A Microphysical Basis For Lightning On Venus?

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Scientific paper

The conditions in the atmosphere of Venus above an altitude of about 57km are suitable for the existence of the frozen species of sulfuric acid monohydrate (weight percent 84.5%). The presence of frozen particles is a key ingredient in most processes of the particle charging that leads to lightning in terrestrial clouds. We have performed simple calculations that show that the introduction of a small admixture of frozen sulfuric acid monohydrate in the upper clouds and/or hazes of Venus can lead to conditions in the clouds that are suitable for the generation of lightning discharges. We estimate that this lightning could occur at a rate roughly comparable to that of Earth. The existence of a population of ice particles in the upper cloud could have ramifications for other long-standing problems in the study if the Venusian atmosphere, including the composition of the upper hazes, and the composition of the controversial Mode 3 particles in the middle and lower clouds.

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