Isoprene emissions are significant, largely from broad-leaved trees, contributing over half of global biogenic VOC emissions, particularly from tropical regions like South America.
During the day, isoprene is emitted into the atmosphere, converting into oxygenated VOCs within hours, representing a complex interaction with hydroxyl radicals.
Deep convection transports isoprene to the upper troposphere rapidly, where it's involved in secondary organic aerosol production, highlighting its role in atmospheric chemistry.
The interaction of isoprene with nitrogen oxides from deep convective clouds showcases the dynamic processes influencing aerosol formation and OH recycling in the atmosphere.
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