Following reductions in the emission and deposition of sulfur compounds in
the past decade, atmospheric deposition of nitrogen has become a focus of c
oncern. Identification of watershed characteristics that mediate the effect
of atmospheric nitrogen deposition can help evaluate the sensitivity of la
kes to chronic and episodic nitrogen addition. Twenty four lakes in the sou
thwestern portion of the Adirondack Park, New York, U.S.A., were classified
into three N classes by cluster analysis of lakewater NO3-N concentration
[N] during the summers of 1994-1996. The lake-N classes were best character
ized as having (1) low [N] throughout the summer, (2) high [N] in early- bu
t low [N] in late-summer, and (3) high [N] throughout the summer. The three
lake-N classes were reconstructed perfectly by canonical discriminant anal
ysis based mainly on lake average depth (AD), and lakewater concentrations
of chlorophyll a [Chla] and SO4-S [S] in mid-summer. Increases in AD and [S
], but decrease in [Chla] corresponded with a transition from low- to high-
N classes.