It has been well established that the greenhouse gas loading of the atmosph
ere has been increasing since the mid 19th century. Consequently, shifts in
the earth's radiative balance are expected with accompanying alterations t
o the earth's climate. With these anticipated, and perhaps already observab
le, changes in both global and regional climate, managers of regional water
resources seek insight to the possible impacts climate change may have on
their present and future water supplies. The types and degrees of impacts t
hat climate change may have on New York City's water supply system were ass
essed in a study of a watershed at Allaben, New York. Hypothetical scenario
s of future climate and climate change projections from three General Circu
lation Models (GCMs) were used in conjunction with the WatBal hydrological
model and the Palmer Drought Severity Index (PDSI) to ascertain how runoff
and soil moisture from this watershed may change in a warmer climate. For t
he worst case predictions, the results indicate that within the century of
the 2000s, the watershed's air temperature may increase up to about 11 degr
ees F, while its precipitation and runoff may decrease by about 13 and 30 p
ercent, respectively. If this watershed is typical of the others within the
New York City water supply system, the system's managers should consider i
mplementing mitigation and adaptation strategies in preparation for the wor
st of these possible future conditions.