沙林河流域高山地质系统的动力学与变异性

B. Kerimbay
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引用次数: 0

摘要

该研究基于地球系统-盆地方法,这是一种确定年周期的季节节奏的方法,处理来自地球遥感(ERS)的数据,并在数字平台(EOS)的集成模块网络浏览器中进行全球监测。构建了沙林河流域高山地质系统重点区域的时空和季节线性NDVI序列,并在此基础上确定了年循环的季节规律。在此基础上,编制了年循环的季节结构分类,揭示了雪线以上(3601)初冰带地质系统的变率和动力学特征。4100米)和高山带(2601…3600米)。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
DYNAMICS AND VARIABILITY OF HIGH-MOUNTAIN GEOSYSTEMS OF THE SHARYN RIVER BASIN
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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