Abstract
A source of error in microphysical retrievals and model simulations is the assumption that clouds are composed of only randomly oriented ice crystals. This assumption is frequently not true, as evidenced by optical phenomena such as parhelia. Here, observations from the Cloud, Aerosol and Polarization Backscatter Lidar at Summit, Greenland are utilized along with other sensors and beam imaging to examine the properties of horizontally oriented ice crystals and the environment conditions in which they occur.
| Original language | English |
|---|---|
| Article number | 05007 |
| Journal | EPJ Web of Conferences |
| Volume | 176 |
| DOIs | |
| State | Published - Apr 13 2018 |
| Event | 28th International Laser Radar Conference, ILRC 2017 - Bucharest, Romania Duration: Jun 25 2017 → Jun 30 2017 |
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