Mountain-gap wind

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Mountain-gap wind (gap wind, gap flow) - a local wind blowing through a gap between mountains.

Gap winds are low-level winds and can be associated with strong winds of 20-40 knots and on occasion exceeding 50 knots. Gap winds are generally strongest close to wind exit.

Example flows incude the surface winds blowing through the Strait of Gibraltar - one of the strongest winds in this region is called levanter. Similar winds occur at other gaps in mountain ranges, such as the tehuantepecer and the jochwinde, and in long channels, such as the Strait of Juan de Fuca between the Olympic Mountains of Washington and Vancouver Island, British Columbia, the Hinlopenstretet near Spitsbergen.

[edit] References

• Bendall, A. A., 1982: Low-level flow through the Strait of Gibraltar. The Meteorological Magazine, Vol. 111, pp. 149-153

• Colle, B. A., C. F. Mass, 2000: High-Resolution Observations and Numerical Simulations of Easterly Gap Flow through the Strait of Juan de Fuca on 9-10 December 1995. Monthly Weather Review: Vol. 128, pp. 2398-2422.

• Colle, B. A., C. F. Mass, 1998: Windstorms along the Western Side of the Washington Cascade Mountains. Part I: A High-Resolution Observational and Modeling Study of the 12 February 1995 Event. Monthly Weather Review: Vol. 126, pp. 28-52.

• Overland, J. E., and B. A. Walter, 1981: Gap winds in the Strait of Juan de Fuca, Monthly Weather Review: Vol. 109, pp. 2221-2233.

• Scorer, R.S., 1952: Mountain-gap winds; a study of the surface wind in Gibraltar. Quarterly Journal of the Royal Meteorological Society: Vol. 78, pp. 53-59

• Sharp, J. and C. F. Mass, 2002: Columbia Gorge Gap Flow: Insights from Observational Analysis and Ultra-High Resolution Simulation. Bulletin of the American Meteorological Society: Vol. 83, pp. 1757-1762.

• Steenburgh, W. J., D. M. Schultz, B. A. Colle, 1998: The Structure and Evolution of Gap Outflow over the Gulf of Tehuantepec, Mexico. Monthly Weather Review: Vol. 126, pp. 2673-2691.