🚨 Montgomery: None 🚨 Maricopa, AZ: Flash Flood Warning issued September 29 at 4:31AM MST until September 29 at 9:30AM MST by NWS Phoenix AZ 🚨 Yavapai, AZ: Flash Flood Warning issued September 29 at 4:30AM MST until September 29 at 7:45AM MST by NWS Flagstaff AZ 🚨 Bering Sea Offshore West of 180 and East of the International Date Line: Gale Warning issued September 29 at 3:30AM AKDT until September 30 at 5:00PM AKDT by NWS Anchorage AK 🚨 Seguam to Adak Pacific Side out to 15 NM: Small Craft Advisory issued September 29 at 3:30AM AKDT until September 30 at 5:00PM AKDT by NWS Anchorage AK 🚨 Kiska to Attu Bering Side: Small Craft Advisory issued September 29 at 3:30AM AKDT until September 30 at 5:00PM AKDT by NWS Anchorage AK 🚨 Saint Matthew Island Waters: Small Craft Advisory issued September 29 at 3:30AM AKDT until September 30 at 5:00AM AKDT by NWS Anchorage AK 🚨 Seguam to Adak Pacific Side from 15 to 75 NM: Small Craft Advisory issued September 29 at 3:30AM AKDT until September 30 at 5:00PM AKDT by NWS Anchorage AK 🚨 Sitkinak to Castle Cape from 15 to 100 NM: Small Craft Advisory issued September 29 at 3:30AM AKDT until September 29 at 5:00PM AKDT by NWS Anchorage AK 🚨 Sitkinak to Castle Cape out to 15 NM: Small Craft Advisory issued September 29 at 3:30AM AKDT until September 29 at 5:00PM AKDT by NWS Anchorage 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.
ZCZC MIATCDAT1 ALL
TTAA00 KNHC DDHHMM
Tropical Storm Fay Discussion Number 37
NWS National Hurricane Center Miami FL AL062026
500 AM AST Tue Sep 29 2026
Proxy-visible satellite imagery shows that the convection around Fay
has increasingly become more sheared in the last several hours.
Infrared imagery does still show some of the convection has cloud
tops near -70 C. In addition, the most recent TAFB Dvorak fix was
2.0/30 KT, and the objective intensity estimates from UW-CIMSS are
in the range of 33-43 kt. Therefore, the initial intensity has been
held at 35 kt for this advisory.
The storm is still moving toward the southwest with an estimated
initial motion of 235/11 kt. Fay is expected to keep a general
southwestward to west-southwestward motion for the next couple of
days as the cyclone is guided by the flow along the southern
periphery of a mid-level ridge situated over the central Atlantic.
The current NHC track forecast is almost identical to the previous
one with just a few minor adjustments based on the HCCA and GDMI
forecast aids.
With the convection expected to pulsate for the next couple of days,
the intensity will also fluctuate as well. However that convection
will likely become increasingly separated from the center as the
SHIPS guidance indicates increasing vertical wind shear over the
couple of days. Based on the global models, Fay will struggle to
maintain deep convection as it moves into a more stable air mass and
an area of upper-level convergence. The current NHC intensity
forecast is based on the HCCA and GDMI forecast guidance and Fay is
still expected to become a post-tropical cyclone in a day or so.
The global models show the system degenerating into a trough
afterwards.
FORECAST POSITIONS AND MAX WINDS
INIT 29/0900Z 25.0N 46.8W 35 KT 40 MPH
12H 29/1800Z 24.0N 48.2W 30 KT 35 MPH
24H 30/0600Z 23.1N 50.2W 30 KT 35 MPH
36H 30/1800Z 22.7N 52.2W 30 KT 35 MPH...POST-TROP/REMNT LOW
48H 01/0600Z 22.6N 54.0W 30 KT 35 MPH...POST-TROP/REMNT LOW
60H 01/1800Z...DISSIPATED
$$
Forecaster Katz
NNNN
ZCZC MIATCDAT3 ALL
TTAA00 KNHC DDHHMM CCA
Tropical Storm Hanna Discussion Number 4...Corrected
NWS National Hurricane Center Miami FL AL082026
500 AM AST Tue Sep 29 2026
Corrected numerical value in second paragraph
Satellite imagery shows Hanna's convective structure has not changed
much and still displays an exposed low-level center due to strong
westerly vertical wind shear. The deepest convection remains
displaced east of the tropical storm's center. A 0225 UTC OSCAT
scatterometer pass revealed an asymmetric wind field. The latest
TAFB Dvorak fix was T2.0/30 kt, slightly below objective estimates
ranging between 34 and 43 kt. Based on a blend of these data, the
initial intensity is held at 40 kt.
The initial motion continues east-southeastward at 115/13 kt. Hanna
is embedded in the flow between a longwave trough to its northeast
and a larger subtropical ridge to its south. This synoptic pattern
should result in a continued east-southeastward motion over the next
24 h or so, with a gradual slowdown in forward speed as the
mid-latitude trough leaves Hanna behind. Much of the track guidance
then shows a slightly quicker east-northeastward motion after the
cyclone becomes vertically shallow and influenced by a low-level
ridge centered south of the Azores. The updated NHC track forecast
was largely unchanged from the previous advisory, roughly in between
the simple (TVCN) and corrected consensus (HCCA) aids.
Tropical Storm Hanna is forecast to persist in a moisture-starved
environment, with moderate to strong vertical wind shear prevailing
over the next 48 to 72 h. However, some near-term fluctuations in
intensity are possible during this period as intermittent bursts of
deep convection well east of the center may allow for slight
intensification. Thereafter, Hanna is expected to be devoid of deep
convection around the 60 h mark, degenerating into a post-tropical
cyclone at that time.
FORECAST POSITIONS AND MAX WINDS
INIT 29/0900Z 35.2N 46.2W 40 KT 45 MPH
12H 29/1800Z 34.4N 44.6W 45 KT 50 MPH
24H 30/0600Z 33.9N 43.5W 40 KT 45 MPH
36H 30/1800Z 34.2N 42.4W 40 KT 45 MPH
48H 01/0600Z 34.9N 40.5W 35 KT 40 MPH
60H 01/1800Z 35.8N 38.3W 30 KT 35 MPH...POST-TROP/REMNT LOW
72H 02/0600Z 37.0N 35.9W 30 KT 35 MPH...POST-TROP/REMNT LOW
96H 03/0600Z...DISSIPATED
$$
Forecaster Pierce/Pasch
NNNN
ZCZC MIATCDEP2 ALL
TTAA00 KNHC DDHHMM CCA
Hurricane Polo Discussion Number 35...Corrected
NWS National Hurricane Center Miami FL EP172026
200 AM MST Tue Sep 29 2026
Corrected for Key Message number 1.
Polo made landfall around 06Z along the west coast of Baja
California Sur, just south of the small town of Las Barrancas.
Several microwave fixes received after the 03Z advisory went out
(WSF-M, SAR, and two ASCAT passes) all indicated that center of Polo
was a bit farther south than was estimated at 03Z. There is some
uncertainty in what the intensity was at landfall, but given all the
data we have received, it is likely that Polo was a category 2
hurricane at the time of landfall with maximum winds in the 90-95
kt range. The center has been over land for about 3 hours now, and
it is estimated that the maximum winds have come down to about 70
kt.
The hurricane is moving northeastward, or 30 degrees at 9 kt. A
significant increase in forward speed is expected this morning as a
mid- to upper-level trough amplifies over the southwestern U.S.
This track should take the system inland over the Mexican state of
Sonora late this morning. The track forecast is a little slower
compared to the previous forecast for the first 12 hours, mainly
due to the slower initial motion.
Some slight additional weakening is likely for another couple of
hours while the center of Polo remains over land. When the center
emerges over the Gulf of California, atmospheric and oceanic
conditions could allow for Polo to maintain its intensity. The
latest HAFS models show landfall in Sonora around 60 kt, but it is
possible that Polo could still be a hurricane when it reaches that
state. After landfall, rapid weakening is expected over the
rugged terrain of northwestern Mexico. Although Polo is likely to
dissipate between the hour 12 and 24 points, a 24 hour point is
included for continuity.
Polo's remnant vorticity will likely interact and phase with a
strong cutoff low digging into the Four Corners region of the U.S.
on Tuesday and Wednesday, contributing to heavy rainfall, flash
flooding, and gusty winds in the southwestern U.S. and southern
Plains. See products issued by the Weather Prediction Center and
local National Weather Service offices for more information.
Key Messages:
1. Polo is still bringing hurricane-force winds to Baja California
Sur, and residents there should remain in a safe shelter through
this morning. Hurricane and tropical storm conditions will spread
into mainland Mexico early today. A dangerous storm surge is
expected in areas of onshore winds.
2. Heavy rainfall associated with Polo will impact Baja California
Sur along with southern and central portions of Sonora today. This
rainfall is expected to produce life-threatening flooding and
mudslides, especially in areas of steep terrain. Moisture from Polo
will support heavy rainfall and flooding potential across the
Southwest U.S. into the Southern High Plains today into early
Wednesday.
3. Even after Polo dissipates, its mid-level remnants may produce
strong gusty winds well inland over the higher terrain of northwest
Mexico, southern New Mexico, and far western Texas.
4. Dangerous surf and rip currents are likely along portions of the
northwest coast of Mexico and Baja California for the next day or
so.
FORECAST POSITIONS AND MAX WINDS
INIT 29/0900Z 26.2N 111.9W 70 KT 80 MPH
12H 29/1800Z 28.4N 110.1W 55 KT 65 MPH...INLAND
24H 30/0600Z 31.7N 106.8W 30 KT 35 MPH...POST-TROP/INLAND
36H 30/1800Z...DISSIPATED
$$
Forecaster Hagen
NNNN
ZCZC MIATCDEP3 ALL
TTAA00 KNHC DDHHMM
Tropical Storm Rachel Discussion Number 9
NWS National Hurricane Center Miami FL EP182026
300 AM CST Tue Sep 29 2026
Rachel has been exhibiting a pattern of bursting very deep
convection over the past several hours with cloud tops as cold as
-90 deg C. However, the deep convective area has a rather
shapeless appearance on satellite imagery, and is lacking
convective banding features. The storm continues to experience
some north-northeasterly vertical wind shear. Observations from a
NOAA Hurricane Hunter Tail Doppler radar research mission indicate
that the system is becoming more vertically aligned. Nonetheless,
since the system's satellite signature indicates arrested
development, the advisory intensity is held at 50 kt which is a
little above the latest Dvorak estimate from TAFB.
Blending center position estimates from the NOAA aircraft along
with geostationary and microwave satellite-base center fixes, the
motion estimate is 300/10 kt which is about the same as before.
Rachel should move along the southwestern side of a mid-level ridge
with a more northwestward motion being induced by a 500 mb cutoff
low over the southwestern United States during the next few days.
By late week, the trough is forecast to lift out and the ridge
should become reestablished to the north, with Rachel expected to
resume a west-northwestward motion by around 72 hours. The
official track forecast is slightly south of the one from the
previous advisory but on the northern side of the track guidance
envelope.
Rachel should be moving through a favorable atmospheric
thermodynamic environment and over generally warm sea surface
temperatures during the next several days. Assuming that the
vertical wind shear does not become too prohibitive, strengthening
is forecast. There is a possibility that the system's
intensification could be slightly inhibited by some cooler waters
due to the wake of Hurricane Polo. The official intensity forecast
is close to the simple intensity model consensus, but the corrected
consensus guidance is somewhat higher, as noted in the previous
advisory discussion.
Key Messages:
1. Although the core of Rachel is forecast to remain offshore of
Mexico, tropical-storm-force winds are expected along a portion of
the coast of southwestern Mexico in the Tropical Storm Warning area
today. Tropical storm conditions are possible in the watch area
tonight or on Wednesday.
2. Outer bands from Rachel will bring locally heavy rainfall to
portions of coastal southwest Mexico through Thursday. This rainfall
may produce areas of flooding and mudslides, especially in regions
of steep terrain.
3. Large waves could produce life-threatening surf and rip current
conditions along portions of the southwestern coast of Mexico during
the next several days.
FORECAST POSITIONS AND MAX WINDS
INIT 29/0900Z 14.7N 104.3W 50 KT 60 MPH
12H 29/1800Z 15.7N 105.4W 55 KT 65 MPH
24H 30/0600Z 17.1N 106.8W 65 KT 75 MPH
36H 30/1800Z 18.4N 108.1W 75 KT 85 MPH
48H 01/0600Z 19.3N 109.1W 80 KT 90 MPH
60H 01/1800Z 19.8N 109.7W 85 KT 100 MPH
72H 02/0600Z 20.2N 110.3W 85 KT 100 MPH
96H 03/0600Z 20.7N 111.6W 85 KT 100 MPH
120H 04/0600Z 21.1N 113.5W 85 KT 100 MPH
$$
Forecaster Pasch
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 290900
MSGID/GENADMIN/JOINT TYPHOON WRNCEN PEARL HARBOR HI//
SUBJ/PROGNOSTIC REASONING FOR TROPICAL STORM 25W (SURIGAE) WARNING NR
025//
RMKS/
1. FOR METEOROLOGISTS.
2. 6 HOUR SUMMARY AND ANALYSIS.
SUMMARY:
INITIAL POSITION: 29.0N 135.0E
INITIAL INTENSITY: 50 KTS
GEOGRAPHIC REFERENCE: 447 NM SOUTHWEST OF YOKOSUKA, JAPAN
MOVEMENT PAST 6 HOURS: EAST-NORTHEASTWARD AT 10 KTS
SIGNIFICANT WAVE HEIGHT: 22 FEET
SATELLITE ANALYSIS, INITIAL POSITION AND INTENSITY DISCUSSION:
ANIMATED MULTISPECTRAL SATELLITE IMAGERY (MSI) DEPICTS A FULLY
EXPOSED LOW-LEVEL CIRCULATION CENTER (LLCC) DISPLACED WEST OF
FLARING DEEP CONVECTION ANCHORED ALONG LOW-LEVEL CONVERGENT
ASYMPTOTES IN THE EASTERN SEMICIRCLE. A 290245Z AMSR3 COLOR-ENHANCED
89GHZ MICROWAVE PASS REVEALS THE VORTEX IS SHALLOW AND STRONGLY
DECOUPLED, WITH DEEP CONVECTIVE CORES RESTRICTED TO THE DOWN-SHEAR
EASTERN FLANK. SYNOPTICALLY, THE SOUTHWESTERN EXTENT OF A STATIONARY
FRONTAL BOUNDARY IS LOCATED APPROXIMATELY 175 NM NORTH OF THE LLCC.
ANIMATED WATER VAPOR IMAGERY AND ATMOSPHERIC MOTION VECTORS (AMVS)
INDICATE AN UPPER-TROPOSPHERIC JET AXIS OVER HONSHU ORIENTED PARALLEL
TO THE SURFACE BOUNDARY, IMPOSING MODERATE-TO-STRONG NORTHWESTERLY
SHEAR DIRECTLY ACROSS TS 25W. THE INITIAL POSITION IS ASSESSED WITH
HIGH CONFIDENCE BASED ON THE FULLY EXPOSED LLCC IN MSI. THE INITIAL
INTENSITY IS HELD AT 50 KNOTS, BIASED SLIGHTLY ABOVE OBJECTIVE
SATELLITE ESTIMATES (ADT/SATCON), BASED ON A BLEND OF DVORAK CURRENT
INTENSITY (CI) ASSESSMENTS AND RECENT SCATTEROMETER WINDS OF 45 KNOTS
ACCOUNTING. ENVIRONMENTAL CONDITIONS ARE UNFAVORABLE, CHARACTERIZED
BY HIGH VWS (20-25 KTS), RESTRICTED UPPER-LEVEL OUTFLOW, AND MID-
LEVEL DRY AIR INTRUSION, MARGINALLY OFFSET BY WARM SEA SURFACE
TEMPERATURES (SSTS).
INITIAL WIND RADII BASIS: SCATTEROMETER DATA
CURRENT STEERING MECHANISM: WESTERN FLANK OF A DEEP-LAYER
SUBTROPICAL RIDGE (STR) CENTERED TO THE EAST.
AGENCY DVORAK AND AUTOMATED FIXES:
PGTW: T3.5 - 55 KTS
RJTD: T4.5 - 77 KTS
RCTP: T3.0 - 45 KTS
CIMSS SATCON: 41 KTS AT 290426Z
CIMSS ADT: 45 KTS AT 290540Z
CIMSS AIDT: 43 KTS AT 290540Z
CIMSS D-MINT: 30 KTS AT 290427Z
CIMSS D-PRINT: 35 KTS AT 290540Z
FORECASTER ASSESSMENT OF CURRENT ENVIRONMENT: UNFAVORABLE
VWS: 20-25 KTS
SST: 28-29 CELSIUS
OUTFLOW: MODERATE EQUATORWARD
OTHER FACTORS: MID-LEVEL DRY AIR INTRUSION ALONG THE
NORTHWESTERN FLANK OF THE VORTEX.
ANALYSIS CONFIDENCE:
INITIAL POSITION: HIGH
INITIAL INTENSITY: MEDIUM
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 (TS) 25W WILL CONTINUE TO TRACK
NORTHEASTWARD ALONG THE NORTHWESTERN SIDE OF THE STR TO THE EAST,
RIDING POLEWARD JUST AHEAD OF THE STATIONARY FRONTAL BOUNDARY JUST
OFFSHORE OF HONSHU, THROUGH TAU 48. BETWEEN TAU 36 AND TAU 48, AS THE
CYCLONE APPROACHES THE LATITUDE OF YOKOSUKA, 25W WILL INTERACT
DIRECTLY WITH THE BAROCLINIC FRONTAL ZONE, PHASE WITH AN APPROACHING
POLAR SHORTWAVE TROUGH, AND COMMENCE EXTRATROPICAL TRANSITION (ETT)
ETT IS PROJECTED TO COMPLETE BY TAU 60, AT WHICH POINT THE SYSTEM
WILL BE RESTRUCTURED AS A COLD-CORE, ASYMMETRIC EXTRATROPICAL CYCLONE
COUPLED WITHIN THE FAVORABLE DIVERGENT RIGHT-ENTRANCE QUADRANT OF A
140-KNOT UPPER-LEVEL JET STREAK EAST OF HOKKAIDO. REGARDING
INTENSITY, 25W WILL SLOWLY WEAKEN OVER THE NEXT 12 HOURS, BUT
PERIODIC PULSES OF DEEP CONVECTION, FUELED BY THE WARM WATERS OF THE
KUROSHIO CURRENT, WILL PROVIDE ENOUGH ENERGY TO MAINTAIN THE
INTENSITY AT 40-45 KNOTS FROM TAU 12 THROUGH TAU 36. AS ETT ENSUES,
BAROCLINIC CYCLOGENESIS AND UPPER-LEVEL JET DIVERGENCE WILL ARREST
THE WEAKENING TREND AND INDUCE SECONDARY RE-INTENSIFICATION AS A
HYBRID/EXTRATROPICAL GALE BY TAU 60.
MODEL DISCUSSION: TRACK GUIDANCE EXHIBITS EXCE…
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: E (80°), 7.8 kt | Gust: 9.7 kt
Pressure: 29.89 steady | Air Temp: 83.7 °F
Water Temp: 86.4 °F | Dew Point: 76.3 °F
Swell: 1.0 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.