SEISMOLOGICAL CONSEQUENCES OF THE COLLISION OF SHOEMAKER-LEVY 9 WITH JUPITER/

The impact of comet Shoemaker-Levy/9 into the atmosphere of Jupiter of fers a seismological probe of the interior structure of the planet. A small but significant fraction of the energy carried by a pressure wav e launched by the explosion of the comet probes deeply into the planet before refracting upward and arriving in the stratosphere of the visi ble hemisphere of Jupiter. Waves from impacts exceeding 10(28) ergs pr oduce temperature fluctuations exceeding 1 K at distances of less than or similar to 16,000 km from the impact site at the 0.02 bar pressure level. Wave arrival locations and times provide a measure of the vari ation of sound speed with radius in Jupiter and may reveal the locatio n of the molecular to metallic hydrogen phase transition. The pressure wave may also excite detectable p-mode oscillations of Jupiter.