Mod-Ex Question 1

MEQ1: Permafrost - Topography - Hydrology

How do permafrost, topographic, and hydrological properties co-evolve and affect carbon and energy fluxes?

In Phase 4, we are testing the hypothesis that co-evolution of permafrost thermal conditions, microtopography, and surface/subsurface hydrology in a warming climate will lead to drier conditions on average but greater large-scale spatial variability in moisture content and partitioning of fluxes between COand CH4. Surface drying will be widespread because of increased evapotranspiration and deeper hydrologic flow paths in general and will be accelerated in polygonal ground by uneven subsidence, which reduces storage in microtopographic depressions. Reduced depression storage will increase the role of macrotopography, leading to greater large-scale spatial variability in moisture content and CO2 and CH4 fluxes.

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