Abstract
Filamentation-induced water condensation and snow formation are investigated
using laser pulses with different chirps and pulse widths. Chirped pulses result in the
laser filamentation with different spatial lengths and intensities, which has a great
impact on airflow motion and snow formation. The experiments show that snow formation
mainly relates to the filament intensity distribution. Negative chirped pulses produce a
greater amount of snow because of higher intensity inside the filaments as compared with
the positive chirped pulses.
© 2015 Chinese Laser Press
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