Spatiotemporal temperature patterns on a polycrystalline nickel disk w
ere recorded using infrared video imaging during atmospheric hydrogen
oxidation and characterized by the proper orthogonal decomposition pat
tern analysis technique. The system was studied at two different resid
ence times, 3.2 s and 6.4 s. At moderate feed temperatures, steady-sta
te multiplicity and rate oscillations were found. Oscillations at a re
sidence time of 6.4 s were periodic and essentially spatially uniform.
A t a residence time of 3.2 s, ho wever, the surface temperature beca
me nonuniform, and rate oscillations occurred via traveling temperatur
e waves which emanated from ''pacemakers '' (locally active regions) o
n the edge of the catalyst. During periodic oscillations, the waves we
re emitted synchronously from the pacemakers, while during chaotic osc
illations, the pacemakers were desynchronized and emitted waves indepe
ndently of each other. Nonlocal gas-phase coupling between distance su
rface elements caused spatial desynchronization during rate oscillatio
ns.