VACILLATION CYCLES AND BLOCKING IN A CHANNEL

The response to a low-level high-frequency wavemaker forcing in a two- layer, beta-plane, quasi-geostrophic channel model is examined. The wa vemaker simulates regular baroclinic instability which then propagates to upper atmospheric levels to excite blocking. By altering the merid ional shear in the upper layer, the large-scale response can vary from a steady large-amplitude split jet, very similar to observed blocks, to a weaker split with a low-frequency vacillation cycle. The eddies w ill always resonantly excite the split flow, but a mixed instability p rocess is responsible for the breakdown in cases which oscillate, and this is demonstrated using a simplified zonal stability analysis and e nergy-tendency diagnostics. The re-excitement by the eddies continues the cycle. This model provides a theory of how the meridional structur e of the upper-level winds may determine whether a large-amplitude blo ck can be excited or persist in the presence of similar high-frequency eddy activity propagating up from below.