Q noise: Difference between revisions
From Glossary of Meteorology
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<div class="definition"><div class="short_definition">Quasi-continuous sequences of VHF (very high frequency) [[radiation]] emanating from [[lightning]] that is associated with high-speed [[K-change]] activity along pre-ionized lightning channels.</div><br/> <div class="paragraph">The process was named by David Proctor (1974).</div><br/> </div><div class="reference">Proctor, D. 1974. VHF radio pictures of lightning. CSIR Special Report, No. TEL 120. Pretoria, South Africa.. </div><br/> | <div class="definition"><div class="short_definition">Quasi-continuous sequences of VHF (very high frequency) [[radiation]] emanating from [[lightning]] that is associated with high-speed [[K changes|K-change]] activity along pre-ionized lightning channels.</div><br/> <div class="paragraph">The process was named by David Proctor (1974).</div><br/> </div><div class="reference">Proctor, D. 1974. VHF radio pictures of lightning. CSIR Special Report, No. TEL 120. Pretoria, South Africa.. </div><br/> | ||
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Latest revision as of 16:41, 25 April 2012
Q noise
Quasi-continuous sequences of VHF (very high frequency) radiation emanating from lightning that is associated with high-speed K-change activity along pre-ionized lightning channels.
The process was named by David Proctor (1974).
Proctor, D. 1974. VHF radio pictures of lightning. CSIR Special Report, No. TEL 120. Pretoria, South Africa..
