Climatology and predictability of the late summer stratospheric zonal wind turnaround over Vanscoy, Saskatchewan

Debra Wunch, Martin P. Tingley, Theodore G. Shepherd, James R. Drummond, G. W.K. Moore, Kimberly Strong

Research output: Contribution to journalArticle

12 Citations (Scopus)

Abstract

A climatology of the late summer stratospheric zonal wind turnaround phenomenon is presented, with a particular focus on the behaviour over the Meteorological Service of Canada's balloon-launching site at Vanscoy, Saskatchewan (52°N, 107°W). Turnaround refers to the change in sign of the zonal wind velocity and occurs twice each year at stratospheric mid-latitudes, in early spring and in late summer. The late summer turnaround is of particular interest to the high-altitude ballooning community because it offers the ideal conditions for launch, but it is also an interesting dynamical phenomenon in its own right. It is studied here using both the National Centers for Environmental Prediction/National Center for Atmospheric Research (NCEP/NCAR) reanalysis and the United Kingdom Meteorological Office (MetO) analysis products as well as climate simulation data from the Canadian Middle Atmosphere Model (CMAM). The phenomenon and its interannual variability are documented. The predictability of the late summer turnaround over Vanscoy is investigated using both statistical averages and autocorrelation analysis. From the statistical averages, it is found that during every year since 1993, the period from 26 August to 5 September has contained appropriate launch dates. From the auto-correlation analysis, it is found that stratospheric zonal wind anomalies can persist for a month or more during most of the summer, but there is a predictability horizon at the end of the summer - just before turnaround.

Original languageEnglish (US)
Pages (from-to)301-313
Number of pages13
JournalAtmosphere - Ocean
Volume43
Issue number4
DOIs
StatePublished - Dec 1 2005

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zonal wind
climatology
summer
autocorrelation
middle atmosphere
wind velocity
anomaly
climate
prediction
simulation
analysis

All Science Journal Classification (ASJC) codes

  • Oceanography
  • Atmospheric Science

Cite this

Wunch, D., Tingley, M. P., Shepherd, T. G., Drummond, J. R., Moore, G. W. K., & Strong, K. (2005). Climatology and predictability of the late summer stratospheric zonal wind turnaround over Vanscoy, Saskatchewan. Atmosphere - Ocean, 43(4), 301-313. https://doi.org/10.3137/ao.430402
Wunch, Debra ; Tingley, Martin P. ; Shepherd, Theodore G. ; Drummond, James R. ; Moore, G. W.K. ; Strong, Kimberly. / Climatology and predictability of the late summer stratospheric zonal wind turnaround over Vanscoy, Saskatchewan. In: Atmosphere - Ocean. 2005 ; Vol. 43, No. 4. pp. 301-313.
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Wunch, D, Tingley, MP, Shepherd, TG, Drummond, JR, Moore, GWK & Strong, K 2005, 'Climatology and predictability of the late summer stratospheric zonal wind turnaround over Vanscoy, Saskatchewan', Atmosphere - Ocean, vol. 43, no. 4, pp. 301-313. https://doi.org/10.3137/ao.430402

Climatology and predictability of the late summer stratospheric zonal wind turnaround over Vanscoy, Saskatchewan. / Wunch, Debra; Tingley, Martin P.; Shepherd, Theodore G.; Drummond, James R.; Moore, G. W.K.; Strong, Kimberly.

In: Atmosphere - Ocean, Vol. 43, No. 4, 01.12.2005, p. 301-313.

Research output: Contribution to journalArticle

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