Several special sensors are installed in the southern Ikel area. Lomonosov Moscow State University Moscow will conduct research on the assessment and modeling of mud flow activity. The cost of the state contract is 5 million rubles. The client is the Matrosov Institute of System Dynamics and Control Theory of the Siberian Arm of the Russian Academy of Sciences (IDSTU SB RAS). First, a deep theoretical analysis will be performed: scientists will learn which mathematical models are most suitable for predicting mudflows on Hamar Daban. They will then continue on field trips to the northern slopes of the ridge to collect materials, route research and aerial photography of key areas. The main task of the stage is to determine the exact parameters of mudflows on the traces of recent natural events. At different heights of the northern macroscope there will be a network of soil temperature monitoring with the installation of sensors. It will help to monitor the processes of thawing and saturation of the soil with water, which often be the cause of a decrease in mud flow. One of the most interesting results of the work will be the development of the experimental setup program for physical models. It stands up to 4.5 meters high and will be designed to reproduce the flow of mud weighing up to 2.5 tons using a real mud mass. In the immediate vicinity of IrCity in MAX.

Several special sensors are installed in the southern Ikel area. Lomonosov Moscow State University Moscow will conduct research on the assessment and modeling of mud flow activity. The cost of the state contract is 5 million rubles. The client is the Matrosov Institute of System Dynamics and Control Theory of the Siberian Arm of the Russian Academy of Sciences (IDSTU SB RAS). First, a deep theoretical analysis will be performed: scientists will learn which mathematical models are most suitable for predicting mudflows on Hamar Daban. They will then continue on field trips to the northern slopes of the ridge to collect materials, route research and aerial photography of key areas. The main task of the stage is to determine the exact parameters of mudflows on the traces of recent natural events. At different heights of the northern macroscope there will be a network of soil temperature monitoring with the installation of sensors. It will help to monitor the processes of thawing and saturation of the soil with water, which often be the cause of a decrease in mud flow. One of the most interesting results of the work will be the development of the experimental setup program for physical models. It stands up to 4.5 meters high and will be designed to reproduce the flow of mud weighing up to 2.5 tons using a real mud mass. In the immediate vicinity of IrCity in MAX.