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• W2160304431 abstract "Terrestrial ecosystems contribute significant amounts of dissolved organic carbon (DOC) to aquatic ecosystems. Temperate lakes vary in DOC concentration as a result of variation in the spatial configuration and composition of vegetation within the watershed, hydrology, and within‐lake processes. We have developed and parameterized a spatially explicit model of lake DOC concentrations, using data from 428 watersheds in the Adirondack Park of New York. Our analysis estimates watershed loading to each lake as a function of the cover type of each 10 × 10 m grid cell within the watershed, and its flow‐path distance to the lake. The estimated export rates for the three main forest cover types were 37.7–47.0 kg C·ha −1 ·yr −1 . The four main wetland cover types had much higher rates of export per unit area (188.4–227.0 kg C·ha −1 ·yr −1 ), but wetlands occupied only 11%, on average, of watershed area. As a result, upland forests were the source of ∼70% of DOC loading. There was evidence of significant interannual variation in DOC loading, correlated with interannual variation in precipitation. Estimated net in situ DOC production within the lakes was extremely low (<1 kg C·ha −1 ·yr −1 ). Many of the lakes have large watersheds relative to lake volume and have correspondingly high flushing rates. As a result, losses due to lake discharge generally had a larger effect on lake DOC concentrations than in‐lake decay. Our approach can be readily incorporated within a GIS framework and allows examination of scenarios such as loss of wetlands, alterations in forest management, or increases in conserved areas, as a function of the unique configuration of individual watersheds." @default.
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• W2160304431 date "2004-06-01" @default.
• W2160304431 modified "2023-10-17" @default.
• W2160304431 title "A SPATIALLY EXPLICIT WATERSHED-SCALE ANALYSIS OF DISSOLVED ORGANIC CARBON IN ADIRONDACK LAKES" @default.
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• W2160304431 doi "https://doi.org/10.1890/02-5271" @default.
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