Clouds their Formation, Optical Properties, and Effects by Peter V. Hobbs

By Peter V. Hobbs

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Extra resources for Clouds their Formation, Optical Properties, and Effects

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10H 5H 0 2 4 6 8 10 12 14 16 18 20 22 24 26 28 DIAMETER (μm) FIGURE Measurements with 8. Aged stratus performed a PMS FSSP droplet in north instrument. size central distribution. Colorado by the author 30 R. G. KNOLLENBERG 34 particle. The p r o b a b i l i t y of m o r e t h a n o n e p a r t i c l e w i t h i n the viewing volume . P(n) = ^ η V where P(n) / V ) follows Poisson occurring statistics, that is. -(v/V) G n! is t h e p r o b a b i l i t y o f t h e p r e s e n c e o f η p a r t i c l e s ; V, t h e v o l u m e p e r p a r t i c l e ; and v , the v i e w i n g v o l u m e .

Aperture in an and exterior TECHNIQUES FOR PROBING CLOUD MICROSTRUCTURE FIGURE R. 9. Τ. Ryan) . Optical cloud particle spectrometer 35 (courtesy of R. G. KNOLLENBERG 36 cowl a s s e m b l y . 3 χ 10 cm sample from t h e a i r c r a f t s k i n . filter. 5 d r o p l e t b e a m and r e c o r d i n g instrument for c l o u d d r o p l e t t r i b u t i o n m e a s u r e m e n t s is t h e F o r w a r d S c a t t e r i n g (FSSP) d e v e l o p e d b y P M S . The F S S P successor to the Axially Scattering The primary electronic size the Spectrometer (18) i s an improved Spectrometer Probe s u b s y s t e m s r a t h e r t h a n in f u n d a m e n t a l d e s i g n forward scattering the F S S P h a v i n g the w i d e r c o l l e c t i n g g e o m e t r y (ASSP).

It is necessary actual depth of field t o considerably is v i e w e d to t r u n c a t e less than this distance to avoid errors associated w i t h the loss of collecting and s c a t t e r i n g signal. aperture This is accomplished by comparing signals from the levels from peak readers observing pair. Because of the annular aperture on the masked prism the l i g h t from a p a r t i c l e n e a r t h e o b j e c t p l a n e is the signal photodiode face, greatly r e d u c e d a n d i s , i n g e n e r a l , l e s s b e c a u s e o f t h e l o s s of c o l l e c t ­ ing a p e r t u r e .

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