The Hubble Space Telescope made systematic observations of the split c
omet P/Shoemaker-Levy 9 (SL9) (P designates a periodic comet) starting
in July 1993 and continuing through mid-July 1994 when the fragments
plunged into Jupiter's atmosphere. Deconvolutions of Wide Field Planet
ary Camera images indicate that the diameters of some fragments may ha
ve been as large as similar to 2 to 4 kilometers, assuming a geometric
albedo of 4 percent, but significantly smaller values (that is, <1 ki
lometer) cannot be ruled out. Most of the fragments (or nuclei) were e
mbedded in circularly symmetric inner comae from July 1993 until late
June 1994, implying that there was continuous, but weak, cometary acti
vity. At least a few nuclei fragmented into separate, condensed object
s well after the breakup of the SL9 parent body, which argues against
the hypothesis that the SL9 fragments were swarms of debris with no do
minant, central bodies. Spectroscopic observations taken on 14 July 19
94 showed an outburst in magnesium ion emission that was followed clos
ely by a threefold increase in continuum emission, which may have been
caused by the electrostatic charging and subsequent explosion of dust
as the comet passed from interplanetary space into the jovian magneto
sphere. No OH emission was detected, but the derived upper limit on th
e H2O production rate of similar to 10(27) molecules per second does n
ot necessarily imply that the object was water-poor.