Interannual variability of the atmosphere of Mars is dominated by the
occurence, or absence, of planet-encircling dust storms. In this paper
we use a recent review of Earth-based telescopic observations of Mars
together with Viking orbiter and lander data to estimate the frequenc
y of occurrence of planet-encircling dust storms over the past century
and to test whether the period spanned by the Mariner 9 and Viking mi
ssions to Mars is representative of the decades prior to 1950. In doin
g so, we take into account the practical limitations imposed on Earth-
based coverage of Mars by the orbital geometries of the two planets. B
oth spacecraft and Earth-based observations suggest that planet-encirc
ling dust storms on Mars occur during a so-called ''dust storm season'
' in southern spring and summer. Viking data demonstrate decidedly tha
t planet-encircling dust storms could have occurred in the past on Mar
s without being detected from Earth during years in which Mars was far
from Earth during the dust storm season and thus difficult to observe
. However, the same historical record indicates that planet-encircling
storms were absent during the dust storm seasons monitored during sev
eral favorable oppositions prior to 1956 and after 1986. Overall, the
chance of a planet-encircling dust storm occurring in any arbitrary Ma
rs year is estimated to be approximately one in three (18-55 % at the
95 % level of confidence), if such occurrence is random from year-to-y
ear and yet restricted seasonally to southern spring and summer.