Low-Frequency Rotation of Surface Winds over Canada

Hourly surface observations from the Canadian Weather Energy and Engineering Dataset were analyzed with respect to long-term wind direction drift or rotation. Most of the Canadian landmass, including the High Arctic, exhibits a spatially consistent and remarkably steady anticyclonic rotation of wind...

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Main Authors: Richard B. Richardson, Vladimir Y. Korolevych
Format: Article
Language:English
Published: MDPI AG 2012-10-01
Series:Atmosphere
Subjects:
Online Access:http://www.mdpi.com/2073-4433/3/4/522
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author Richard B. Richardson
Vladimir Y. Korolevych
author_facet Richard B. Richardson
Vladimir Y. Korolevych
author_sort Richard B. Richardson
collection DOAJ
description Hourly surface observations from the Canadian Weather Energy and Engineering Dataset were analyzed with respect to long-term wind direction drift or rotation. Most of the Canadian landmass, including the High Arctic, exhibits a spatially consistent and remarkably steady anticyclonic rotation of wind direction. The period of anticyclonic rotation recorded at 144 out of 149 Canadian meteostations directly correlated with latitude and ranged from 7 days at Medicine Hat (50°N, 110°W) to 25 days at Resolute (75°N, 95°W). Only five locations in the vicinity of the Rocky Mountains and Pacific Coast were found to obey a “negative” (i.e., cyclonic) rotation. The observed anticyclonic rotation appears to be a deterministic, virtually ubiquitous, and highly persistent feature of continental surface wind. These findings are directly applicable to probabilistic assessments of airborne pollutants.
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spelling doaj.art-6c8d7e0d53f8479ea9230f2e770414222022-12-22T00:01:55ZengMDPI AGAtmosphere2073-44332012-10-013452253610.3390/atmos3040522Low-Frequency Rotation of Surface Winds over CanadaRichard B. RichardsonVladimir Y. KorolevychHourly surface observations from the Canadian Weather Energy and Engineering Dataset were analyzed with respect to long-term wind direction drift or rotation. Most of the Canadian landmass, including the High Arctic, exhibits a spatially consistent and remarkably steady anticyclonic rotation of wind direction. The period of anticyclonic rotation recorded at 144 out of 149 Canadian meteostations directly correlated with latitude and ranged from 7 days at Medicine Hat (50°N, 110°W) to 25 days at Resolute (75°N, 95°W). Only five locations in the vicinity of the Rocky Mountains and Pacific Coast were found to obey a “negative” (i.e., cyclonic) rotation. The observed anticyclonic rotation appears to be a deterministic, virtually ubiquitous, and highly persistent feature of continental surface wind. These findings are directly applicable to probabilistic assessments of airborne pollutants.http://www.mdpi.com/2073-4433/3/4/522low frequency variabilitysurface observationswind direction
spellingShingle Richard B. Richardson
Vladimir Y. Korolevych
Low-Frequency Rotation of Surface Winds over Canada
Atmosphere
low frequency variability
surface observations
wind direction
title Low-Frequency Rotation of Surface Winds over Canada
title_full Low-Frequency Rotation of Surface Winds over Canada
title_fullStr Low-Frequency Rotation of Surface Winds over Canada
title_full_unstemmed Low-Frequency Rotation of Surface Winds over Canada
title_short Low-Frequency Rotation of Surface Winds over Canada
title_sort low frequency rotation of surface winds over canada
topic low frequency variability
surface observations
wind direction
url http://www.mdpi.com/2073-4433/3/4/522
work_keys_str_mv AT richardbrichardson lowfrequencyrotationofsurfacewindsovercanada
AT vladimirykorolevych lowfrequencyrotationofsurfacewindsovercanada