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An Atmospheric Water Balance over a Mountain Barrier

The flow of moisture through a "slab" of air, upwind and over the Park Range in northwest Colorado, was estimated from wintertime meteorological measurements. On average, 6–14% of the inflow moisture precipitated onto the barrier (86 to 94% flowed over the barrier). Because such a small amount... Full description

1st Person: Hindman, Edward E.
Source: in Journal of applied meteorology Vol. 25, No. 2 (1986), p. 180-183
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Type of Publication: Article
Language: English
Published: 1986
Keywords: research-article
Online: Volltext
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