Affiliation:
1. Academy of Sciences of the Republic of Sakha (Yakutia); Yugra University
2. Academy of Sciences of the Republic of Sakha (Yakutia)
3. Academy of Sciences of the Republic of Sakha (Yakutia); Ammosov North-Eastern Federal University
Abstract
The main mathematical models used to address issues related to global climate change and human impact on the natural systems of the northern regions are discussed. These models were employed to analyze the effects of emergency situations and develop regional decision-making systems for prevention and mitigation. Moreover, these models can be utilized to establish automated networks for monitoring carbon flows, forecasting climate change, identifying sources of pollution, and describing the processes by which pollution spreads in the atmosphere, soil, or water bodies. These efforts aim to address the environmental damage and mitigate the negative impacts of human activity on the natural world.
Publisher
Academy of Sciences of the Republic of Sakha (Yakutia)
Reference30 articles.
1. Glagolev M.V., Sabrekov A.F. Determination of gas exchange on the border between ecosystem and atmosphere: inverse modeling. Mathematical Biology and Bioinformatics. 2012;7(1):81–101.
2. Belolipetsky V.M., Belolipetsky P.V. Estimation of carbon flux between atmosphere and terrestrial ecosystem using vertical distribution of co2 concentrations measured on tall-tower. Vestnik NSU. Series: Information Technologies. 2011;9(1):75–81. (In Russ.)
3. Glagolev M.V., Fillipov I.V. Measurements of green-house gas fluxes in wetland ecosystems . Khanty-Mansiysk: Ugra State University; 2014.
4. Borodulin A.I., Desyatkov B.D., Makhov G.A., Sarmanaev S.R. Determination of the emission of swamp methane from the measured values of its concentration in the surface layer of the atmosphere. Meteorologiya i Gidrologiya . 1997;(1):66–74. (In Russ.)
5. Pyatkov S., Shilenkov D. Existence and uniqueness theorems in the inverse problem of recovering surface fluxes from pointwise measurements. Mathematics. 2022;10(9):1549.