MAIN CHARACTERISTICS OF CHANGES IN RIVER RUNOFF IN A LONG-TERM SECTION ACROSS THE TERRITORY OF THE REPUBLIC OF BASHKORTOSTAN

Abstract

The article reveals the main characteristics of the change in the values of the river runoff layer indicator in the long-term section across the territory of the Republic of Bashkortostan. In previously published works related to 1990-2000, the statistical parameters of river runoff are considered without taking into account the changes that have occurred in the general population of the initial information. It is noted in the article that the calculations and estimates for the study of the peculiarities of changes in hydrometeorological conditions, carried out by us in recent years, indicate a violation of the homogeneity of the observation series. At the same time, attention is drawn to the fact that this trend is dependent on the influence of factors associated with global climate change. The article indicates that ignoring the facts reflecting the ongoing changes can affect not only the accuracy of the calculations, but also lead to the adoption of incorrect and unjustified decisions in the water sector and the assessment of environmental conditions in watercourses. The analysis was carried out according to the values of the annual runoff layer, the change in the indicators of the annual runoff of the rivers of the republic was calculated for two time intervals. As the boundary conditions between them, the year was taken, from which a rather clear tendency of the trend change in terms of the annual runoff values is revealed. Cartographic analysis of the information obtained was carried out using the ArcGIS software package. It has been established that during the period of noticeable climatic changes in most of the territory of the republic, there is a tendency to an increase in the values of the annual runoff layer. At the same time, the greatest indicators of change occur on the western slopes of the Southern Urals and the Ufa plateau within the republic. It was found that a noticeable decrease in the values of the annual runoff layer is observed over the territory of the Bashkir Trans-Urals.