基于哨兵-2 和卡诺普斯-V 图像组合的俄罗斯北极地区东部热卡湖大小分布研究

Pub Date : 2024-02-20 DOI:10.1134/s0001433823120150
I. N. Muratov, O. A. Baysalyamova, Y. M. Polishchuk
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引用次数: 0

摘要

摘要 本文专门对俄罗斯北极地区东部的热喀斯特湖泊的面积分布进行了遥感研究。研究在北极地区的东北冻原(NET)(雅库特)和楚科奇冻原(CT)进行,这两个地区在自然属性方面相对单一(此处称为生态区)。利用 2017-2021 年夏季获得的 Kanopus-V 和 Sentinel-2 卫星图像(空间分辨率分别为 2.1 米和 20 米),按区域对温卡湖泊的分布进行了遥感研究。对湖泊的解读使用了 Sentinel-2 卫星图像马赛克(全面覆盖研究区域)、12 个测试点的 Kanopus-V 图像以及 QGIS 3.22 工具。我们简要介绍了整合(组合)Kanopus-V 和 Sentinel-2 图像数据的方法,以绘制按湖泊大小划分的湖泊分布合成直方图。通过这种技术,我们可以获得所研究的北极生态区湖泊分布的直方图,湖泊面积从 50 到 108 平方米不等。直方图显示,两个生态区域的湖泊分布情况相似,都是湖泊面积越小,湖泊数量越多。图中显示,与 CT 相比,NET 中的湖泊面积更大,是湖泊数量的主要来源,这可能表明俄罗斯北极东部不同北极地区的地质气候条件存在显著差异。对这些地区的湖泊覆盖程度进行了评估。结果表明,楚科奇地区的湖泊覆盖率是所研究地区的 7 倍。
本文章由计算机程序翻译,如有差异,请以英文原文为准。

Study of Thermokarst Lake Size Distribution in the Eastern Part of the Russian Arctic Based on Combining Sentinel-2 and Kanopus-V Images

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Study of Thermokarst Lake Size Distribution in the Eastern Part of the Russian Arctic Based on Combining Sentinel-2 and Kanopus-V Images

Abstract

The article is devoted to remote studies of the size distribution of thermokarst lakes in the eastern part of the Russian Arctic. The studies are carried out in the Arctic territories of the Northeastern tundra (NET) (Yakutia) and the Chukotka tundra (CT), which are relatively homogeneous areas in terms of their natural properties (referred to here as ecoregions). Remote studies of the distribution of thermokarst lakes by area are conducted using satellite images from Kanopus-V and Sentinel-2 (with spatial resolutions of 2.1 and 20 m, respectively), obtained in the summer months of 2017–2021. The lakes are interpreted using a Sentinel-2 satellite image mosaic, which provides full coverage of the study territories; Kanopus-V images at 12 test sites; and QGIS 3.22 tools. We briefly describe the method of integration (combination) of data from Kanopus-V and Sentinel-2 images for plotting synthesized histograms of lakes distribution by their sizes. This technique allows us to get histograms of lake distribution in a very wide range of their sizes from 50 to 108 m2 in the studied Arctic ecoregions. The histogram plots show a similar behavior in both ecoregions, manifesting itself in an increase in the number of lakes as their size decreases. It is shown that the main contribution to the number of lakes in the NET is made by much larger lakes than in the CT, which may indicate a significant difference in the geocryological conditions in different Arctic territories of the eastern part of the Russian Arctic. The degree of the lake cover of the territories is assessed. It is shown that the lake cover of the NET is 7 times higher than in the studied territories of Chukotka.

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