Hydro-climatic forcing of dissolved organic carbon in two boreal lakes of Canada
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文摘

Rainfall is a driving force of dissolved organic carbon (DOC) in lacustrine systems.

We derive a parsimonious model of the hydro-climatic forcing of DOC.

We analyze long-term hydrologic controls of DOC in two pristine boreal lakes (Canada).

The model did not reveal increasing in-lake DOC concentrations through the 20th century.

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