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Due to climatic changes, the intensity of certain cryogenic processes (in particular, warm ones, such as: thermokarst, thermoerosion, thermoabrasion, thermodenudation, which have a negative effect on permafrost conditions) has increased, and therefore the question of a detailed study of the formation of cryogenic processes in “new reality” arises in the changed environmental conditions. What is needed is the development of uniform methods for the long-term monitoring of processes, an attempt to create a modern classification of cryogenic processes from the position of finding the “triggers” for their activation. The paper discusses the main classifications of cryogenic processes, reveals the general parameters necessary for the selection of triggers