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Water Vapor. -. 104.5. +. Droplets. Haze. 1. 10. 100. 1000. 10,000. 100,000. Angstroms. -10. -9. -8. -7. -6. -5. 10. 10. 10. 10. 10. 10. Meters. Mie Scattering. Rayleigh Scattering. I. a. 2. 4. p. r. [. ]. =. ,. I. =. J. (. 2. m. ). 1. m. l. 4. I.
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- 104.5 +
Droplets Haze 1 10 100 1000 10,000 100,000 Angstroms -10 -9 -8 -7 -6 -5 10 10 10 10 10 10 Meters
Mie Scattering Rayleigh Scattering I a 2 4 p r [ ] = , I = J ( 2 m ) 1 m l 4 I 0 p r sin f 2 m = . J where l f 2 = 1 + cos f . J 90 Haze Droplets 0 1 -1 10 10 10 Micrometers
Mie Scattering Rayleigh Scattering Droplets Haze 1 10 100 1000 10,000 100,000 Angstroms -10 -9 -8 -7 -6 -5 10 10 10 10 10 10 Meters
Condensation Nuclei k N = cr Number per unit volume Continental d Maritime AJunge@ Distribution valid for r<2 :m. Radius
Water Vapor Water Vapor N N O O 2 2 2 2 CO CO 2 2 - Cl Liquid Water + Na +2 Mg + Na
101 100 80 Relative Humidity % 60 40 20 0 4 6 8 10 Radius in arbitrary units
101 100 80 Relative Humidity % 60 40 20 0 4 6 8 10 Radius in arbitrary units
101 100 80 60 Relative Humidity % 40 20 0 10 4 6 8 Radius in arbitrary units
101 100 80 Relative Humidity % 60 40 20 0 10 4 6 8 Radius in arbitrary units
101 100 80 60 Relative Humidity % 40 20 0 10 4 6 8 Radius in arbitrary units
101 100 80 60 40 Relative Humidity % 20 0 10 4 6 8 Radius in arbitrary units
101 100 80 60 40 Relative Humidity % 20 0 10 4 6 8 Radius in arbitrary units
101 100 80 60 40 Relative Humidity % 20 0 10 4 6 8 Radius in arbitrary units
101 100 80 60 40 Relative Humidity % 20 0 10 4 6 8 Radius in arbitrary units
101 100 80 60 40 Relative Humidity % 20 0 10 4 6 8 Radius in arbitrary units
Water Vapor Water Vapor N N O O 2 2 2 2 CO CO 2 2 Liquid Water Liquid Water + Na
101 100 Relative Humidity % 80 4 6 8 10 Radius in arbitrary units
e c b RH = » 1 + - 3 e rT r s K H Water Vapor Scavenging
T T 2 1 # # Radius Radius T T 4 3 # # Radius Radius
Time - r p - 1 e x f ( r ) = G ( p ) Number/interval Cloud Mist Rain Radius of Drops
Energetics of Phase Changes in Water Energy Vapor c=0.5 cal/g Liquid c=1 cal/g 20 0 Ice c=0.5 cal/g -20 40 Temperature (Celsius)
Condensation Nuclei Distribution k cr N = d Gamma Distribution (Cloud droplets) - r p - 1 e x f ( r ) = G ( p ) Truncated Log-normal Distribution (rain)