Water resources are the lifeblood of the Near East region. Careful planning
and management of water resources in dry land regions requires information
on the likelihood of extreme events, especially prolonged drought. It is e
ssential to understand the variability of climate on time scales of decades
to centuries to assign reasonable probabilities to such events. Tree-ring
analysis is one way to increase our knowledge of the climate variability be
yond the short period covered by the instrumental data. In this paper, we r
econstruct October-May precipitation from a Juniperus phoenicia tree-ring c
hronology in southern Jordan to gain a longterm (A.D. 1600-1995) perspectiv
e on runs of dry years and on time series fluctuations in precipitation ave
raged over several years. The reconstruction equation derived by regression
of log-transformed precipitation on tree-ring indices explains 44 percent
of the variance of observed precipitation. The longest reconstructed drough
t, as defined by consecutive years below a threshold of 217.4 mm, was four
years, compared with three years for the 1946-95 instrumental data. A Monte
Carlo analysis designed to account for uncertainty in the reconstruction i
ndicates a lower than 50 percent chance that the region has experienced dro
ught longer than five years in the past 400 years.