We review recent analyses of tracer observations within the Arctic vortex,
showing anomalous tracer-tracer relationships which indicate the mixing of
outside air into the vortex. Similar anomalous relationships have previousl
y been observed in vortex fragments, following breakdown of the Arctic vort
ex, and interpreted as indicative of mixing within the filamentary fragment
s. In the light of other observations we conclude that this interpretation
is incorrect: the mixing took place into the vortex prior to breakdown. We
discuss the effects of mixing on tracer relationships within the vortex, il
lustrated by results both from a simple conceptual model and from two three
-dimensional chemical transport models. These models indicate that continuo
us mixing across the vortex edge produces entirely changed tracer relations
inside the vortex and that separate, compact vortex relationships can deve
lop. In general, tracer relationships should not be used to estimate denitr
ification or chemical ozone loss unless the effects of mixing can be quanti
fied; this may be possible using information from other tracers, but one ca
nnot assume that the effects of anomalous mixing are manifested as simple m
ixing lines on tracer-tracer diagrams.