The same bacteria that cause frost damage on plants can help clouds to produce rain and snow. Studies on freshly fallen snow suggest that ‘bio-precipitation’ might be much more common than was suspected.
Before a cloud can produce rain or snow, rain drops or ice particles must form. This requires the presence of aerosols: tiny particles that serve as the nuclei for condensation. Most such particles are of mineral origin, but airborne microbes — bacteria, fungi or tiny algae — can do the job just as well. Unlike mineral aerosols, living organisms can catalyse ice formation even at temperatures close to 0 ºC.
The effect of the biological ‘ice nucleators’ on precipitation has been a mystery, not least because no one has yet been able to detect them in clouds.Further more see on article by Quirin Schiermeier here.
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