The Columbus Day Storm October 12, 1962 Cliff Mass, Atmospheric Sciences

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The Columbus Day Storm October 12, 1962 Cliff Mass, Atmospheric Sciences The steeple atop historic Campbell Hall, on the Oregon College of Education Campus, Monmouth.

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The Columbus Day Storm October 12, 1962 Cliff Mass, Atmospheric Sciences. The steeple atop historic Campbell Hall, on the Oregon College of Education Campus, Monmouth. Native Americans knew about the great storms and the damage they can bring … and had several legends regarding their origin. - PowerPoint PPT Presentation

Transcript of The Columbus Day Storm October 12, 1962 Cliff Mass, Atmospheric Sciences

Page 1: The Columbus Day Storm October 12, 1962 Cliff Mass, Atmospheric Sciences

The Columbus Day StormOctober 12, 1962

Cliff Mass, Atmospheric Sciences

The steeple atop historic Campbell Hall, on the Oregon College of Education Campus, Monmouth.

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Native Americans knew about the great storms and the damage they can bring… and had several legends regarding their origin.

The Thunderbird

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European explorers immediately appreciated the threat…

““The force of southerly storms was evident to every eye; large and The force of southerly storms was evident to every eye; large and extensive woods being laid flat by their power, the branches forming extensive woods being laid flat by their power, the branches forming one long line to the North West, intermingled with the roots of one long line to the North West, intermingled with the roots of innumerable trees, which have been torn from their beds and helped to innumerable trees, which have been torn from their beds and helped to mark the furious course of their tempests.”mark the furious course of their tempests.”

John Meares,1788, off of Cape Flattery of the Olympics Peninsula

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Early settlers learned quickly

about the impacts of the great Northwest

windstormsArthur Denny

Seattle

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January 9, 1880• Hit northern Oregon and southern Washington

toppling tens of thousands of trees. • Wind gusts were estimated to reach 138 mph on

the coast and 70-80 mph in the interior.• Buildings throughout the Willamette Valley, were

damaged or destroyed. Part of the roof of the Oregon State Capital in Salem was blown off.

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January 29, 1921• Hurricane-force winds struck the entire Washington Coast

– At North Head sustained winds reached 126 mph, with a maximum one-minute wind of 150 mph before the sensor failed.

– At Tatoosh Island, 150 miles to the north, winds reached 110 mph.

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As a result, this event has become known as the “The Olympic Blowdown Storm”

In some areas over 40% of the trees were blown down

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But these and other storms were overshadowed by the Columbus

Day Storm • The strongest Pacific

storm to strike the NW since the arrival of European settlers

• Probably the most powerful non-tropical cyclone to hit the lower-48 states in a century.

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Extraordinary Impact• An extensive area, stretching from northern

California to southern British Columbia experienced hurricane-force winds, massive treefalls, and power outages.

• In Oregon and Washington, 46 died and 317 required hospitalization.

• Flooding and landslides in n. California. • Fifteen billion board feet of timber were

downed, 53,000 homes were damaged, thousands of utility poles were toppled, and the twin 520-ft steel towers that carried the main power lines of Portland were crumpled.

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On the state capitol ground in Salem, Oregon, the bronze status, the Circuit Rider was toppled

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The CD Storm had winds and a central pressure equivalent to a category 3 hurricane.

The Saffir-Simpson Hurricane ScaleNote that 1-minute average winds are used below.

• Category One:Winds 74-95 mph, above 980 mb

• Category Two:Winds 96-110 mph, 965-980 mb

• Category Three:Winds 111-130 mph , 945-965 mb

• Category Four:Winds 131-155 mph, 920-945 mb

• Category Five:Winds greater than 155 mph, below 920 mb

• Category Six: Only in the imagination of TV scriptwriters

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Hurricane Katrina Approaching the Gulf Coast

Katrina was a category 3 hurricane when it made landfall. The Columbus Day Storm was every bit as powerful…and larger.

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There is a lot of talk back east about the “Perfect Storm”

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But our Columbus Day Storm was more perfect than theirs…

• Their “Perfect Storm” had a low center of 972 hPa and maximum (estimated) sustained winds of 60 knots (observed 53 knots) with observed gusts to 65 knots.

• The Columbus Day storm had a central low pressure of 955-960 hPa and many reports of gusts above 110 knots

• NO CONTEST!

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Columbus Day 1962: At Cape Blanco there were 150 mph with gusts to 179!

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Max Winds (mph)

Columbus Day Storm 1962

Credit:Wolf Read

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Mt. Hebo Radar Facility

Courtesy: Mark Cole

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Leading to the Storm

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On October 11th, a fairly deep low pressure system

moved northward offshore, producing a windy day over

western Washington and

Oregon 4 PM October 11, 1962

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October 11th Forecast: No Storm on October 12th!

Seattle Times

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Typhoon Frieda (Freda) moved northward and transformed into a midlatitude cyclone.

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Weather Bureau Forecasters Had a Better Handle on the Storm During the Morning of October 12th

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Could a modern weather prediction model run at high

resolution get the forecast right?• Rick Steed, Research Scientist in the UW

Atmospheric Sciences Department, run the WRF model…the same one we use for real-time weather prediction.

• Initialized the model with the NCEP reanalysis grids.

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The Answer: No

Consider a forecast begun the day before (October 11th) at 5

AM.

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Start 12h later: Worse!

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The Problem? • Probably the lack

of data over the Pacific.

• Just a few ship reports and islands.

• Today we have massive satellite data assets, buoys, ships, and more.

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Pause

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Big Windstorm This Year?

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El Nino/La Nina and Major Windstorms

•Major windstorms appear to avoid El Nino and La Nino years•They like neutral winters. •Right now it looks like we will have a weak El Nino year