We present here a six-species comparison of tree-ring growth response to ex
tremes (below the 30th and above the 70th percentile) in temperature, preci
pitation, and corresponding streamflow. The species compared are Pinus edul
is (PIED), Pseudotsuga menziesii (PSME), Pinus ponderosa (PIPO), Pinus flex
ilis (PIFL), Pinus aristata (PIAR), and Picea engelmannii (PCEN). Sensitivi
ty was determined using contingency scores obtained by comparing tree-ring
growth at different lags with hydroclimatic observations from the Upper Col
orado River Basin in the southwestern United States. The scores were comput
ed using dual scaling methods in which the higher scores are assigned to st
ronger relationships between tree-ring growth and severe hydroclimatic occu
rrences. At lag 0, PIED and PSME present the greatest sensitivity to severe
streamflow events. For precipitation and temperature the most sensitive sp
ecies at lag 0 are PIED and PIPO. PIAR and PCEN show no significant relatio
nship with extreme hydroclimatic events. PIFL shows more uniform lag-to-lag
scores, suggesting a higher year-to-year persistence for this species. In
general, tree-ring growth for all sensitive species is more responsive to h
ot-dry than to cool-moist extreme conditions. The scoring method proposed i
n this study for the analysis of tree-ring records proved to be a useful to
ol for evaluating ring-width sensitivity to extreme climatic forcing.