Fig. 3
From: Effects of snow manipulation on larch trees in the taiga forest ecosystem in northeastern Siberia
Depth distribution of isotherms and seasonal variation of soil temperature. Depth distribution of isotherms (daily averages of soil temperature) at the CONTROL (a), SNOW− (b), and SNOW+ (c) plots, seasonal variations in soil temperature at 0.1, 0.4, and 0.8 m, and air temperature in the CONTROL, SNOW+ and SNOW− plots (d), from August 2015 to August 2016