🚨 Northerly Island to Calumet Harbor IL; Calumet Harbor IL to Gary IN; Gary to Burns Harbor IN; Burns Harbor to Michigan City IN; Lake Michigan from Wilmette Harbor to Michigan City in 5NM offshore to Mid Lake: Special Marine Warning issued August 11 at 12:30AM CDT until August 11 at 2:00AM CDT by NWS Chicago IL     🚨 Montgomery: None     🚨 Hardin, OH; Logan, OH; Union, OH: Flood Warning issued August 11 at 1:27AM EDT until August 11 at 5:30AM EDT by NWS Wilmington OH     🚨 Cuyahoga; Lake; Geauga: Special Weather Statement issued August 11 at 1:27AM EDT by NWS Cleveland OH     🚨 Cuyahoga; Geauga; Summit; Portage; Trumbull; Mahoning: Special Weather Statement issued August 11 at 1:26AM EDT by NWS Cleveland OH     🚨 La Paz, AZ; Yuma, AZ; Imperial, CA; Riverside, CA: Dust Advisory issued August 10 at 10:26PM MST until August 10 at 11:30PM MST by NWS Phoenix AZ     🚨 Maumee Bay to Reno Beach OH; Reno Beach to The Islands OH; The Islands to Vermilion OH; Detroit River Lt. to Maumee Bay OH to Reno Beach OH beyond 5NM offshoreline to US-Canadian border; Reno Beach to The Islands OH beyond 5NM off shoreline to US-Canadian border; The Islands to Vermilion OH beyond 5 nm off shoreline to US-Canadian border: Severe Thunderstorm Watch issued August 11 at 1:25AM EDT until August 11 at 2:00AM EDT by NWS Cleveland OH     🚨 Vermilion to Avon Point OH; Avon Point to Willowick OH; Willowick to Geneva-on-the Lake OH; Vermilion to Avon Point OH beyond 5 nm off shoreline to US-Canadian border; Avon Point to Willowick OH beyond 5 nm off shoreline to US-Canadian border; Willowick to Geneva-on-the-Lake OH beyond 5NM off shoreline to US-Canadian border: Special Marine Warning issued August 11 at 1:22AM EDT until August 11 at 2:45AM EDT by NWS Cleveland OH     🚨 Garrett, MD: Flash Flood Warning issued August 11 at 1:21AM EDT until August 11 at 4:15AM EDT by NWS Baltimore MD/Washington DC     🚨 Reno Beach to The Islands OH; The Islands to Vermilion OH; Reno Beach to The Islands OH beyond 5NM off shoreline to US-Canadian border: Special Marine Warning issued August 11 at 1:19AM EDT until August 11 at 2:00AM EDT by NWS Cleveland OH    

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.

Summary & NHC 7-Day Formation Outlook

Valid: 05 UTC 11 Aug 2026

Active storms summary

Select a Storm

93C (CP932026)

Type: DB Max Wind: 25 kt Min Pressure: 1006 hPa Position: 10.7, -140.8 Basin: East Pacific

PEILOU (WP132026)

Type: TS Max Wind: 35 kt Min Pressure: 995 hPa Position: 24.4, 155.8 Basin: West Pacific
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 110300 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 13W (PEILOU) WARNING NR 017// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 24.4N 155.8E INITIAL INTENSITY: 35 KTS GEOGRAPHIC REFERENCE: 674 NM WEST-NORTHWEST OF WAKE ISLAND MOVEMENT PAST 6 HOURS: NORTHEASTWARD AT 25 KTS SIGNIFICANT WAVE HEIGHT: 14 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS DISORGANIZED CONVECTION OBSCURING THE LOW-LEVEL CIRCULATION CENTER (LLCC) OF TROPICAL STORM (TS) 13W. A WEDGE OF DRY AIR TO THE WEST OF THE SYSTEM CAN BE OBSERVED IN ANIMATED WATER VAPOR IMAGERY MAKING ITS WAY INTO THE VORTEX CORE. SOME PRESSURE FROM SOUTHERLY VERTICAL WIND SHEAR IS ALSO EVIDENT, DISPLACING THE REMAINING CONVECTION SLIGHTLY NORTH OF THE ASSESSED CENTER. THE INITIAL POSITION IS PLACED WITH MEDIUM CONFIDENCE BASED ON LOW-LEVEL CLOUD MOTION BRIEFLY EXPOSED IN THE SOUTHEASTERN QUADRANT AND TRACKING CONVECTIVE FEATURES IN ANIMATED MSI. THE INITIAL INTENSITY OF 35 KTS IS ASSESSED WITH MEDIUM CONFIDENCE BASED ON THE AGENCY DVORAK FIXES AND OVERALL LACK OF STRUCTURAL CHANGE IN THE ANIMATED MSI. THE ENVIRONMENT IS CHARACTERIZED AS MARGINAL WITH WARM SEA SURFACE TEMPERATURES AND LOW VERTICAL WIND SHEAR, OFFSET BY THE DRY AIR ENTRAINMENT AND WEAK OUTFLOW ALOFT. INITIAL WIND RADII BASIS: PERSISTENCE CURRENT STEERING MECHANISM: EASTERN PERIPHERY OF A LARGE, LOW-LEVEL CYCLONIC GYRE CENTERED TO THE WEST. AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T2.5 - 35 KTS RJTD: T2.5 - 35 KTS RCTP: T3.0 - 45 KTS KNES: T2.5 - 35 KTS CIMSS ADT: 53 KTS AT 110000Z CIMSS AIDT: 43 KTS AT 110000Z CIMSS D-PRINT: 45 KTS AT 110000Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL VWS: 5-10 KTS SST: 28-29 CELSIUS OUTFLOW: WEAK POLEWARD OTHER FACTORS: DRY AIR ENTRAINMENT FROM THE WEST ANALYSIS CONFIDENCE: INITIAL POSITION: MEDIUM INITIAL INTENSITY: MEDIUM INITIAL WIND RADII: LOW 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. FORECAST DISCUSSION: TS 13W (PEILOU) HAS ACCELERATED NORTHEASTWARD OVER THE PAST 6 HOURS ON A TRACK THAT IS SEPARATING IT FROM THE EASTERN PERIPHERY OF THE CYCLONIC GYRE CENTERED TO THE WEST. AN EXTENSION OF A SUBTROPICAL RIDGE BUILDING IN SOUTH OF THE SYSTEM IS HELPING TO MAINTAIN THE NORTHEASTWARD TRACK OVER THE NEXT 24 HOURS, EVENTUALLY STEERING THE SYSTEM EAST-NORTHEASTWARD BY TAU 36. THE INTENSITY IS EXPECTED TO STEADILY DECREASE FOR THE DURATION OF THE FORECAST PERIOD AS DRY AIR CONTINUES TO INTRUDE INTO THE CORE, SEA SURFACE TEMPERATURES DECREASE, AND WESTERLY VWS INCREASES. DISSIPATION IS EXPECTED UNDER THESE UNFAVORABLE ENVIRONMENTAL CONDITIONS BY TAU 36. MODEL DISCUSSION: MODEL TRACK GUIDANCE IS IN GOOD AGREEMENT ABOUT THE NORTHEASTWARD TRAJECTORY FOLLOWED BY AN EAST-NORTHEASTWARD TURN BY TAU 36, WITH A CROSS-TRACK SPREAD OF 75 NM AT THAT TIME. THE JTWC TRACK FORECAST IS PLACED CLOSE TO THE MULTI-MODEL CONSENSUS WITH HIGH CONFIDENCE. MODEL INTENSITY GUIDANCE IS ALSO IN AGREEMENT ABOUT THE WEAKENING TREND OF 13W, WITH THE NOTABLE EXCEPTION OF THE DECAY SHIPS SOLUTIONS, WHICH SUGGEST STEADY INTENSIFICATION. THIS ABERRATION IS LIKELY DUT TO THE FACT THAT SHIPS LOSES TRACK OF THE VORTEX AND REVERTS TO CLIMATOLOGY BASED SOLUTIONS. THE JTWC INTENSITY FORECAST IS PLACED ON THE LOW END OF THE GUIDANCE ENVELOPE WITH MEDIUM CONFIDENCE, DISCOUNTING THE SHIPS SOLUTIONS AS OUTLIERS. FORECAST CONFIDENCE: TRACK 00-72 HR: HIGH INTENSITY 00-72 HR: MEDIUM// NNNN

CHAN-HOM (WP142026)

Type: TS Max Wind: 50 kt Min Pressure: 976 hPa Position: 36.8, 143.7 Basin: West Pacific
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 110300 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 14W (CHAN-HOM) WARNING NR 017// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 36.8N 143.7E INITIAL INTENSITY: 50 KTS GEOGRAPHIC REFERENCE: 173 NM EAST-NORTHEAST OF NARITA AIRPORT MOVEMENT PAST 6 HOURS: WESTWARD AT 18 KTS SIGNIFICANT WAVE HEIGHT: 29 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS A FULLY EXPOSED LOW-LEVEL CIRCULATION CENTER (LLCC) MOVING BRISKLY WESTWARD TOWARD CENTRAL HONSHU. THE ARRANGEMENT OF CONVECTION AND DRY AIR AROUND THE CIRCULATION HAS ROTATED COUNTERCLOCKWISE OVER THE PAST SIX HOURS, WITH LIMITED CONVECTION NOW CONFINED SOUTHWEST AND SOUTH OF THE LLCC, WHILE A DEEP-LAYER DRY SLOT HAS ENVELOPED THE EASTERN SEMICIRCLE AND IS NOW ROTATING INTO THE NORTHERN SEMICIRCLE. AFTER PASSING OVER A COLD OCEAN EDDY EARLIER, THE STORM IS NOW OVER A WARMER EDDY OF 26C TO 27C SEA SURFACE TEMPERATURES, YET CONVECTIVE COVERAGE HAS NOT IMPROVED. THE STORM CONTINUES TO DEGRADE OVERALL IN TERMS OF CONVECTIVE STRUCTURE. THE CIRCULATION REMAINS VIGOROUS, HOWEVER, AND A RECENT 102359Z ASCAT-C SCATTEROMETER PASS REVEALED THAT THE WIND FIELD REMAINS PERSISTENT DESPITE THE STORM'S DEGRADING SATELLITE APPEARANCE, WITH 45 TO 50 KT WINDS ARCING THROUGH THE NORTHERN SEMICIRCLE OF THE CIRCULATION. THE INITIAL INTENSITY IS THUS BUMPED TO 50 KT. GALE-FORCE WIND RADII HAVE EXPANDED RELATIVE TO SIX HOURS AGO, AND ARE NOW APPROACHING COASTAL AREAS OF NORTHERN HONSHU. INITIAL WIND RADII BASIS: SCATTEROMETER DATA CURRENT STEERING MECHANISM: SUBTROPICAL RIDGE TO THE NORTH AND A DEEP UPPER LOW TO THE SOUTH AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T3.0 - 45 KTS RJTD: T2.5 - 35 KTS RCTP: T2.5 - 35 KTS CIMSS D-MINT: 40 KTS AT 102031Z CIMSS D-PRINT: 37 KTS AT 102330Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL VWS: 25-30 KTS SST: 26-27 CELSIUS OUTFLOW: MODERATE WESTWARD OTHER FACTORS: DEEP-LAYER DRY AIR WRAPPING AROUND THE EASTERN AND NORTHERN SEMICIRCLES ANALYSIS CONFIDENCE: INITIAL POSITION: HIGH INITIAL INTENSITY: HIGH INITIAL WIND RADII: HIGH 3. FORECAST REASONING. SIGNIFICANT FORECAST CHANGES: THERE ARE NO SIGNIFICANT CHANGES TO THE FORECAST FROM THE PREVIOUS WARNING. FORECAST DISCUSSION: TROPICAL STORM 14W (CHAN-HOM) CONTINUES TO MARCH TOWARD CENTRAL HONSHU WITH PACE AS IT PINWHEELS AROUND THE NORTHERN PERIPHERY OF A DEEP UPPER-LEVEL LOW TO ITS SOUTH. THIS UPPER LOW IS IMPOSING STRONG EASTERLY WIND SHEAR AND INJECTING DEEP-LAYER DRY AIR INTO THE CIRCULATION, WHICH SHOULD PREVENT INTENSIFICATION IN THE FINAL HOURS PRIOR TO LANDFALL IN JAPAN. THE CURRENTLY BARREN CONVECTIVE STRUCTURE SUPPORTS THIS CONCLUSION, THOUGH A POTENT WIND FIELD WILL NEVERTHELESS MOVE ASHORE. LANDFALL IN IBARAKI PREFECTURE, JAPAN IS EXPECTED IN LESS THAN 12 HOURS, FOLLOWED BY A GENERALLY WESTWARD TRACK ACROSS THE MOUNTAINOUS TERRAIN OF CENTRAL HONSHU, WHICH WILL RESULT IN QUICK WEAKENING BELOW TROPICAL STORM INTENSITY. EMERGENCE OVER THE SOUTHERN SEA OF JAPAN IS EXPECTED IN ABOUT 24 HOURS, WHERE HOSTILE ENVIRONMENTAL CONDITIONS CONSISTING OF STRONG WIND SHEAR AND DRY AIR ARE EXPECTED TO PREVENT REDEVELOPMENT. INDEED, MODELS AGREE THAT 14W WILL ARRIVE IN THE SEA OF JAPAN IN A STATE OF SUCH DISREPAIR THAT ITS STRUCTURE WILL UNRAVEL, RESULTING IN DISSIPATION IN AROUND 48 HOURS WITHIN AN UNFAVORABLE ENVIRONMENT. MODEL DISCUSSION: PHYSICS-BASED AND AI-BASED MODEL TRACK GUIDANCE HAS COME INTO TIGHTER AGREEMENT OVER THE PAST SIX HOURS AND CONNOTES HIGH CONFIDENCE IN THE TRACK FORECAST. THE JTWC FORECAST TRACK LEANS TOWARD THE SOUTHERN HALF OF THE GUIDANCE ENVELOPE THROUGH 12 HOURS, THEN CLOSE TO THE MULTI-MODEL CONSENSUS THEREAFTER. INTENSITY GUIDANCE IS ALSO IN TIGHT AGREEMENT, AND THE JTWC INTENSITY FORECAST IS MADE WITH HIGH CONFIDENCE. FORECAST CONFIDENCE: TRACK 0…

FIFTEEN (WP152026)

Type: TD Max Wind: 25 kt Min Pressure: 997 hPa Position: 28.4, 160.8 Basin: West Pacific
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.

Streamline Wind Map

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.

TC Drift Path Map

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: E (90°), 11.7 kt   |   Gust: 13.6 kt

Pressure: 30.12 rising   |   Air Temp: 85.3 °F

Water Temp: 85.8 °F   |   Dew Point: 80.6 °F

Swell: 0.7 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.

US National Radar Loop

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.

Satellite

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.

GOES IR Band 13

Most recent GOES Band 13 image. Provided by NOAA/NESDIS/STAR.