About Jeff Masters
Dr. Masters co-founded wunderground in 1995. He flew with the NOAA Hurricane Hunters from 1986-1990. Co-blogging with him: Bob Henson, @bhensonweather
By: Dr. Jeff Masters , 5:34 PM GMT on January 27, 2010
The 6,288-foot peak of New Hampshire's Mount Washington is a forbidding landscape of wind-swept barren rock, home to some of planet Earth's fiercest winds. As a 5-year old boy, I remember being blown over by a terrific gust of wind on the summit, and rolling out of control towards a dangerous drop-off before a fortuitously-placed rock saved me. Perusing the Guinness Book of World Records as a kid, three iconic world weather records always held a particular mystique and fascination for me: the incredible 136°F (57.8°C) at El Azizia, Libya in 1922, the -128.5°F (-89.2°C) at the "Pole of Cold" in Vostok, Antarctica in 1983, and the amazing 231 mph wind gust (103.3 m/s) recorded in 1934 on the summit of Mount Washington, New Hampshire. Well, the legendary winds of Mount Washington have to take second place now, next to the tropical waters of northwest Australia. The World Meteorological Organization (WMO) has announced that the new world wind speed record at the surface is a 253 mph (113.2 m/s) wind gust measured on Barrow Island, Australia. The gust occurred on April 10, 1996, during passage of the eyewall of Category 4 Tropical Cyclone Olivia.
Figure 1. Instruments coated with rime ice on the summit of Mt. Washington, New Hampshire. Image credit: Mike Theiss.
Tropical Cyclone Olivia
Tropical Cyclone Olivia was a Category 4 storm on the U.S. Saffir-Simpson scale, and generated sustained winds of 145 mph (1-minute average) as it crossed over Barrow Island off the northwest coast of Australia on April 10, 1996. Olivia had a central pressure of 927 mb and an eye 45 miles in diameter at the time, and generated waves 21 meters (69 feet) high offshore. According to Black et al. (1999), the eyewall likely had a tornado-scale mesovortex embedded in it that caused the extreme wind gust of 253 mph. The gust was measured at the standard measuring height of 10 meters above ground, on ground at an elevation of 64 meters (210 feet). A similar mesovortex was encountered by a Hurricane Hunter aircraft in Hurricane Hugo of 1989, and a mesovortex was also believed to be responsible for the 239 mph wind gust measured at 1400 meters by a dropsonde in Hurricane Isabel in 2003. For reference, 200 mph is the threshold for the strongest category of tornado, the EF-5, and any gusts of this strength are capable of causing catastrophic damage.
Figure 2. Visible satellite image of Tropical Cyclone Olivia a few hours before it crossed Barrow Island, Australia, setting a new world-record wind gust of 253 mph. Image credit: Japan Meteorological Agency.
Figure 3. Wind trace taken at Barrow Island, Australia during Tropical Cyclone Olivia. Image credit: Buchan, S.J., P.G. Black, and R.L. Cohen, 1999, "The Impact of Tropical Cyclone Olivia on Australia's Northwest Shelf", paper presented at the 1999 Offshore Technology Conference in Houston, Texas, 3-6 May, 1999.
Why did it take so long for the new record to be announced?
The instrument used to take the world record wind gust was funded by a private company, Chevron, and Chevron's data was not made available to forecasters at Australia's Bureau of Meteorology (BOM) during the storm. After the storm, the tropical cyclone experts at BOM were made aware of the data, but it was viewed as suspect, since the gusts were so extreme and the data was taken with equipment of unknown accuracy. Hence, the observations were not included in the post-storm report. Steve Buchan from RPS MetOcean believed in the accuracy of the observations, and coauthored a paper on the record gust, presented at the 1999 Offshore Technology Conference in Houston (Buchan et al., 1999). The data lay dormant until 2009, when Joe Courtney of the Australian Bureau of Meteorology was made aware of it. Courtney wrote up a report, coauthored with Steve Buchan, and presented this to the WMO extremes committee for ratification. The report has not been made public yet, and is awaiting approval by Chevron. The verified data will be released next month at a World Meteorological Organization meeting in Turkey, when the new world wind record will become official.
New Hampshire residents are not happy
Residents of New Hampshire are understandably not too happy about losing their cherished claim to fame. The current home page of the Mount Washington Observatory reads, "For once, the big news on Mount Washington isn't our extreme weather. Sadly, it's about how our extreme weather--our world record wind speed, to be exact--was outdone by that of a warm, tropical island".
Comparison with other wind records
Top wind in an Atlantic hurricane: 239 mph (107 m/s) at an altitude of 1400 meters, measured by dropsonde in Hurricane Isabel (2003).
Top surface wind in an Atlantic hurricane: 211 mph (94.4 m/s), Hurricane Gustav, Paso Real de San Diego meteorological station in the western Cuban province of Pinar del Rio, Cuba, on the afternoon of August 30, 2008.
Top wind in a tornado: 302 mph (135 m/s), measured via Doppler radar at an altitude of 100 meters (330 feet), in the Bridge Creek, Oklahoma tornado of May 3, 1999.
Top surface wind not associated with a tropical cyclone or tornado: 231 mph (103.3 m/s), April 12, 1934 on the summit of Mount Washington, New Hampshire.
Top wind in a typhoon: 191 mph (85.4 m/s) on Taiwanese Island of Lanyu, Super Typhoon Ryan, Sep 22, 1995; also on island of Miyakojima, Super Typhoon Cora, Sep 5, 1966.
Top surface wind not measured on a mountain or in a tropical cyclone: 207 mph (92.5 m/s) measured in Greenland at Thule Air Force Base on March 6, 1972.
Top wind measured in a U.S. hurricane: 186 mph (83.1 m/s) measured at Blue Hill Observatory, Massachusetts, during the 1938 New England Hurricane.
Buchan, S.J., P.G. Black, and R.L. Cohen, 1999, "The Impact of Tropical Cyclone Olivia on Australia's Northwest Shelf", paper presented at the 1999 Offshore Technology Conference in Houston, Texas, 3-6 May, 1999.
Black, P.G., Buchan, S.J., and R.L. Cohen, 1999, "The Tropical Cyclone Eyewall Mesovortex: A Physical Mechanism Explaining Extreme Peak Gust Occurrence in TC Olivia, 4 April 1996 on Barrow Island, Australia", paper presented at the 1999 Offshore Technology Conference in Houston, Texas, 3-6 May, 1999.
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