The Arctic has historically been a carbon (C) sink, resulting in vast quantities of C stored in soil and permafrost. Approximately twice as much C is stored in permafrost as is in the entire atmosphere. As permafrost thaws, this C can be decomposed by soil microorganisms and respired as carbon dioxide (CO2) or methane (CH4), and dissolved and transported through inland waters. The Arctic is now warming at an accelerated rate, and recent research has shown increasing emissions of CH4 and CO2 (C fluxes), inducing the Arctic to switch from a sink to a source of C to the atmosphere. Modeling C fluxes in the Arctic and predicting them into a warmer future has been one of the greatest challenges to understanding the Arctic carbon cycle.
The overarching objective of this project is to produce high-resolution maps of wetlands, surface water, and vegetation to interpret airborne C fluxes in the YK Delta. We will quantify and scale functional relationships of wetland and inland aquatic C that incorporate biogeochemical mechanisms, hydrologic connectivity in contributing watersheds, and water- body shape and size. We will incorporate airborne data and identify the relevant scale needed to accurately quantify C fluxes from tundra, wetlands, and terrestrial-aquatic interfaces and resolve the discrepancy between top-down and bottom-up C budgets for the YK Delta.