Is midlatitude convection an active or a passive player in producing global circulation patterns?

The ability of persistent midlatitude convective regions to influence hemis pheric circulation patterns during the Northern Hemisphere summer is invest igated. Global rainfall data over a 15-yr period indicate anomalously large July total rainfalls occurred over mesoscale-sized, midlatitude regions of North America and/or Southeast Asia during the years of 1987, 1991, 1992, and 1993. The anomalous 200-hPa vorticity patterns for these same years are suggestive of Rossby wave trains emanating from the regions of anomalous r ainfall in the midlatitudes. Results from an analysis of an 11-yr mean monthly 200-hPa July wind field i ndicate that, in the climatological mean, Rossby waveguides are present tha t could assist in developing a large-scale response from mesoscale-sized re gions of persistent convection in the midlatitudes. This hypothesis is test ed using a barotropic model linearized about the 200-hPa July time-mean flo w and forced by the observed divergence anomalies. The model results are in qualitative agreement in the observed July vorticity anomalies for the fou r years investigated. Model results forced by observed tropical forcings fo r the same years do not demonstrate any significant influence on the midlat itude circulation. It is argued that persistent midlatitude convective regi ons may play a role in the development, maintenance, and dissipation of the large-scale circulations that help to support the convective regions.