Abstract
Simultaneous in situ measurements of stratospheric ClO and HCl have been made for the first time during numerous flights of the ER‐2 aircraft covering latitudes 24–90°N from October 1991 through March 1992. The ClO/HCl ratio is identified as a key indicator of heterogeneous processing both outside and within the Arctic polar vortex. For ClO mixing ratios below about 120 pptv, remarkably constant ClO/HCl values of about 15% characterize the lower stratosphere. The observed values are significantly higher than those derived from a 2‐D model using either gas phase photochemistry alone (2%), or including heterogeneous sulfate chemistry (5–10%). During the Arctic early spring, after conversion of HCl into reactive chlorine has taken place, the vortex edge is poorly defined by ClO levels. Loss of HCl and its slow recovery following low‐temperature polar heterogeneous chemistry distinguishes HCl as a new and unique dynamical tracer of PSC‐processed air.
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