Fig. 8
From: Influence of snowmelt on increasing Arctic river discharge: numerical evaluation
Spatial distribution of standard deviations for a active layer thickness and b surface soil moisture. Surface soil moisture is defined as the water content in a soil column extending from the surface to a depth of 1.5Â m. The standard deviations, calculated from the anomalous values representing the difference between the treated simulations and the reference simulation, illustrate the sensitivity of the active layer and the soil moisture to climatic variations during the Arctic cold season