Spicules are known as one of the most prevalent small-scale dynamic ph
enomena on the sun, which are likely to give considerable contribution
to coronal heating and mass supply. We discuss a model of the spicule
s driven by a train of slow MHD shock waves propagating along a vertic
al expanding magnetic flux tube. The shocks are initiated due to compr
ession of the tube by the increasing external pressure in the lower ch
romosphere. Downflow of spicular material depends on radiative cooling
and other dissipative processes.