🚨 Newton, MS; Scott, MS: Severe Thunderstorm Warning issued August 26 at 7:33PM CDT until August 26 at 8:15PM CDT by NWS Jackson MS 🚨 Santa Cruz, AZ: Severe Thunderstorm Warning issued August 26 at 5:32PM MST until August 26 at 6:00PM MST by NWS Tucson AZ 🚨 Brown, IN; Greene, IN; Monroe, IN; Owen, IN: Severe Thunderstorm Warning issued August 26 at 8:32PM EDT until August 26 at 9:30PM EDT by NWS Indianapolis IN 🚨 Banner, NE: Severe Thunderstorm Warning issued August 26 at 6:31PM MDT until August 26 at 7:00PM MDT by NWS Cheyenne WY 🚨 Niobrara County: Special Weather Statement issued August 26 at 6:31PM MDT by NWS Cheyenne WY 🚨 Lonoke, AR; Pulaski, AR: Severe Thunderstorm Warning issued August 26 at 7:29PM CDT until August 26 at 8:15PM CDT by NWS Little Rock AR 🚨 Monroe, IN; Owen, IN: Flood Advisory issued August 26 at 8:28PM EDT until August 26 at 11:30PM EDT by NWS Indianapolis IN 🚨 Scott; Newton: Special Weather Statement issued August 26 at 7:28PM CDT by NWS Jackson MS 🚨 Walsenburg Vicinity/Upper Huerfano River Basin Below 7500 Ft; Trinidad Vicinity/Western Las Animas County Below 7500 Ft: Special Weather Statement issued August 26 at 6:28PM MDT by NWS Pueblo CO 🚨 Montgomery: None
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 MIATCDEP4 ALL
TTAA00 KNHC DDHHMM
Tropical Storm Iselle Discussion Number 14
NWS National Hurricane Center Miami FL EP092026
200 PM PDT Wed Aug 26 2026
Deep convection remains limited this afternoon with Iselle, and its
time as a tropical cyclone is limited. The low-level center remains
fully exposed as the system deals with dry air and moderate wind
shear. A recent scatterometer pass, which showed a peak wind of 34
kt, was helpful in adjusting the wind radii as the system continues
to weaken. Subjective and objective satellite intensity estimates
also continue to trend downward. Based on the scatterometer data and
the deteriorating satellite appearance, the initial intensity is
lowered to 35 kt.
Iselle is expected to continue moving west-northwestward over the
next few days, steered by a mid-level ridge to the north. Increasing
wind shear, cooler sea surface temperatures, and a drier air mass
will continue to weaken the cyclone. The latest NHC forecast follows
these trends and indicates Iselle will likely become a post-tropical
cyclone tonight. The post-tropical/remnant low is then expected to
gradually spin down and open into a trough in about 2 to 3 days.
Very minor adjustments were made to the previous NHC track and
intensity forecasts.
FORECAST POSITIONS AND MAX WINDS
INIT 26/2100Z 22.7N 124.9W 35 KT 40 MPH
12H 27/0600Z 23.2N 126.2W 35 KT 40 MPH...POST-TROPICAL
24H 27/1800Z 23.9N 127.9W 30 KT 35 MPH...POST-TROP/REMNT LOW
36H 28/0600Z 24.6N 129.6W 30 KT 35 MPH...POST-TROP/REMNT LOW
48H 28/1800Z 25.3N 131.1W 25 KT 30 MPH...POST-TROP/REMNT LOW
60H 29/0600Z...DISSIPATED
$$
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 262100
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TYPHOON 17W (SAUDEL) WARNING NR 034//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 28.6N 125.3E
INITIAL INTENSITY: 75 KTS
GEOGRAPHIC REFERENCE: 183 NM NORTHWEST OF KADENA AB
MOVEMENT PAST 6 HOURS: WESTWARD AT 05 KTS
SIGNIFICANT WAVE HEIGHT: 30 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS A STEADILY
BUT SLOWLY WEAKENING TYPHOON 17W, WHICH HAS MAINTAINED A 30NM WIDE,
RAGGED EYE FEATURE OVER THE PAST SIX HOURS. THE PREVIOUSLY OBSERVED
CLOUD-TOP WARMING HAS CEASED WITH THE APPROACH OF DIURNAL MAXIMUM AND
SMALL POCKETS OF DEEP CONVECTION ARE REFORMING ALONG THE EASTERN
FLANK OF THE EYE. A 261726Z NOAA-20 ATMS 89GHZ MICROWAVE IMAGE
REVEALED A LARGE MICROWAVE EYE FEATURE, TILTED WESTWARD WITH
REFERENCE TO THE LOWER-LEVEL EYE DUE TO THE PERSISTENT MODERATE
EASTERLY SHEAR, AND MODERATE CONVECTIVE ACTIVITY ACROSS THE
SOUTHEASTERN FLANK. THE INITIAL POSITION IS ASSESSED WITH HIGH
CONFIDENCE BASED ON THE 30NM WIDE EYE IN THE EIR AND THE MICROWAVE
IMAGE DISCUSSED ABOVE. THE INITIAL INTENSITY IS ASSESSED WITH MEDIUM
CONFIDENCE, BASED ON AN AVERAGE OF THE OBJECTIVE AND SUBJECTIVE
INTENSITY ESTIMATES NOTED BELOW. ENVIRONMENTAL CONDITIONS ARE
MARGINAL, WITH THE WARM SSTS AND MODERATE RADIAL OUTFLOW ALOFT BEING
OFFSET BY THE MODERATE TO HIGH EASTERLY SHEAR AND STEADILY DECREASING
OHC.
INITIAL WIND RADII BASIS: PERSISTENCE
CURRENT STEERING MECHANISM: SYSTEM IS POSITIONED TO THE SOUTH OF A
WEAKNESS IN THE SUBTROPICAL RIDGE (STR).
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T4.5 - 77 KTS
RJTD: T5.0 - 90 KTS
RCTP: T4.5 - 77 KTS
KNES: T4.5 - 77 KTS
CIMSS SATCON: 84 KTS AT 261728Z
CIMSS ADT: 65 KTS AT 261730Z
CIMSS AIDT: 71 KTS AT 261730Z
CIMSS D-MINT: 86 KTS AT 261729Z
CIMSS D-PRINT: 75 KTS AT 261800Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL
VWS: 20-25 KTS
SST: 28-29 CELSIUS
OUTFLOW: MODERATE RADIAL
OTHER FACTORS: DRY MID-LEVEL AIR TO THE NORTH.
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: TYPHOON (TY) 17W IS CURRENTLY POSITIONED SOUTH
OF A WEAKNESS IN THE STR TO THE NORTH, WHICH HAS RESULTED IN THE
SYSTEM SLOWLY DRIFTING NORTHWESTWARD OVER THE PAST 12 HOURS. OVER THE
LAST SIX HOURS, THE SYSTEM HAS REACHED ITS SLOWEST FORWARD SPEED, BUT
IMPORTANTLY, HAS BEGUN TO TURN WESTWARD AS THE STEERING PATTERN
BEGINS TO SHIFT. TY 17W WILL CONTINUE TO TRACK GENERALLY WESTWARD FOR
THE NEXT 12 HOURS AT A SLIGHTER FASTER SPEED THAN ITS CURRENTLY
TRACKING. THE SYSTEM THEN TURNS MORE SOUTHWESTWARD AS A LARGE STR
CENTERED OVER NORTH-CENTRAL CHINA BECOMES THE DOMINANT STEERING
INFLUENCE. TY 17W IS FORECAST TO MAKE LANDFALL ALONG THE CHINESE
COAST IN SOUTHERN ZHEJIANG PROVINCE BETWEEN TAU 24 AND TAU 36, BEFORE
CONTINUING INLAND ALONG A WEST-SOUTHWESTWARD TRACK THROUGH TAU 60.
REGARDING INTENSITY, THE SYSTEM IS EXPECTED TO SLOWLY WEAKEN AS IT
APPROACHES THE CHINESE COAST DUE TO THE PERSISTENT MODERATE TO HIGH
EASTERLY SHEAR AND DRY AIR ENTRAINMENT. ONCE THE SYSTEM MOVES ASHORE,
IT WILL RAPIDLY DECAY DUE TO LAND INTERACTION AND FRICTIONAL EFFECTS,
ULTIMATELY DISSIPATING OVER SOUTHEASTERN CHINA WITHIN THE NEXT 60
HOURS.
MODEL DISCUSSION: TRACK GUIDANCE IS IN STRONG AGREEMENT, WITH MINIMAL
CROSS- OR ALONG-TRACK SPREAD THROUGH THE END OF THE FORECAST PERIOD.
THE ONE NOTABLE EXCEPTION BEING THE EC-AIFS, WHICH TRACKS THE SYSTEM
ON A MUCH MORE SOUTHWARD TRAJECTORY, ENDING THE SYSTEM JUST NORTH OF
HONG KONG BY TAU 60. THE JTWC FORECAST IS PLACED…
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 262100
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL DEPRESSION 20W (TWENTY)
WARNING NR 003//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 17.2N 161.0E
INITIAL INTENSITY: 30 KTS
GEOGRAPHIC REFERENCE: 343 NM WEST-SOUTHWEST OF WAKE ISLAND
MOVEMENT PAST 6 HOURS: EASTWARD AT 01 KTS
SIGNIFICANT WAVE HEIGHT: 12 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS AN EXTREMELY
COMPACT AND DISORGANIZED SYSTEM, WITH A PARTIALLY EXPOSED LOW LEVEL
CIRCULATION CENTER (LLCC) DISPLACED TO THE SOUTH OF FLARING DEEP
CONVECTION AND ASSOCIATED MID-LEVEL MESOVORTEX. A 261524Z AMSR2 36GHZ
IMAGE REVEALED THE COMPACT LLCC EXPOSED ON THE SOUTHERN EDGE OF A
WEDGE OF LINEAR CONVECTION EXTENDING NORTHWARD. BASED ON COMPARISON OF
THE AMSR2 IMAGERY AND THE EARLIER ASCAT DATA, THE SYSTEM HAS REMAINED
QUASI-STATIONARY SINCE 1200Z. THE INITIAL POSITION IS ASSESSED WITH
HIGH CONFIDENCE BASED ON THE AMSR2 DATA AND ANIMATED MSI. THE INITIAL
INTENSITY IS ASSESSED WITH MEDIUM CONFIDENCE BASED ON A BLEND OF THE
AVAILABLE SUBJECTIVE AND OBJECTIVE INTENSITY ESTIMATES NOTED BELOW.
THE ENVIRONMENT IS MARGINALLY FAVORABLE, CHARACTERIZED BY LOW DEEP-
LAYER WIND SHEAR, MODERATE POLEWARD OUTFLOW ALOFT, AND WARM SSTS WITH
HIGH OHC. THE SYSTEM IS APPROXIMATELY 415NM SOUTHWEST OF INVEST 91W
AND UNDERGOING THE INITIAL PHASE OF BINARY INTERACTION. THE TWO
SYSTEMS ARE INTER-CONNECTED WITHIN A 1009MB CLOSED OUTER ISOBAR. THE
TWO ARE ALSO INTERTWINED ALOFT, WITH 20W POSITIONED IN THE
SOUTHWESTERN END OF AN ELONGATED UPPER-LEVEL ANTICYCLONE CENTERED
ROUGHLY IN THE VICINITY OF INVEST 91W.
INITIAL WIND RADII BASIS: NOT APPLICABLE (THERE ARE NO INITIAL WIND
RADII).
CURRENT STEERING MECHANISM: WEAK STEERING ENVIRONMENT; WEAK BAND OF
LOW-LEVEL SOUTHWESTERLIES ALONG THE NORTHWESTERN PERIPHERY OF A NEAR
EQUATORIAL RIDGE (NER) AND BINARY INTERACTION WITH INVEST 91W TO THE
NORTHEAST.
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T1.5 - 25 KTS
RJTD: T1.0 - 25 KTS
KNES: T2.0 - 30 KTS
PHFO: T2.5 - 35 KTS
CIMSS SATCON: 34 KTS AT 261720Z
CIMSS ADT: 34 KTS AT 261740Z
CIMSS AIDT: 32 KTS AT 261740Z
CIMSS D-MINT: 22 KTS AT 261751Z
CIMSS D-PRINT: 22 KTS AT 261800Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINALLY FAVORABLE
VWS: 5-10 KTS
SST: 29-30 CELSIUS
OUTFLOW: MODERATE POLEWARD
OTHER FACTORS: EXTREMELY COMPACT NATURE OF THE SYSTEM AND THE
INFLUENCE OF THE BINARY INTERACTION WITH 91W.
ANALYSIS CONFIDENCE:
INITIAL POSITION: HIGH
INITIAL INTENSITY: MEDIUM
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: TROPICAL DEPRESSION (TD) 20W HAS MOVED LITTLE IN
THE PAST SIX HOURS, CURRENTLY TRAPPED IN A WEAK AND COMPETING STEERING
ENVIRONMENT. OVER THE NEXT 12 TO 24 HOURS, TD 20W WILL TRACK SLOWLY
EASTWARD ALONG THE NORTH SIDE OF THE WEAK NER TO THE SOUTHEAST. AFTER
TAU 24, THE NER IS EXPECTED TO RECEDE EQUATORWARD, WHILE A NOSE OF THE
STR TO THE NORTHEAST PUSHES SOUTHWARD TO THE EAST OF BOTH 20W AND 91W.
THE COMBINATION OF A STRENGTHENING GRADIENT ON THE EASTERN SIDE OF TD
20W AND THE INFLUENCE OF THE BINARY INTERACTION WITH 91W, WILL PUSH TD
20W NORTHWARD THROUGH THE REMAINDER OF THE FORECAST PERIOD. REGARDING
INTENSITY, THE SYSTEM WILL REMAIN STAGNANT OR INTENSIFY ONLY SLIGHTLY
OVER THE COURSE OF THE NEXT 24 HOURS DUE TO THE CONTINUED INFLUENCE OF
MODERATE MID-LEVEL SOUTHERLY SHEAR AND A RELATIVELY WEAK OUTFLOW
ENVIRONMENT ALOFT. BY TAU 36, AS 91W MOVES RAPIDLY NORTHWARD INTO A
BAND OF UNFAVORABLE CONDITIONS ALOFT, 20W WILL HAVE AN OPPORTUNITY TO
INTENSIFY MORE RAPIDLY AS IT REMAINS IN A REGION OF LIGHT SHEAR A…
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 (40°), 3.9 kt | Gust: 5.8 kt
Pressure: 29.95 | Air Temp: 87.1 °F
Water Temp: 88.7 °F | Dew Point: 77.7 °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.