Large-amplitude electromagnetic plasma waves are one of the dominant f
eatures of the solar wind-comet interaction. Wave characteristics stro
ngly depend on parameters such as the solar wind flow and Alfven veloc
ities and the angle between flow and interplanetary magnetic field as
well as the production rate. With respect to the latter the flyby of t
he spacecraft Giotto at comet P/Grigg-Skjellerup provides a unique pos
sibility to study such waves in further detail. Pickup ion-related wav
e signatures have been observed up to a distance of 600,000 km from th
e nucleus. Peak spectral power in the spacecraft frame of reference oc
curs at frequencies mainly somewhat below the water group ion gyrofreq
uency. From this the waves are determined to be mainly left-hand polar
ized waves, causing one-sided pitch angle diffusion outbound. The wave
activity strongly increases close to the comet; upstream it exhibits
a quadratic dependence on the water group pickup ion free energy. Furt
hermore, a phenomenological study of the wave characteristics provides
a unique description of the fine-structure of the interaction region.
Indications of steepened magnetosonic waves have been found in the ou
tbound magnetosheath region.