Lily Zhang CRTMDS WSM6 Parameterized Phase Function Rayleigh Henyey Greenstein Scattering Phase Functions Combined Phase Function Combined HenyeyGreenstein and Rayleigh Phase Function Modified asymmetry parameter G ID: 636077
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Slide1
Impact of Non-Spheric Particle Shapes on Cloud Radiative/Optical Properties
Lily ZhangSlide2
CRTM-DS WSM6, Parameterized Phase FunctionSlide3
Rayleigh
Henyey Greenstein
Scattering Phase Functions
Combined Phase FunctionSlide4
Combined Henyey–Greenstein and Rayleigh Phase Function
Modified asymmetry parameter - G
g-GSlide5
Mie Theory
CRTM treats the ice particles as spheres
Mie theory describes scattering of a homogenous sphereSlide6
CRTM-DS WSM6, Parameterized Phase Function
CRTM-DS WSM6, Mie Theory Phase FunctionSlide7
Phase FunctionSlide8
Phase FunctionSlide9
Moving ForwardSlide10
Non-Spheric Particles
Ice does not form in spheroid shapes
Guosheng Liu databaseSlide11
Differences are not immediately obviousMore detailed cross section data for different particles needed