1967 North Atlantic hurricane season

Hurricane Beulah 1967

Hurricane Beulah is remembered in South Texas for extensive flooding and an extraordinary tornado outbreak. Before reaching the Rio Grande in September 1967, it had already crossed the Caribbean and Yucatán Peninsula through repeated periods of strengthening and weakening.

PEAK INTENSITYCategory 5
Image of Beulah 1967
United States Environmental Data Service. public domain Source
BEULAH: complete recorded track, Sep 5, 1967–Sep 24, 1967Recorded track from Sep 5, 1967 to Sep 24, 1967. Colors show the recorded wind category. The highlighted position follows the replay controls.NORTH AMERICACUBAAtlantic OceanSep 6, 12:00 AM UTCSep 7, 12:00 AM UTCSep 8, 12:00 AM UTCSep 9, 12:00 AM UTCSep 10, 12:00 AM UTCSep 11, 12:00 AM UTCSep 12, 12:00 AM UTCSep 13, 12:00 AM UTCSep 14, 12:00 AM UTCSep 15, 12:00 AM UTCSep 16, 12:00 AM UTCSep 17, 12:00 AM UTCSep 18, 12:00 AM UTCSep 19, 12:00 AM UTCSep 20, 12:00 AM UTCSep 21, 12:00 AM UTCSep 22, 12:00 AM UTCSep 23, 12:00 AM UTCSep 24, 12:00 AM UTCPeak: Category 5SEP 5SEP 24

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DepressionTropical stormCat 1Cat 2Cat 3Cat 4Cat 5Post-tropical
Wind speed 161 mphPressure 923 mb
09201009702001020mphmbSep 5Sep 11Sep 18Sep 24
Forward speed 9 mphCumulative ACE 35.40 10⁴ kt²
001022.52045mph10⁴ kt²Sep 5Sep 11Sep 18Sep 24
Maximum sustained wind161 mph

161 mph

Minimum recorded pressure923 hPa

Sep 19, 1967 during the tropical stage

Recorded track duration18.75 days

Full archive record, including non-tropical stages if present

Approximate track distance3,730 mi

Along the recorded center positions

STORM HISTORY

Across the Caribbean and Yucatán

Beulah developed east of Barbados and entered the Caribbean near Martinique. It strengthened rapidly south of Puerto Rico, where radar captured an entire eyewall replacement cycle: an outer ring of thunderstorms replaced the original inner eyewall.

The hurricane weakened markedly near Hispaniola under wind shear and the influence of land. It passed south of Jamaica, then recovered over the western Caribbean. Beulah crossed Cozumel and the Yucatán Peninsula before entering the Gulf of Mexico.

A Gulf peak before the Rio Grande

Rapid intensification over the Gulf brought Beulah to peak one-minute winds of 140 kt early on 20 September. It weakened before making landfall near the mouth of the Rio Grande later that day, bringing destructive conditions to northeastern Mexico and South Texas.

Beulah's slow movement inland prolonged the rain and produced severe flooding. The storm spawned 115 tornadoes across Texas, setting a tropical-cyclone tornado record that stood until 2004. At least 59 people died along its full path, and damage was estimated at US$234.6 million in 1967 values.

A longer-lived inland circulation

After stalling near Alice, Texas, the weakening circulation turned southwest across Mexico. Later reanalysis extended Beulah's history through 24 September, when it returned to the southern Gulf of Mexico as a tropical depression. That later continuation is included in the archived track.

Further reading

NOAA IBTrACS v04r01 historical track archive

Wikipedia, Hurricane Beulah

QUICK ANSWERS

Beulah in brief

What was Hurricane Beulah's highest wind speed?

161 mph, the highest one-minute sustained wind in its tropical stage, recorded on Sep 20, 1967, 12:00 AM UTC.

What category was Hurricane Beulah?

Category 5 at its peak on the Saffir–Simpson one-minute wind scale, first reaching Category 5 on Sep 19, 1967, 09:00 PM UTC. Other agencies classify storms differently.

What was Hurricane Beulah's lowest pressure?

923 mb, the minimum central pressure recorded during its tropical stage, on Sep 19, 1967, 06:00 PM UTC.

When did Hurricane Beulah occur?

The archived track runs from Sep 5, 1967, 12:00 PM UTC to Sep 24, 1967, 06:00 AM UTC, with the tropical stage from Sep 5, 1967, 12:00 PM UTC to Sep 24, 1967, 06:00 AM UTC.

Where did Hurricane Beulah form?

In the North Atlantic basin, in the 1967 season. Its first archived position is 13.4°N, 57°W on Sep 5, 1967, 12:00 PM UTC.

Did Hurricane Beulah make landfall?

The archive places its center over land at 2 recorded positions; the strongest is 127 mph on Sep 17, 1967, 05:00 AM UTC. Positions are six-hourly, so this is not a landfall chronology.

METHODOLOGY

Data sources and limitations

The map and summary are generated from NOAA's IBTrACS v04r01 archive. Wind and category use US-agency records; minimum pressure is calculated during the tropical stage, with the archive's pressure source retained. Category 5 refers to the Saffir–Simpson one-minute wind scale; local agencies may use different classifications. Coastlines use Natural Earth's 1:10m land data.

Track distance adds great-circle distances between consecutive observations, excluding gaps over 12 hours. This track has no gaps over 12 hours. The line shows the storm's center, not its size, rainfall or flood extent. Converted wind speeds are rounded to the nearest whole unit.

Archive retrieved

NOAA IBTrACS archive and Field documentation

Sources & methodology