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From Glossary of Meteorology
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The technique of
in which an instrument sends
vertically and receives reflections from atmospheric features such as inversions or turbulent layers.
A representation of the
of one or more of the
of a fluid body (typically the ocean or
) deduced from variations in reflected acoustic
A particular measurement of depth of water below an instrument (either at the surface or at some moored depth) computed from the
of an acoustic
emitted by the acoustic
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This page was last edited on 25 April 2012, at 16:19.