1970Journal of Geophysical Research AtmospheresRequires access

Ducting of acoustic-gravity waves in the atmosphere with spatially periodic wind shears

C. H. Liu

Open publisher page 17 citations

Abstract

A mechanism for horizontal ducting of acoustic gravity waves in the atmosphere is studied. We assume a background horizontal wind with a periodic vertical shear of the form υo sin K1z. This wind may interact with the acoustic-gravity wave to cause horizontal ducting of the wave. The ducting condition is derived. Trapping depth for a typical atmosphere is computed.

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What this paper is about

A mechanism for horizontal ducting of acoustic gravity waves in the atmosphere is studied. We assume a background horizontal wind with a periodic vertical shear of the form υo sin K1z. This wind may interact with the acoustic-gravity wave to cause horizontal ducting of the wave. The ducting condition is derived. Trapping depth for a typical atmosphere is computed.

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Available abstract

A mechanism for horizontal ducting of acoustic gravity waves in the atmosphere is studied. We assume a background horizontal wind with a periodic vertical shear of the form υo sin K1z. This wind may interact with the acoustic-gravity wave to cause horizontal ducting of the wave. The ducting condition is derived. Trapping depth for a typical atmosphere is computed.

Key concepts: Atmospheric duct, Atmosphere (unit), Gravity wave, Geology, Geophysics, Gravitational wave, Meteorology, Atmospheric sciences

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