This project will compare in situ measurements of active layer thickness depths with remotely sensed estimates of snow seasonality. Snow seasoality is an important driver of active layer depths in permafrost regions. We expecte there to be a strong correlation between the duration of the snow free period and active layer depths over several years.
data used will include: inster data here
Approach will be described here" describe
All code is copy righted by Ksenia Lepikhina & Jeffery A. Thompson and CU Earth Lab all rights reserved