Optical particle probe: Difference between revisions

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|Meaning=(''Also called'' electro-optical particle probe.) Any of a class of instruments for  sizing and counting large numbers of individual [[aerosols]] or [[hydrometeors]] to characterize populations,  or also for imaging and classifying the shapes of individual hydrometeors by measuring  the optical [[illumination]], [[scattering]], or [[attenuation]] of a [[laser]] beam by each [[particle]] and recording  the result electronically.
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|Explanation=Included are [[optical scattering probes]] and [[optical imaging probes]]. Primarily airborne instruments,  they can be adapted for stationary use at the surface for [[precipitation]] or [[fog]] monitoring,  in some cases with forced [[ventilation]] to create a particle flux.
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== optical particle probe ==
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<div class="definition"><div class="short_definition">(<br/>''Also called'' electro-optical particle probe.) Any of a class of instruments for  sizing and counting large numbers of individual [[aerosols]] or [[hydrometeors]] to characterize populations,  or also for imaging and classifying the shapes of individual hydrometeors by measuring  the optical [[illumination]], [[scattering]], or [[attenuation]] of a [[laser]] beam by each [[particle]] and recording  the result electronically.</div><br/> <div class="paragraph">Included are [[optical scattering probes]] and [[optical imaging probes]]. Primarily airborne instruments,  they can be adapted for stationary use at the surface for [[precipitation]] or [[fog]] monitoring,  in some cases with forced [[ventilation]] to create a particle flux.</div><br/> </div>
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Latest revision as of 03:27, 27 March 2024

(Also called electro-optical particle probe.) Any of a class of instruments for sizing and counting large numbers of individual aerosols or hydrometeors to characterize populations, or also for imaging and classifying the shapes of individual hydrometeors by measuring the optical illumination, scattering, or attenuation of a laser beam by each particle and recording the result electronically.

Included are optical scattering probes and optical imaging probes. Primarily airborne instruments, they can be adapted for stationary use at the surface for precipitation or fog monitoring, in some cases with forced ventilation to create a particle flux.

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