🚨 South Shore Bays from Jones Inlet through Shinnecock Bay; Fire Island Inlet NY to Moriches Inlet NY out 20 NM; Sandy Hook NJ to Fire Island Inlet NY out 20 NM; Waters from Fire Island Inlet NY to Moriches Inlet NY from 20 to 60 NM; Waters from Sandy Hook NJ to Fire Island Inlet NY out 20 to 60 NM: Marine Weather Statement issued August 23 at 7:32AM EDT by NWS Upton NY 🚨 Fisher; Nolan; Sterling; Coke; Runnels; Tom Green; Concho; Haskell; Throckmorton; Jones; Shackelford; Taylor; Callahan; Coleman; Brown; McCulloch; San Saba; Mason: Heat Advisory issued August 23 at 6:28AM CDT until August 23 at 7:00PM CDT by NWS San Angelo TX 🚨 Montgomery: None 🚨 Coastal waters from Sandy Hook to Manasquan Inlet NJ out 20 NM; Coastal waters from Manasquan Inlet to Little Egg Inlet NJ out 20 NM; Waters from Sandy Hook NJ to Manasquan Inlet NJ from 20 to 40 NM; Waters from Manasquan Inlet NJ to Little Egg Inlet NJ from 20 to 60 NM: Special Marine Warning issued August 23 at 7:24AM EDT until August 23 at 7:45AM EDT by NWS Mount Holly NJ 🚨 Waters from Oregon Inlet to Cape Hatteras NC from 20 to 60 NM: Special Marine Warning issued August 23 at 7:24AM EDT until August 23 at 8:30AM EDT by NWS Newport/Morehead City NC 🚨 Bronx, NY; Kings, NY; Nassau, NY; New York, NY; Queens, NY; Westchester, NY: Flash Flood Warning issued August 23 at 7:21AM EDT until August 23 at 9:15AM EDT by NWS Upton NY 🚨 Apalachee Bay or Coastal Waters From Keaton Beach to Ochlockonee River Fl out to 20 Nm; Coastal Waters From Ochlockonee River to Apalachicola FL out to 20 Nm; Coastal waters from Suwannee River to Keaton Beach out 20 NM; Waters from Suwannee River to Apalachicola FL from 20 to 60 NM: Special Marine Warning issued August 23 at 7:05AM EDT until August 23 at 8:30AM EDT by NWS Tallahassee FL 🚨 Chautauqua, NY: Flash Flood Warning issued August 23 at 7:03AM EDT until August 23 at 11:00AM EDT by NWS Buffalo NY 🚨 Clarence Strait: Small Craft Advisory issued August 23 at 3:02AM AKDT until August 24 at 7:00AM AKDT by NWS Juneau AK 🚨 Clarence Strait: Small Craft Advisory issued August 23 at 3:02AM AKDT until August 24 at 5:00AM AKDT by NWS Juneau AK
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.
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 230900
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TYPHOON 17W (SAUDEL) WARNING NR 020//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 21.9N 140.9E
INITIAL INTENSITY: 110 KTS
GEOGRAPHIC REFERENCE: 768 NM EAST-SOUTHEAST OF KADENA AB
MOVEMENT PAST 6 HOURS: WEST-NORTHWESTWARD AT 14 KTS
SIGNIFICANT WAVE HEIGHT: 45 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS TYPHOON 17W
(SAUDEL) WITH A SLIGHTLY RAGGED EYE AS THE SYSTEM CONTINUES TO UNDERGO
AN EYEWALL REPLACEMENT CYCLE (ERC) WHICH HAS STALLED FURTHER
INTENSIFICATION. THE MSI ALSO SHOWS A STRONG BAND OF CONVECTION
WRAPPING INTO THE CENTER ALONG THE WESTERN PERIPHERY OF THE SYSTEM.
THE ERC WAS CONFIRMED BY A 230422Z AMSR2 36 GHZ MICROWAVE IMAGE, WHICH
SHOWED A CLEAR MOAT FEATURE SURROUNDING THE INNER EYEWALL. THE AMSR2
IMAGE ALSO REVEALED THAT THE OUTER EYEWALL IS BECOMING MORE DOMINANT,
HINTING THAT THE ERC IS WELL UNDERWAY. THE INITIAL POSITION IS PLACED
WITH HIGH CONFIDENCE BASED ON THE EYE IN ANIMATED MSI AND
EXTRAPOLATION FROM THE AMSR2 IMAGE. THE INITIAL INTENSITY OF 110 KTS
IS ASSESSED WITH MEDIUM CONFIDENCE BASED ON THE AGENCY DVORAK FIXES
AND CIMSS INTENSITY ESTIMATES LISTED BELOW. ENVIRONMENTAL ANALYSIS
INDICATES THAT 17W IS IN A FAVORABLE ENVIRONMENT CHARACTERIZED BY
STRONG RADIAL OUTFLOW ALOFT, LOW (5-10 KTS) VERTICAL WIND SHEAR, AND
WARM (29-30 C) SEA SURFACE TEMPERATURES.
INITIAL WIND RADII BASIS: OBJECTIVE BEST TRACK
CURRENT STEERING MECHANISM: SOUTHWESTERN PERIPHERY OF AN ELONGATED
SUBTROPICAL RIDGE (STR) POSITIONED TO THE NORTHEAST
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T6.0 - 115 KTS
RJTD: T5.5 - 102 KTS
RCTP: T6.0 - 115 KTS
KNES: T5.5 - 102 KTS
CIMSS SATCON: 114 KTS AT 230600Z
CIMSS ADT: 112 KTS AT 230600Z
CIMSS AIDT: 105 KTS AT 230600Z
CIMSS D-MINT: 115 KTS AT 230417Z
CIMSS D-PRINT: 109 KTS AT 230600Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: FAVORABLE
VWS: 5-10 KTS
SST: 29-30 CELSIUS
OUTFLOW: STRONG RADIAL
OTHER FACTORS: ONGOING EYEWALL REPLACEMENT CYCLE
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: TY 17W IS FORECAST TO CONTINUE TRACKING WEST-
NORTHWESTWARD, ALONG THE SOUTHWESTERN PERIPHERY OF THE STR TO THE
NORTHEAST THROUGH TAU 24. NEAR TAU 24, THE STR IS EXPECTED TO MERGE
WITH A SEPARATE STR CENTERED OVER SOUTHERN JAPAN, WHICH WILL KEEP 17W
ON A WEST-NORTHWESTWARD TRAJECTORY THROUGH TAU 60. LANDFALL OVER
NORTHERN OKINAWA IS FORECAST TO OCCUR RIGHT AROUND TAU 60. AFTER TAU
60, TRACK SPEEDS ARE EXPECTED TO SLOW AS THE RIDGING TO THE NORTH
PROPAGATES EASTWARD AND THE STEERING INFLUENCE TRANSITIONS TO A STR
CENTERED OVER EASTERN CHINA. 17W IS THEN FORECAST TO BEGIN TRACKING
WEST-SOUTHWESTWARD, ALONG THE SOUTHEASTERN EXTENT OF THAT STR THROUGH
THE REMAINDER OF THE FORECAST PERIOD. IN TERMS OF INTENSITY, 17W IS
NOW FORECAST TO MAINTAIN ITS CURRENT INTENSITY OF 110 KTS THROUGH TAU
36 AS THE SYSTEM ATTEMPTS TO RECOVER FROM THE ONGOING ERC. 17W IS NOW
ALSO ENTERING WATERS CONTAINING A LOWER OCEAN HEAT CONTENT (OHC),
WHICH WILL ALSO SLIGHTLY HINDER THE CHANCES FOR REDEVELOPMENT AFTER
THE ERC COMPLETES. AFTER TAU 36, NORTHWESTERLY SHEAR AND DRY AIR
ENTRAINMENT FROM THE WEST IS EXPECTED TO INCREASE, CAUSING 17W TO
GRADUALLY WEAKEN AS IT APPROACHES OKINAWA. ONCE THE SYSTEM ENTERS THE
EAST CHINA SEA, NORTHERLY SHEAR INDUCED BY THE STRONG RIDGE OVER CHINA
WILL CAUSE FURTHER WEAKENING THROUGH THE REMAINDER OF THE FORECAST
PERIOD.
MODEL DISCUSSION: MODEL TRACK GUIDANCE REMAINS IN GOOD AGREEMENT
THROUGH TAU 72 W…
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 230900
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 18W (NARRA) WARNING NR
011//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 20.6N 108.1E
INITIAL INTENSITY: 35 KTS
GEOGRAPHIC REFERENCE: 126 NM EAST OF HANOI, VIETNAM
MOVEMENT PAST 6 HOURS: SOUTHEASTWARD AT 01 KTS
SIGNIFICANT WAVE HEIGHT: 12 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS TROPICAL
STORM 18W (NARRA) WITH A PARTIALLY EXPOSED LOW-LEVEL CIRCULATION
CENTER (LLCC) AND DEEP CONVECTION CONFINED TO THE WESTERN
PERIPHERY, CLOSE TO THE COAST. A 230610Z AMSR2 89 GHZ MICROWAVE
IMAGE REVEALED DEFINED LOW-LEVEL CLOUDS TIGHTLY WRAPPING INTO THE
CENTER, SUPPORTING THE INITIAL POSITION WITH HIGH CONFIDENCE. THE
INITIAL INTENSITY OF 35 KTS IS ASSESSED WITH HIGH CONFIDENCE BASED
ON THE AGREEMENT OF T2.5 FROM ALL FIXING AGENCIES. ENVIRONMENTAL
ANALYSIS INDICATES THAT 18W IS IN A MARGINALLY FAVORABLE
ENVIROMENT CHARACTERIZED BY MODERATE EQUATORWARD OUTFLOW ALOFT,
LOW TO MODERATE (15-20 KTS) NORTHEASTERLY VERTICAL WIND SHEAR, AND
VERY WARM (30-31 C) SEA SURFACE TEMPERATURES.
INITIAL WIND RADII BASIS: 230213Z METOP-B ASCAT SCATTEROMETER DATA
CURRENT STEERING MECHANISM: A COMPETING STEERING PATTERN WITH A
NEAR EQUATORIAL RIDGE (NER) TO THE SOUTH AND A SUBTROPICAL RIDGE
(STR) TO THE NORTH
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.5 - 35 KTS
RJTD: T2.5 - 35 KTS
RCTP: T2.5 - 35 KTS
KNES: T2.5 - 35 KTS
DEMS: T2.5 - 35 KTS
CIMSS ADT: 39 KTS AT 230610Z
CIMSS AIDT: 42 KTS AT 230610Z
CIMSS D-MINT: 36 KTS AT 230601Z
CIMSS D-PRINT: 39 KTS AT 230610Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINALLY FAVORABLE
VWS: 15-20 KTS
SST: 30-31 CELSIUS
OUTFLOW: MODERATE EQUATORWARD
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 18W IS FORECAST TO DRIFT SLOWLY SOUTHWARD
OVER THE NEXT 24 HOURS AS IT REMAINS PLACED WITHIN A COMPETING
STEERING ENVIRONEMENT. THE ACTUAL TRACK OF 18W IS LIKELY TO BE
ERRATIC DURING THIS TIME, WHICH IS NOT CAPTURED BY THE JTWC
FORECAST. AROUND TAU 36, THE NER TO THE SOUTH IS EXPTECTED TO BUILD
TO THE SOUTHEAST OF 18W, CAUSING IT TO MAKE AN EASTWARD AND THEN
NORTHWARD TURN TOWARD THE SOUTHERN COAST OF CHINA. IN TERMS OF
INTENSITY, 18W IS FORECAST TO MAINTAIN ITS CURRENT INTENSITY OF 35
KTS THROUGH TAU 24 AS THE SHEAR REMAINS RELATIVELY LOW. AFTER TAU
24, NORTHEASTERLY SHEAR WILL INCREASE, CAUSING THE SYSTEM TO BEGIN
ON A WEAKENING TREND AS IT APPROACHES THE COAST OF CHINA. 18W IS
THEN FORECAST TO QUICKLY DISSIPATE AFTER MAKING LANDFALL AROUND TAU
72.
MODEL DISCUSSION: MODEL TRACK GUIDANCE CONTINUES TO BE IN POOR
AGREEMENT UNDER THE EFFECTS OF THE COMPETING STEERING ENVIRONMENT.
MODELS GENERALLY SHOW A SOUTHWARD TRACK THROUGH TAU 24 FOLLOWED BY
A POLEWARD TURN, HOWEVER THERE IS SIGNIFICANT SPREAD THROUGHOUT THE
ENTIRE FORECAST DURATION. THE JTWC TRACK FORECAST IS PLACED CLOSER
TO THE ECMWF AND EXPERIMENTAL GOOGLE DEEPMIND ENSEMBLE MEANS WITH
LOW CONFIDENCE. INTENSITY GUIDANCE AGREES ON A STEADY INTENSITY
THROUGH TAU 24 FOLLOWED BY GRADUAL WEAKENING THROUGH TAU 72 WITH NO
SIGNIFICANT OUTLIERS. THE JTWC INTENSITY FORECAST CLOSELY FOLLOWS
THE CONSENSUS WITH MEDIUM CONFIDENCE.
FORECAST CONFIDENCE:
TRACK 00-72 HR: LOW
INTENSITY 00-72 HR: MEDIUM//
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.
WDPN33 PGTW 230900
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL DEPRESSION 19W (NINETEEN)
WARNING NR 004//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 13.4N 135.9E
INITIAL INTENSITY: 30 KTS
GEOGRAPHIC REFERENCE: 267 NM NORTHWEST OF YAP
MOVEMENT PAST 6 HOURS: NORTH-NORTHWESTWARD AT 08 KTS
SIGNIFICANT WAVE HEIGHT: 12 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS A FULLY
EXPOSED LOW-LEVEL CIRCULATION CENTER (LLCC) ASSOCIATED WITH TROPICAL
DEPRESSION (TD) 19W (NINETEEN) ACCELERATING NORTHEASTWARD. DEEP
CONVECTION HAS BEEN DISPLACED TO THE SOUTHWEST AS A RESULT OF STRONG
GRADIENT FLOW IN WHICH THE LLCC IS CURRENTLY EMBEDDED, MULTIPLIED BY
10-15 KT VERTICAL WIND SHEAR (VWS) FROM THE NORTHEAST. ADDITIONAL
ENVIRONMENTAL ANALYSIS REVEALS MARGINAL CONDITIONS FOR FURTHER
DEVELOPMENT. SEA SURFACE TEMPERATURES (SST) REMAIN WARM (29-30 C) AND
OUTFLOW IS ENHANCED BY A MODERATE EQUATORWARD CHANNEL. WHILE
PERSISTENT TROPOSPHERIC MOISTURE IS HIGHLY CONCENTRATED WITHIN THE
WESTERN QUADRANT, SIGNIFICANT DRY-AIR INTRUSION EMBEDDED TO THE EAST
AND NORTHEAST CONTINUES TO ENVELOPE THE SYSTEM. STRUCTURALLY, TD 19W
IS BECOMING MORE ELONGATED AS WITNESSED BY 230420Z GW1 AMSR2 MICROWAVE
IMAGERY AND SUPPORTED BY AN EARLIER (230057Z) METOP-C ASCAT PASS. THE
INITIAL POSITION IS ASSESSED WITH HIGH CONFIDENCE BASED ON VISIBLE
IMAGERY OF THE FULLY EXPOSED LLCC. THE INITIAL INTENSITY OF 30 KTS IS
ALSO ASSESSED WITH HIGH CONFIDENCE BASED ON A 230230Z OSCAT PASS, AND
THE AUTOMATED AND AGENCY ESTIMATES LISTED BELOW.
INITIAL WIND RADII BASIS: NOT APPLICABLE (THERE ARE NO INITIAL WIND
RADII).
CURRENT STEERING MECHANISM: NEAR-EQUATORIAL RIDGE (NER) TO THE
SOUTHEAST AND LOW-LEVEL SOUTHWESTERLIES
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T2.5 - 35 KTS
RJTD: T1.5 - 25 KTS
KNES: T2.5 - 35 KTS
CIMSS SATCON: 39 KTS AT 230610Z
CIMSS ADT: 34 KTS AT 230610Z
CIMSS AIDT: 31 KTS AT 230610Z
CIMSS D-MINT: 27 KTS AT 230500Z
CIMSS D-PRINT: 31 KTS AT 230640Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: MARGINAL
VWS: 10-15 KTS
SST: 29-30 CELSIUS
OUTFLOW: MODERATE EQUATORWARD
OTHER FACTORS: DRY AIR ENTRAINMENT THROUGHOUT THE EASTERN
SEMICIRCLE
ANALYSIS CONFIDENCE:
INITIAL POSITION: HIGH
INITIAL INTENSITY: HIGH
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: TD 19W IS CURRENTLY ACCELERATING NORTHEASTWARD,
DRIVEN BY THE STEERING INFLUENCE OF A NER ANCHORED TO THE EAST-
SOUTHEAST AND ENHANCED BY LOW-LEVEL SOUTHWESTERLIES. AROUND TAU 24,
THE DOMINANT STEERING INFLUENCE WILL SHIFT TO A SUBTROPICAL RIDGE
POSITIONED TO THE NORTHEAST, VEERING TD 19W NORTHWARD AND
NORTHWESTWARD ALONG THE SUBSIDED WAKE OF TYPHOON 17W (SAUDEL). WHILE
THE VWS IS EXPECTED TO REMAIN INITIALLY LOW, MODEL GUIDANCE INDICATES
SIGNIFICANT UPTICK JUST PRIOR TO TAU 24, WHICH COMBINED WITH
INCREASING ENTRAINMENT OF DRY AIR INTO THE CORE WILL INITIATE A
WEAKENING TREND, DEPRESSING INTENSITY TO 20-25 KTS BY TAU 36. TOWARDS
TAU 48, TD 19W WILL STRUGGLE TO PRESERVE ITS VERTICAL STRUCTURE AS IT
ENTERS THE REGION OF SHEARED TAIL END WINDS OF TYPHOON 17W.
ACCORDINGLY, COMPLETE DISSIPATION OVER OPEN WATER IS PROJECTED BY TAU
48, ALTHOUGH AN ACCELERATED DECAY TIMELINE REMAINS VIABLE SHOULD
INCREASED VERTICAL WIND SHEAR AND DRY AIR ADVECTION BE MORE PRONOUNCED
AS CURRENTLY MODELED.
MODEL DISCUSSION: NUMERICAL MODEL GUIDANCE EXHIBITS FAIR INITIAL
CONSISTENCY, EVIDENCED BY A CONSTRAINED 115 NM CROSS-TRACK SPREAD AT
TAU 48, WITH ALL MAJOR GLOBAL AND MESOSCALE SYSTEMS RESOLVING COHERENT
MOTION UNDER CURRENT STEERING FORCING. WHILE THE OFFICIAL JTWC…
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: SSW (210°), 5.8 kt | Gust: 7.8 kt
Pressure: 29.99 | Air Temp: 84.9 °F
Water Temp: 87.1 °F | Dew Point: 79.0 °F
Swell: 1.3 ft | Wind Wave: 0.7 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.