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Are observed small, rounded ice particles important in a climate model?
Anthony Baran
, James Manners
,
Evelyn Hesse
, Elizabeth Reeja Mathen
, Harry Ballington
School of Physics, Engineering & Computer Science
Centre for Atmospheric and Climate Physics Research
Light Scattering and Radiative Processes
Department of Physics, Astronomy and Mathematics
Centre for Climate Change Research (C3R)
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peer-review
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Keyphrases
2D Light Scattering
33%
Aerosol
16%
Albedo Parameter
16%
All-climate
16%
Asymmetry Parameter
16%
Beam-tracing Methods
33%
Cirrus
33%
Climate Modeling
16%
Climate Models
100%
Cold Temperature
33%
Crystal Composition
16%
Ensemble Model
33%
Extinction Cross Section
16%
Hertfordshire
16%
Hexagonal Columnar
33%
Hexagonal Plates
16%
High Altitude
16%
Ice Crystals
33%
Ice Particles
100%
Ice-crystal Clouds
16%
Interface Transition
16%
Low Temperature
16%
Met Office
16%
Opacity
16%
Optical Properties
16%
Radiation Field
16%
Radiation Simulation
16%
Radiative Balance
33%
Radiative Transfer Modeling
16%
Research Aircraft
16%
Rosette
33%
Rounded Particles
50%
Scattering Cross Section
16%
Scattering Image
33%
Shortwave Radiation
16%
Simulation Model
16%
Single Scattering
16%
Single Scattering Albedo
16%
Smooth Plate
16%
Spatial Composition
16%
Spatial Distribution
16%
Spectrometer
16%
Surface Roughening
16%
Temperature Simulation
16%
Thin Plate
16%
Transfer Climate
16%
Tropical Tropopause
33%
Tropical Tropopause Layer
83%
Tropics
16%
Two-stream
16%
Very High Altitude
16%
Western Pacific
16%
Earth and Planetary Sciences
Albedo
14%
Climate Modeling
100%
Ice Crystal
42%
Light Scattering
28%
Optical Property
14%
Pacific
14%
Radiation Distribution
14%
Radiative Transfer
14%
Research Aircraft
14%
Short Wave Radiation
14%
Spatial Distribution
14%
Thin Plate
14%
Tropopause
100%
Unmanned Aerial Vehicle
28%