Comparative characteristics of the wind regime on the sandy massifs of Western Turkmenistan and the Mangystau Peninsula and its influence on the development of deflation processes)

Abstract

A comparative description of the long-term indicators of the wind regime and their influence on the intensity of the development of deflationary processes in the eolian forms of Western Turkmenistan and the Mangystau Peninsula is given. A comprehensive analysis of the wind regime at six meteorological stations of the studied territory was carried out with indicators of the average annual wind speed and predictive quantitative data on the transfer of sand to develop effective methods for protecting various types of engineering objects from sand drifts and blowing.