The planet Mars has been visited in the past by orbital probes and lan
ders to study the atmosphere and the ground. But despite these numerou
s missions, more than 20 years ago, many parameters and phenomena are
not known at this time. The large possibilities given by new technolog
ies, in terms of weight and power consumption, allow the realization o
f new experiments at the surface of Mars. The aim is to propose the in
stallation of a bottomside ionospheric sounder. This instrument will c
ontribute to our scientific understanding of Mars. It will answer one
of the main scientific objectives of the IMEWG (International Mars Exp
loration Working Group) mission scenario: the characterization of the
Martian upper atmosphere and its interaction with the solar wind. Iono
spheric sounding is a well-known technique at the surface of the Earth
which has proven to be very useful for the study of the lower ionosph
ere. The principle is to transmit a radio pulse vertically and to meas
ure the time which elapses before the echo is received. By varying the
frequency of the pulse carrier wave, a plot can be obtained of echo d
elay versus frequency. It gives information about the propagation medi
um. The scientific objectives are described which can be achieved with
such an experiment and the parameters which can be measured underlini
ng the specificity of the Martian atmosphere are given. The theoretica
l scientific background of this sounder is briefly described and, fina
lly, its feasibility is discussed. Copyright (C) 1996 Elsevier Science
Ltd