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The influence of climatic factors on desertification processes on the example of the Terek-Kuma Lowland

https://doi.org/10.32786/2071-9485-2024-01-15

Abstract

Summary. The article presents the results of calculating the correlation between climatic factors and the dynamics of desertification. The data indicates an inverse and moderately strong correlation of -0.61. This means that as the GTK coefficient decreases, desertification area tends to increase. Conversely, during 2016 and 2019 when the GTK coefficient increased, there was a decrease in desertification area.

Introduction. Desertification is one of the main environmental problems in the south of Russia. To successfully combat desertification, it is required to identify all possible factors that affect the dynamics of land desertification. The article presents data on changes in the area of desertification, a study was conducted to identify the correlation between climate data and the area of desertification.

Object. territory of the Terek Kuma lowland.

Materials and methods. According to the research program, an analysis of the images of satellite images Lansat 8, 9 was carried out using the classification method "without training" according to the value of spectral-zonal channels. The work was carried out using ArcGIS PRO software. As a result, synthesized images of the study area were obtained, in which areas of desertification were identified and vectorized. On the basis of vector maps developed from multi-temporal images, a study of the dynamics of desertification was carried out. The area of desertification was calculated by years. The change during the study of climatic factors, in particular precipitation, was studied. The calculation of desertification areas from 2013 to 2021 was carried out. The calculation of the SCC index Selyaninova G. T. for the period 2013-2021. The correlation between the moistening of the territory by means of the GTK index and the area of desertification was calculated.

Results and conclusions. As a result, an inversely weak correlation of - 0.61 was revealed. With a decrease in the GTK coefficient, an increase in the area of desertification is observed. In 2016, 2019, when an increase in the value of the GTK coefficient was observed, a decrease in the area of desertification was also observed. There is an inverse correlation between the amount of precipitation and the dynamics of desertification, but there are other factors influencing this process.

About the Author

V. A. Romanov
Federal Research Center of Agroecology of the Russian Academy of Sciences
Russian Federation

Romanov Vladislav Aleksandrovich, Junior Researcher, Laboratory of Geoinformation Modeling and Mapping of Agroforestry Landscapes

Russian Federation, 400062, Volgograd, Universitetskiy Ave., 97 



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For citations:


Romanov V.A. The influence of climatic factors on desertification processes on the example of the Terek-Kuma Lowland. Title in english. 2024;(1 (73)):143-149. (In Russ.) https://doi.org/10.32786/2071-9485-2024-01-15

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