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Scattering optics of snow
Alexander A Kokhanovsky1, Eleonora P Zege
1Institute of Environmental Physics, Bremen University, Otto Hahn Allee 1, D-28213 Bremen, Germany. alexk@iup.physik.uni-bremen.de
Applied Optics
|March 16, 2004
Summary
Snow
Area of Science:
- Earth Science
- Atmospheric Science
- Optical Physics
Background:
- Snow cover is crucial for the hydrological cycle and planetary albedo regulation.
- Snow's spectral albedo is influenced by grain microstructure, age, temperature, and pollutants.
- Understanding snow's optical properties is vital for climate and heating regime studies.
Purpose of the Study:
- To theoretically investigate snow's spectral albedo and bidirectional reflectance.
- To analyze the impact of nonspherical grain shapes and packing effects on snow reflectance.
- To explore how grain size and pollutants affect the transition from reflective to absorptive snow.
Main Methods:
- Theoretical modeling of snow's spectral albedo and bidirectional reflectance.
- Investigation of nonspherical grain shapes and close-packed effects.
- Analysis of visible and near-infrared electromagnetic spectrum interactions with snow.
Main Results:
- Nonspherical grain shape and packing significantly influence snow reflectance.
- Snow grain size and pollutant load dictate the spectral transition from high albedo to absorption.
- Snow's optical properties are sensitive to its physical characteristics and impurity content.
Conclusions:
- Snow's spectral albedo is a complex property influenced by microstructural and chemical factors.
- Satellite-based spectrometers and radiometers can monitor snow characteristics and impurity concentrations globally.
- This research provides insights for remote sensing of snow cover and its environmental impact.
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