🚨 Kiowa; Clark; Comanche: Special Weather Statement issued August 6 at 7:31PM CDT by NWS Dodge City KS     🚨 Wayne; Mingo; Logan: Special Weather Statement issued August 6 at 8:30PM EDT by NWS Charleston WV     🚨 Bleckley; Laurens; Treutlen; Dodge: Special Weather Statement issued August 6 at 8:30PM EDT by NWS Peachtree City GA     🚨 Bleckley, GA; Dodge, GA; Pulaski, GA: Severe Thunderstorm Warning issued August 6 at 8:27PM EDT until August 6 at 9:00PM EDT by NWS Peachtree City GA     🚨 Guadalupe County: Special Weather Statement issued August 6 at 6:27PM MDT by NWS Albuquerque NM     🚨 Montgomery: None     🚨 Marion; Baxter; Searcy County Lower Elevations; Eastern, Central, and Southern Searcy County Higher Elevations: Special Weather Statement issued August 6 at 7:23PM CDT by NWS Little Rock AR     🚨 Swain; Graham; Macon: Special Weather Statement issued August 6 at 8:21PM EDT by NWS Greenville-Spartanburg SC     🚨 Pulaski; Wayne: Special Weather Statement issued August 6 at 8:20PM EDT by NWS Jackson KY     🚨 Marion; Baxter: Special Weather Statement issued August 6 at 7:20PM CDT by NWS Little Rock AR    

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: 00 UTC 07 Aug 2026

Active storms summary

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DOLPHIN (WP122026)

Type: HU Max Wind: 80 kt Min Pressure: 957 hPa Position: 26.9, 130.4 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.
WDPN31 PGTW 062100 MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI// SUBJ/PROGNOSTIC REASONING FOR TYPHOON 12W (DOLPHIN) WARNING NR 044// RMKS/ 1. FOR METEOROLOGISTS. 2. 6 HOUR SUMMARY AND ANALYSIS. SUMMARY: INITIAL POSITION: 26.9N 130.4E INITIAL INTENSITY: 80 KTS GEOGRAPHIC REFERENCE: 141 NM EAST OF KADENA AB MOVEMENT PAST 6 HOURS: WEST-NORTHWESTWARD AT 10 KTS SIGNIFICANT WAVE HEIGHT: 40 FEET SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION: ANIMATED ENHANCED INFRARED (EIR) SATELLITE IMAGERY DEPICTS DISCONTINUOUS DEEP CONVECTIVE BANDING SURROUNDING A COMPACT INNER CORE WITH A SMALL 10 NM RAGGED EYE. THE DEEP CONVECTION SURROUNDING THE INNER CORE THAT MAKES UP THE EYEWALL HAD BEEN ERODING ON THE WESTERN SIDE EARLIER BUT NOW APPEARS TO BE RECONSTITUTING WITHIN THE PAST FEW HOURS. A 061725Z AMSR-2 37 GHZ MICROWAVE IMAGE HIGHLIGHTS THE DISCONTINUOUS STRUCTURE OF THE CONVECTIVE BANDING AND THE WEAKNESS OF CONVECTION IN THE WESTERN SIDE OF THE CORE CONVECTION. THE INITIAL POSITION IS PLACED WITH HIGH CONFIDENCE BASED ON THE RAGGED EYE IN IR IMAGERY AND EXTRAPOLATION FROM THE MICROWAVE EYE IN THE AMSR-2 IMAGE. A 051300Z ASCAT-C WIND SPEED PRODUCT REVEALED THE NEARLY 500 NM DIAMETER EXTENT OF GALE FORCE WINDS SURROUNDING THE SYSTEM. NOTABLY, THE ASCAT-C IMAGE SHOWS THAT THE WIND FIELD IN THE SOUTHERN SEMICIRCLE HAS BECOME MORE HOMOGENEOUS AND LESS INTENSE THAN WHAT HAS BEEN OBSERVED OVER THE PAST FEW DAYS. THE INITIAL INTENSITY OF 80 KTS IS ASSESSED WITH MEDIUM CONFIDENCE BASED ON UNANIMOUS T4.5 DVORAK CURRENT INTENSITIES FROM THE FIXING AGENCIES, HEDGED SLIGHTLY HIGHER GIVEN THE LITTLE CHANGE IN OVERALL SATELLITE PRESENTATION. THE ENVIRONMENT IS CHARACTERIZED AS FAVORABLE, WITH WARM SEA SURFACE TEMPERATURES, LOW VERTICAL WIND SHEAR (VWS), AND EXCELLENT RADIAL OUTFLOW. INITIAL WIND RADII BASIS: PERSISTENCE CURRENT STEERING MECHANISM: SOUTHWESTERN FLANK OF A SUBTROPICAL RIDGE CENTERED OVER HONSHU AGENCY DVORAK AND AUTOMATED FIXES: PGTW: T4.5 - 77 KTS RJTD: T4.5 - 77 KTS RCTP: T4.5 - 77 KTS KNES: T4.5 - 77 KTS CIMSS SATCON: 73 KTS AT 061800Z CIMSS ADT: 61 KTS AT 061800Z CIMSS AIDT: 72 KTS AT 061800Z CIMSS D-MINT: 75 KTS AT 061749Z CIMSS D-PRINT: 74 KTS AT 061730Z FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE VWS: 5-10 KTS SST: 29-30 CELSIUS OUTFLOW: STRONG RADIAL 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) 12W (DOLPHIN) HAS CONTINUED ON A WOBBLING WEST-NORTHWESTWARD TRACK OVER THE PAST 6 HOURS UNDER THE STEERING INFLUENCE OF THE STR OVER HONSHU. THE SYSTEM IS FORECAST TO CONTINUE NEARLY DUE WESTWARD THROUGH TAU 60 AS THE STEERING RIDGE MIGRATES EAST AND A WEAKER RIDGE EXTENSION BUILDS IN FROM THE WEST. THE TRACK SPEED IS EXPECTED TO SLOW SLIGHTLY BETWEEN TAU 36-60 AS THE STEERING GRADIENT WEAKENS BETWEEN THE TWO RIDGE FEATURES. AFTER TAU 60, THE STEERING ENVIRONMENT GETS A BIT MORE COMPLICATED WITH THE PASSAGE OF A MIDLATITUDE TROUGH TO THE NORTH, INTRODUCING SOME UNCERTAINTY IN THE RECURVING TRACK. THE CPA TO KADENA AB AROUND 080900Z IS 42 NM, HOWEVER, THE EXPANSIVE WIND FIELD HAS ALREADY REACHED OKINAWA, WITH 40+ KT GUSTS OBSERVED AT RODN SINCE 1600Z. TY 12W IS EXPECTED TO MAKE LANDFALL IN EASTERN CHINA AROUND TAU 72 AS IT BEGINS TO RECURVE NORTHWESTWARD. THE INTENSITY IS FORECAST TO REMAIN STEADY AROUND 80 KTS UNTIL TAU 48, AFTER WHICH A STEADY WEAKENING TREND WILL BE INITIATED BY LOWER OCEAN HEAT CONTENT AND PROXIMITY TO MAINLAND CHINA. RAPID DISSIPATION IS EXPECTED AS THE SYSTEM RECURVES INLAND OVER EASTERN CHINA. MODEL DISCUSSION: MODEL TRACK GUIDANCE IS IN GOOD AGREEMENT ABOUT THE WESTWARD TRAJECTORY THROUGH TAU 60, THEN SPREADS …

96W (WP962026)

Type: TS Max Wind: 45 kt Min Pressure: 987 hPa Position: 28.2, 162.1 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 (80°), 11.7 kt   |   Gust: 13.6 kt

Pressure: 30.05 falling   |   Air Temp: 85.6 °F

Water Temp: 87.8 °F   |   Dew Point: 78.6 °F

Swell: 0.3 ft   |   Wind Wave: 1.6 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.