“…Increased COS (20-50%) in the tropical tropopause layer (the main entry region to the stratosphere), along with a substantial increase in other tracers of biomass burning (BB), including CO, HCN, CH 3 Cl, NO x , NO y in 1996 and 1999-2000, has been observed (20). Potassium (K), a tracer of BB, can serve in certain circumstances as a tracer of forest fires (21,22), and ice-core data have revealed increased K concentration after intensive biomass burning events from 1750 to 1980 (23). There are no global measurements of trace gases available from 1998 to 1999 BB events.…”