  The eddy straining mechanism of Shutts (1983; S83) has long been considered a
main process for explaining the maintenance of atmospheric blocking. As
hypothesized in S83, incoming synoptic eddies experience a meridional straining
effect when approaching a split jetstream, and as a result, enhanced PV fluxes
reinforce the block. A two-layer QG model is adopted here as a minimal model to
conduct mechanism-denial experiments. While transient eddies' forcing is
clearly critical to the formation and maintenance of a block, using a large
ensemble, the authors demonstrate that the straining of generic eddies does not
maintain blocks, thus challenge the idea of eddy straining serving as a
positive feedback for the blocks. These results indicate that specific
configurations of the eddy field are required for the maintenance stage. The
authors also remark on the main supporting evidence in S83: the second-order
induced flow is sensitive to the location of the wavemaker.
