Shortwave radiation: Difference between revisions
From Glossary of Meteorology
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#<div class="definition"><div class="short_definition">Energy in the visible and near-visible portion of the [[electromagnetic spectrum]] (0.4–1.0 μm in [[wavelength]]).</div><br/> </div> | #<div class="definition"><div class="short_definition">Energy in the visible and near-visible portion of the [[electromagnetic spectrum|electromagnetic spectrum]] (0.4–1.0 μm in [[wavelength]]).</div><br/> </div> | ||
#<div class="definition"><div class="short_definition">In meteorology, a term used loosely to distinguish [[radiation]] in the visible and near-visible portions of the [[electromagnetic spectrum]] (roughly 0.4–4.0 μm in [[wavelength]]), usually of solar origin, from that at longer wavelengths ([[longwave radiation]]), usually of terrestrial origin.</div><br/> </div> | #<div class="definition"><div class="short_definition">In meteorology, a term used loosely to distinguish [[radiation]] in the visible and near-visible portions of the [[electromagnetic spectrum]] (roughly 0.4–4.0 μm in [[wavelength]]), usually of solar origin, from that at longer wavelengths ([[longwave radiation]]), usually of terrestrial origin.</div><br/> </div> | ||
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Latest revision as of 16:52, 25 April 2012
shortwave radiation
- Energy in the visible and near-visible portion of the electromagnetic spectrum (0.4–1.0 μm in wavelength).
- In meteorology, a term used loosely to distinguish radiation in the visible and near-visible portions of the electromagnetic spectrum (roughly 0.4–4.0 μm in wavelength), usually of solar origin, from that at longer wavelengths (longwave radiation), usually of terrestrial origin.
