The sensitivity of hydrology and water resources to climate variation and c
limate change is assessed for the Mid-Atlantic Region (MAR) of the United S
tates. Observed streamflow, groundwater, and water-quality data are shown t
o vary in association with climate variation; Projections of future streamf
low, groundwater, and water quality are made using models determined from t
hese associations and are applied to 2 transient general circulation model
(GCM) scenarios. Regional streamflow increases in one scenario, but decreas
es in the other; both scenarios result in changes in the seasonality of pea
k flows. Response of groundwater to climate change depends on the GCM scena
rio used. Canadian Climate Center (CCC) scenarios suggest recharge will occ
ur earlier in the year, and that seasonal fluctuations in groundwater level
s will be less extreme. Hadley Center scenarios suggest recharge will occur
earlier in the medium term, but later in the long term, with seasonal fluc
tuations in general being more extreme. Both scenarios show that nutrient l
oads can be expected to increase in winter and spring because of the expect
ed increase in streamflow. Projected decreases in streamflow and associated
nutrient fluxes in July and August could ameliorate problems associated wi
th estuarine stratification and eutrophication in late summer. These projec
tions demonstrate that future hydrology and water resources will be influen
ced by climate change, but that uncertainty in accurately projecting that i
nfluence will continue until model scenarios improve.