Earlier
WSF-M passive microwave imagery from 1437 UTC showed a closed ring
in the 37 GHz channel, while the 89 GHz image indicated the
mid-level eyewall was open to the southwest. The latest Dvorak
classification from TAFB was a 5.5/6.0, while recent AiDT, D-MINT,
and D-PRINT estimates have fallen to around 105 kt. Based on a blend
of these data, the initial intensity is conservatively lowered to
110 kt. The wind radii for Odalys were adjusted based on recent
RCM-1 synthetic aperture radar data.
Odalys is moving slowly north-northeastward (030/4 kt) within the
flow between a mid- to upper-level trough to its west and a
mid-level ridge over northern Mexico. The hurricane is expected to
move northward during the next day or two as the aforementioned
trough amplifies over the eastern Pacific. By Monday, Odalys is
forecast to slow down and turn abruptly to the east and southeast as
the increasingly shallow circulation becomes steered by the
low-level flow. The latest track guidance shows a sharper turn than
the previous cycle in the 60-96 h time frame, and the NHC track
forecast has been adjusted to reflect this trend. Overall, the NHC
forecast remains close to the skillful HCCA aid.
Southwesterly shear is expected to markedly increase over the next
couple of days, while Odalys' forecast track should take the system
over cooler waters by Sunday. As a result, a faster weakening trend
is forecast over the weekend, with Odalys likely to lose organized
convection and degenerate to a post-tropical cyclone in 48-60 h. The
updated NHC intensity forecast is in best agreement with the Google
DeepMind ensemble mean and lies slightly above the HCCA and IVCN
multi-model aids.
Distant moisture from Hurricane Odalys and Polo will be transported
into the southwestern United States this weekend and early next
week, and may indirectly contribute to a heavy rainfall and flash
flood threat in the region. See products issued by the Weather
Prediction Center for more information.
FORECAST POSITIONS AND MAX WINDS
INIT 25/2100Z 18.3N 123.6W 110 KT 125 MPH
12H 26/0600Z 18.9N 123.5W 105 KT 120 MPH
24H 26/1800Z 20.0N 123.4W 85 KT 100 MPH
36H 27/0600Z 21.1N 123.3W 70 KT 80 MPH
48H 27/1800Z 22.0N 122.9W 50 KT 60 MPH
60H 28/0600Z 22.4N 122.3W 40 KT 45 MPH...POST-TROPICAL
72H 28/1800Z 21.9N 121.6W 30 KT 35 MPH...POST-TROP/REMNT LOW
96H 29/1800Z 19.9N 120.3W 25 KT 30 MPH...POST-TROP/REMNT LOW
120H 30/1800Z 17.5N 119.0W 20 KT 25 MPH...POST-TROP/REMNT LOW
$$
Forecaster Reinhart
NNNN
ZCZC MIATCDEP2 ALL
TTAA00 KNHC DDHHMM
Hurricane Polo Discussion Number 21
NWS National Hurricane Center Miami FL EP172026
200 PM MST Fri Sep 25 2026
A NOAA research aircraft has found that Polo remains a very
powerful category 5 hurricane. The highest flight level winds
measured by the aircraft were 165 kt in the northeast quadrant, and
since that measurement the central pressure has decreased a couple
millibars, to 913. An UAS launched from the plane measured a peak
wind just above 200 kt at an altitude just below 500 m, which
corresponds to a 10 m wind of 150-155 kt based on an experimental
wind reduction model. Taken all together, this data supports an
initial intensity of 155 kt.
The NOAA aircraft reported that there may be signs of an eyewall
replacement cycle beginning. Although this does not appear to be
having an impact on the hurricane yet, it does highlight that
fluctuations in the intensity of Polo are likely over the next 24 h
while it remains over warm waters. After that, some weakening is
expected as Polo begins to move into a region with lower ocean heat
content and the vertical wind shear increases slightly. However, it
is expected to remain a powerful major hurricane through the
weekend. The NHC intensity forecast is still near the upper-end of
the intensity guidance and is very similar to the previous advisory.
Only small adjustments were made to the official track forecast,
with the biggest change being that the anticipated forward motion
for Polo is slightly faster in this advisory. Polo is still
expected to turn gradually northwestward, then northward this
weekend as it moves around the western side of a ridge centered
over northern Mexico. Then early next week an upper-level trough
approaching from the northwest will likely cause the hurricane to
turn northeastward toward Baja California Sur and west-central
Mexico. The AI models, notably GDM and the experimental
WeatherNext3, generally show a slightly faster motion than most of
the dynamical guidance, and the model spread has increased at 72 h
and beyond. The forecast confidence is correspondingly lower with
this advisory. The NHC forecast is a blend of the consensus
and continuity with the previous advisory. Based on the forecast
track, watches could be required for portions of Baja California Sur
as soon as tonight.
Distant moisture from Hurricane Polo and Odalys will be transported
into the southwestern United States this weekend and early next
week, and may indirectly contribute to a heavy rainfall and flash
flood threat in the region. See products issued by the Weather
Prediction Center for more information.
Key Messages:
1. Polo is forecast to approach the Baja California Peninsula early
next week as a hurricane. Interests there should closely monitor
the latest updates and ensure that they have their preparedness
plan in place. Watches could be required as early as tonight for
portions of the area.
2. Heavy rainfall associated with Polo may begin to impact Baja
California Sur late Sunday into Monday. This rainfall may produce
life-threatening flooding and mudslides, especially in areas of
steep terrain.
FORECAST POSITIONS AND MAX WINDS
INIT 25/2100Z 17.2N 109.2W 155 KT 180 MPH
12H 26/0600Z 17.4N 110.6W 150 KT 175 MPH
24H 26/1800Z 18.2N 112.1W 140 KT 160 MPH
36H 27/0600Z 19.6N 113.2W 125 KT 145 MPH
48H 27/1800Z 21.5N 113.7W 115 KT 130 MPH
60H 28/0600Z 23.4N 113.6W 100 KT 115 MPH
72H 28/1800Z 25.1N 112.8W 95 KT 110 MPH
96H 29/1800Z 28.5N 109.7W 60 KT 70 MPH...INLAND
120H 30/1800Z 32.0N 105.5W 25 KT 30 MPH...POST-TROP/INLAND
$$
Forecaster D. Zelinsky
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 252100
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 25W (SURIGAE) WARNING NR
011//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 21.9N 127.8E
INITIAL INTENSITY: 55 KTS
GEOGRAPHIC REFERENCE: 276 NM SOUTH OF KADENA AB
MOVEMENT PAST 6 HOURS: NORTH-NORTHWESTWARD AT 07 KTS
SIGNIFICANT WAVE HEIGHT: 22 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS TROPICAL
STORM (TS) 25W (SURIGAE) CONTINUING TO IMPROVE ITS CONVECTIVE
STRUCTURE AS THE LOW LEVEL CIRCULATION CENTER (LLCC) REMAINS TUCKED
UNDERNEATH THE PERSISTENT CENTRAL DENSE OVERCAST (CDO), AS WELL AS
BEGINNING TO DEVELOP A BAND OF CONVECTION ON THE NORTHERN QUADRANT.
A 251658 AMSR3 37 GHZ MICROWAVE IMAGE DEPICTS AN ALMOST FULLY
CLOSED MICROWAVE EYE FEATURE WITH A PARTIALLY CLOSED AND SLIGHTLY
OFFSET RING OF CONVECTION REFLECTED IN THE 89 GHZ IMAGE, INDICATING
A SLIGHT BUT LESSENING NORTHWESTWARD TILT WITH HEIGHT.
ENVIRONMENTAL CONDITIONS ARE ASSESSED TO BE HIGHLY FAVORABLE, WITH
VERTICAL WIND SHEAR (VWS) ASSESSED TO BE LOW (5-10 KTS), WARM
(29-30 C) SEA SURFACE TEMPERATURES (SSTS), AND IMPROVED OUTFLOW
ALOFT, BOTH IMPROVING RADIALLY AS UPPER LEVEL SHEAR HAS ABATED, AS
WELL AS MAINTAINING A ROBUST POLEWARD OUTFLOW CHANNEL. THE INITIAL
POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE AMSR3 DATA.
THE INITIAL INTENSITY IS ASSESSED WITH HIGH CONFIDENCE BASED ON
AGREEMENT ACROSS AGENCY DVORAK FIXES AND CIMSS OBJECTIVE ESTIMATES
LISTED BELOW.
INITIAL WIND RADII BASIS: PERSISTENCE
CURRENT STEERING MECHANISM: SUBTROPICAL RIDGE CENTERED TO THE
NORTHEAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T3.5 - 55 KTS
RJTD: T3.0 - 45 KTS
RCTP: T3.0 - 45 KTS
CIMSS SATCON: 54 KTS AT 251712Z
CIMSS ADT: 51 KTS AT 251750Z
CIMSS AIDT: 49 KTS AT 251750Z
CIMSS D-MINT: 59 KTS AT 251713Z
CIMSS D-PRINT: 59 KTS AT 251710Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: HIGHLY FAVORABLE
VWS: 5-10 KTS
SST: 29-30 CELSIUS
OUTFLOW: STRONG RADIAL
OTHER FACTORS: ADDITIONAL POLEWARD OUTFLOW CHANNEL
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 HAS BEGUN TO SLOW IN TRACK SPEED AND
TURN POLEWARD AS IT APPROACHES THE AXIS OF THE SUBTROPICAL RIDGE
(STR) CENTERED TO THE NORTHEAST. TRACK SPEED IS FORECAST TO REMAIN
SLOWER OUT TO TAU 36 AS 25W ENTERS THE COL BETWEEN THE STR TO THE
NORTHEAST AND THE WEAKER STR CENTERED FARTHER TO THE WEST OVER
SOUTHERN CHINA. BY TAU 36, THE STRONGER STEERING INFLUENCE OF THE
EASTERN STR AS WELL AS THE PASSAGE OF A MID-LATITUDE SHORTWAVE
TROUGH WILL BOTH AID IN THE RECURVATURE AND NORTHEASTWARD TURN OF
25W. ONCE POLEWARD OF THE STEERING STR, TRACK SPEED IS FORECAST TO
ACCELERATE AS 25W NEARS THE STRONG WESTERLIES ASSOCIATED WITH THE
UPPER-LEVEL JET, CAUSING THE ONSET OF EXTRATROPICAL TRANSITION
(ETT) AT TAU 120. REGARDING INTENSITY, TS 25W IS FORECAST TO
INTENSIFY 25 KTS OVER THE NEXT 24 HOURS, JUST SHORT OF THE TRUE
RATE OF RI AS THE SYSTEM NEARS THE AXIS OF THE STR AND AN AREA OF
ENHANCED OUTFLOW ALOFT WHILE ALL OTHER ENVIRONMENTAL CONDITIONS ARE
EXPECTED TO REMAIN FAVORABLE. 25W IS FORECAST TO PEAK AT 85 KTS
BETWEEN TAUS 36 AND 48 IN CONJUNCTION WITH THE TIME OF CPA TO
KADENA AS IT PASSES TO THE SOUTHEAST OF OKINAWA. AFTER THIS POINT,
25W IS EXPECTED TO BEGIN A WEAKENING TREND FOR THE REMAINDER OF THE
FORECAST PERIOD AS NORTHWESTERLY VWS INCREASES AND SSTS COOL. THERE
REMAINS A POSSIBILITY FOR 25W TO INTENSIFY MORE RAPIDLY THAN
FORECAST IN THE SHORT TERM DEPENDING HOW QUICKLY 25W VERTICALLY
ALIGNS ITS INNER CORE AS WELL AS HOW LONG IT WILL BE IN THE…
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: ENE (60°), 7.8 kt | Gust: 9.7 kt
Pressure: 29.93 steady | Air Temp: 85.1 °F
Water Temp: | Dew Point: 75.9 °F
Swell: 2.3 ft | Wind Wave: 1.3 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.