High-altitude watersheds in the Front Range of Colorado show symptoms of ad
vanced stages of nitrogen excess, despite having less nitrogen in atmospher
ic deposition than other regions where watersheds retain nitrogen. In two a
lpine/subalpine subbasins of the Loch Vale watershed, atmospheric depositio
n of NO3- plus NH4+ was 3.2-5.5 kg N ha(-1), and watershed export was 1.8-3
.9 kg N ha(-1) for water years 1992-1997. Annual N export increased in year
s with greater input of N, but most of the additional N was retained in the
watershed, indicating that parts of the ecosystem are nitrogen-limited. Di
ssolved inorganic nitrogen (DIN) concentrations were greatest in subsurface
water of talus landscapes, where mineralization and nitrification augment
high rates of atmospheric deposition of N. Tundra landscapes had moderately
high DIN concentrations, whereas forest and wetland landscapes had low con
centrations, indicating little export of nitrogen from these landscapes. Be
tween the two subbasins the catchment of Icy Brook had greater retention of
nitrogen than that of Andrews Creek because of landscape and hydrologic ch
aracteristics that favor greater N assimilation in both the terrestrial and
aquatic ecosystems. These results suggest that export of N from alpine/sub
alpine watersheds is caused by a combination of direct flushing of N from a
tmospheric deposition and release of N from ecosystem biogeochemical proces
ses (N cycling). Sensitivity of alpine ecosystems in the western United Sta
tes to atmospheric deposition of N is a function of landscape heterogeneity
, hydrologic flow paths, and climatic extremes that limit primary productiv
ity and microbial activity, which, in turn, control retention and release o
f nitrogen. Conceptual and mechanistic models of N excess that have been de
veloped for forested ecosystems need to be modified in order to predict the
response of alpine ecosystems to future changes in climate and atmospheric
deposition of N.