Published September 29, 2021 | Version v1
Conference paper Open

Monitoring dust particle orientation with measurements of sunlight dichroic extinction

  • 1. Institute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National Observatory of Athens, Athens, Greece & University of Crete, Department of Physics, Section of Astrophysics and Space Physics, Heraklion, Greece
  • 2. Institute for Environmental Research and Sustainable Development, National Observatory of Athens, Athens, Greece
  • 3. Institute for Astronomy, Astrophysics, Space Applications and Remote Sensing, National Observatory of Athens, Athens, Greece
  • 4. Physicalisch-Meteorologisches Observatorium Davos, World Radiation Center, Davos, Switzerland & Institute for Environmental Research and Sustainable Development, National Observatory of Athens, Athens, Greece
  • 5. University of Manchester, Department of Earth and Environmental Sciences, Manchester, UK
  • 6. University of Crete, Department of Physics, Section of Astrophysics and Space Physics, Heraklion, Greece & Institute of Electronic Structure and Laser and Institute of Astrophysics, Foundation for Research and Technology–Hellas, Heraklion, Greece
  • 7. University of Hertfordshire, Centre for Atmospheric and Climate Physics Research, Hertfordshire, United Kingdom

Description

Alignment of irregularly shaped dust aerosols leading to linear dichroism has been reported in atmospheric layers. The present study intents to quantify the excess linear polarization of direct solar radiation propagating through atmospheric layers, when these contain oriented dust particles. In order to record the linear polarization, we have used the Solar Polarimeter (SolPol). SolPol is an instrument that measures the polarization of direct solar irradiance at 550nm. It is installed on an astronomical tracker in order target the solar disk. Using the measurements, the Stokes parameters are retrieved (I, Q/I, U/I and V/I) with an accuracy of ~1% and precision of 1 ppm. Collocated measurements of a sun-photometer (Aerosol Robotic Network; AERONET) and lidar are used to quantify the Aerosol Optical Depth (AOD) and identify the vertical distribution of dust layers, respectively. We will present indications of dust particle orientation recorded at the PANGEA station in the island of Antikythera, Greece, and at Nicosia, Cyprus during the preparatory phase for the ASKOS campaign in July 2021. The relation of the linear polarization of the solar irradiance to other optical properties of the dust layer is investigated.

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Additional details

Funding

D-TECT – Does dust triboelectrification affect our climate? 725698
European Commission