{"title":"DYNAMICS AND VARIABILITY OF HIGH-MOUNTAIN GEOSYSTEMS OF THE SHARYN RIVER BASIN","authors":"B. Kerimbay","doi":"10.54668/2789-6323-2022-104-1-103-114","DOIUrl":null,"url":null,"abstract":"The study is based on a geosystem-basin approach, a method for determining the seasonal rhythm of the annual cycle, processing data from remote sensing of the Earth (ERS) and global monitoring in the integrated modules web browser of the digital platform (EOS). Spatial-temporal and seasonal linear NDVI series of key areas of high-mountain geosystems of the Sharyn river basin were constructed, and seasonal rhythms of the annual cycle were determined based on analytical data. As a result, a classification of the seasonal structure of the annual cycle was compiled, were revealedand the variability and dynamics of the geosystems of the nival-glacial belt above the snow line (3601...4100 m) and the high mountain belt (2601...3600 m).","PeriodicalId":256870,"journal":{"name":"Hydrometeorology and ecology","volume":"11 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-06-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Hydrometeorology and ecology","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.54668/2789-6323-2022-104-1-103-114","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 0
Abstract
The study is based on a geosystem-basin approach, a method for determining the seasonal rhythm of the annual cycle, processing data from remote sensing of the Earth (ERS) and global monitoring in the integrated modules web browser of the digital platform (EOS). Spatial-temporal and seasonal linear NDVI series of key areas of high-mountain geosystems of the Sharyn river basin were constructed, and seasonal rhythms of the annual cycle were determined based on analytical data. As a result, a classification of the seasonal structure of the annual cycle was compiled, were revealedand the variability and dynamics of the geosystems of the nival-glacial belt above the snow line (3601...4100 m) and the high mountain belt (2601...3600 m).
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