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The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency and Intensity of McMurdo Area High Wind Events David M. Rasmussen Jr. 1,* , Linda M. Keller 1,2 , and Matthew A. Lazzara 1 1 Antarctic Meteorological Research Center 2 Department of Atmospheric and Oceanic Science University of Wisconsin-Madison, Madison, Wisconsin

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Page 1: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

A 20 Year Assessment of the Frequency and Intensity of McMurdo Area High Wind Events

David M. Rasmussen Jr.1,*, Linda M. Keller1,2, and Matthew A. Lazzara1

1Antarctic Meteorological Research Center2 Department of Atmospheric and Oceanic Science

University of Wisconsin-Madison, Madison, Wisconsin

Page 2: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Outline

• Motivation

• Defining a ‘high wind event’

• Difficulties

• Results

• Conclusion

• Future Work

Page 3: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Motivation

• Address hypothesis:– Recent structural damage in the McMurdo

region is do to an increase in the frequency, duration, and/ or intensity of ‘high wind events’

– Use wind speed data from AWS stations in McMurdo/ Ross Island Region

Page 4: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Spatial Variation

Page 5: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Wind Event Thresholds

• Thresholds ~2 standard deviations from mean wind speed

• Choose nearest Beaufort Wind Force Scale

Page 6: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Wind Distributions

Pegasus North AWS Wind Speed Distribution 1990-2009

Page 7: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Beaufort Wind Force Scale Review

Force Wind Speed

Description

7 13.9-17.1 m/s Trees in motion, effort needed to walk against the wind.

*Pegasus North and Herbie Alley AWS

8(Gale)

17.2-20.7 m/s Some twigs broken from trees. Cars veer on road. Progress on foot is seriously impeded.

*Cape Bird AWS

Page 8: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Beaufort Scale cont.

Force Wind Speed

Description

9 20.8-24.4 m/s Some branches break off trees, and some small trees blow over. Construction/temporary signs and barricades blow over.*Minna Bluff AWS

10(Storm)

24.5-28.4 m/s Trees are broken off or uprooted, saplings bent and deformed. Poorly attached asphalt shingles and shingles in poor condition peel off roofs.*Black Island AWS

Page 9: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

High Wind Event Duration

• Meets 6, 12, and 24-hour duration requirements

• At least half of observations from each high wind event must:– not be missing– meet Beaufort Force thresholds assigned to each

AWS station

Page 10: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Difficulties

• Too much missing wind data to make many clear assessments

Page 11: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Difficulties cont.

Seasonal Missing AWS Data AWS Name DJF MAM JJA SON

Black Island 19% 24% 21% 14% Cape Bird 15% 0% 12% 18% Herbie Alley 9% 21% 55% 33% Minna Bluff 24% 15% 29% 33% Pegasus North 22% 15% 22% 18% Average 18% 15% 28% 23%

• Instrument changes at AWS sites

• Missing data by seasons

Page 12: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Results

• Little or no change in frequency of 6, 12, and 24 hour wind events between 1990’s and 2000’s at 3 AWS sites

Page 13: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Results cont.

• Maximum wind speeds

• Two-tailored Student’s t-test used to determine changes in annual maximum wind speeds between 1990’s and 2000’s

AWS t-test result Black Island Minor Significance Minna Bluff Not significant Pegasus North Not significant

Page 14: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Results cont.Changes in the intensity of seasonal high wind events

Cape Bird AWS

Pegasus North AWS

Page 15: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Results cont.

• AWS wind speed direction

Normalized Wind Direction (Scale 1-100)

Mean Wind Speed (m/s)

Page 16: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Conclusion

• Slight increase in number of seasonal events at a few AWS sites seen between decades, but not significant

• Analysis heavily dependent upon quality of data, data availability– seasons and years with greater than 25% missing data

not included in analysis

• No significant change in high wind event frequency, duration and intensity seen across all sites between 1990’s and 2000’s, but analysis continuing

Page 17: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Conclusion cont.

• No clear link between ENSO years and ‘high wind events’

• Re-verification that the fewest frequency of events occurs in the Austral Summer

• Disagreement exists between other seasons as to which has the greatest frequency of ‘high wind events’

Page 18: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Future Work

• Continuing to improve wind observation consistency (esp. in austral winter months)

• Improvement in data distribution (missing years of Black Island AWS data)

• Meteorologists working more closely with Antarctic builders and/or architects

Page 19: The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010. A 20 Year Assessment of the Frequency

The 5th Antarctic Meteorological Observations, Modeling, and Forecasting Workshop. Columbus, Ohio July 12-14, 2010.

Acknowledgements

• This material is based upon work supported by the National Science Foundation under Grant Numbers: ANT-0537827, ANT-0636873, and ANT 0838834