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Top of the atmosphere normalized radiance (a), and degree of linear (b) and circular (c, multiplied by 103) polarization as a function of aerosol optical depth (AOD) at 550 um for selected near-UV to near-IR wavelengths angle 142.5 (SZAD40, VZAD40, RelAzimD120).

Circular Polarization in Atmospheric Aerosols

ESSIC Scientist Santiago Gasso is first author on a new paper in Atmospheric Chemistry and Physics that provides an overview of aerosol sources of circular polarization in the atmosphere and discusses possible remote sensing signatures.

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