Temperature fluctuations of a Si melt in a Czochralski crucible are me
asured. Spectral analysis revealed that a baroclinic wave occurred abo
ve a certain crucible rotation rate. Above the critical condition, the
temperature fluctuation increased abruptly in amplitude. The fluctuat
ion involved a characteristic frequency component that did not coincid
e with the period of the crucible rotation. Examination of phase diffe
rences among the data measured at different point revealed that the pe
riodic motions were the result of azimuthal propagation of a temperatu
re pattern. Experimental conditions based on the thermal Rossby number
yielded wave motion which agrees with the theoretical value according
to the theory of baroclinic instability.