Laws for Size Distribution of Khasyreis

Research into Cryolithozone Spatial Pattern Changes Based on the Mathematical Morphology of Landscapes

“…where µ is the mean number of depressions per unit area, s is the area of the test site, and t is the time since the process started. This model was examined along with three other variants of the morphological pattern development model for the thermokarst plains with fluvial erosion (synchronous start, quasiuniform growth of lakes), and was confirmed as the most common [41] within the cryolithozone. This model's analysis reveals the dynamic balance between the origin of new lakes and their transformation into khasyreis, which appear after a long period of development within a wide range of natural conditions [38,41,42].…”