Interplanetary shock waves, propagating in the heliosphere faster than
earlier-emitted coronal ejecta, penetrate them and modify their param
eters during this interaction. Using two and one half dimensional MHD
simulations, we show how a magnetic cloud ( flux rope) propagating wit
h a speed 3 times higher than the ambient solar wind is affected by an
even faster traveling shock wave overtaking the cloud. The magnetic f
ield increases inside the cloud during the interaction as it is compre
ssed in the radial direction and becomes very oblate. The cloud is als
o accelerated and moves faster, as a whole, while both shocks (driven
by the cloud and the faster interplanetary shock) merge upstream of th
e cloud. This interaction may be a rather common phenomenon due to the
frequency of coronal mass ejections and occurrence of shock waves dur
ing periods of high solar activity.