Within the study region in southern Israel, the annual average rainfal
l during the period 1961-1990 increased by up to approximately 30%, wi
th only minor changes in the control stations representing the central
and northern parts of the country. The retreat of aridity is made eve
n more pronounced by an appreciable decrease in the coefficient of var
iation (CV) in nearly all of the 30 rain stations within the study reg
ion. The geographical area where maximum CV reductions were found corr
elates well with the area where intensive land-use variations took pla
ce with the initial operation of the National Water Carrier in 1964. A
global climate change in the sea surface temperatures starting in the
early 1960's may have had an effect to increase seasonal rainfall. Cu
rrent research is aimed at resolving this issue.