The intensity of chorus as observed at several high latitude ground station
s in the Antarctic is highly correlated with the solar wind dynamic pressur
e exerted on the magnetopause boundary. In two different cases, intense cho
rus and associated precipitation measured as riometer absorption were abrup
tly interrupted by several minutes of deep quieting. Satellite measurements
of solar wind dynamic pressure showed the intensity of chorus to rapidly r
espond to magnetospheric compression and relaxation over an extended region
as evidenced by the fact the effect was observed at multiple sites.