Remote assessment of natural hazards on the base of the mathematical morphology of landscape

A. Victorov, А. С. Викторов, T. Orlov, Т. В. Орлов, S. Sadkov, С.А. Садков, O. Trapeznikova, О.Н. Трапезникова
{"title":"Remote assessment of natural hazards on the base of the mathematical morphology of landscape","authors":"A. Victorov, А. С. Викторов, T. Orlov, Т. В. Орлов, S. Sadkov, С.А. Садков, O. Trapeznikova, О.Н. Трапезникова","doi":"10.31857/s0869-78092019561-73","DOIUrl":null,"url":null,"abstract":"The aim of this paper is to show approaches for the quantitative evaluation of natural hazards using the remote sensing data and basing on the results of the mathematical morphology of landscape. The mathematical model of the morphological pattern for lacustrine thermokarst plains with fluvial erosion was taken for the decision of the problem in case of an asynchronous start of the thermokarst process with the continuous generation of new thermokarst depressions. \nThe mathematical analysis of assumptions taken in the model gives us the regularities of the morphological pattern for the thermokarst plains with fluvial erosion including exponential distribution for khasyrei areas, integral-exponential distribution for lake areas, and the Poisson distribution for a quantity of either khasyreis or lakes within the key sites. Besides, analyzing the development of the territory in question by the approaches used in mathematical morphology of landscape we found out that in case of asynchronous start under very general conditions a dynamic equilibrium is established in generating thermokarst lakes and turning them into khasyreis after a long time. At the same time, the distribution density of thermokarst foci and their sizes, as well as process damage and the dimensions of khasyreis tend to some final levels specified by the expressions described above. \nThe results obtained were empirically tested at 17 key sites. Generally, the empirical testing shows that the asynchronous start takes place within thermokarst plains with fluvial erosion at a sufficient number of sites, and the theoretically obtained regulations are valid. \nThe regulations obtained were used for the mathematical solution of the probabilistic task for damage of a linear structure crossing the thermokarst plain with fluvial erosion.","PeriodicalId":309934,"journal":{"name":"Геоэкология. Инженерная геология. Гидрогеология. Геокриология","volume":"54 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2019-09-20","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Геоэкология. Инженерная геология. Гидрогеология. Геокриология","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.31857/s0869-78092019561-73","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 aim of this paper is to show approaches for the quantitative evaluation of natural hazards using the remote sensing data and basing on the results of the mathematical morphology of landscape. The mathematical model of the morphological pattern for lacustrine thermokarst plains with fluvial erosion was taken for the decision of the problem in case of an asynchronous start of the thermokarst process with the continuous generation of new thermokarst depressions. The mathematical analysis of assumptions taken in the model gives us the regularities of the morphological pattern for the thermokarst plains with fluvial erosion including exponential distribution for khasyrei areas, integral-exponential distribution for lake areas, and the Poisson distribution for a quantity of either khasyreis or lakes within the key sites. Besides, analyzing the development of the territory in question by the approaches used in mathematical morphology of landscape we found out that in case of asynchronous start under very general conditions a dynamic equilibrium is established in generating thermokarst lakes and turning them into khasyreis after a long time. At the same time, the distribution density of thermokarst foci and their sizes, as well as process damage and the dimensions of khasyreis tend to some final levels specified by the expressions described above. The results obtained were empirically tested at 17 key sites. Generally, the empirical testing shows that the asynchronous start takes place within thermokarst plains with fluvial erosion at a sufficient number of sites, and the theoretically obtained regulations are valid. The regulations obtained were used for the mathematical solution of the probabilistic task for damage of a linear structure crossing the thermokarst plain with fluvial erosion.
基于景观数学形态学的自然灾害远程评价
本文的目的是展示利用遥感数据和基于景观数学形态学结果的自然灾害定量评价方法。建立了河流侵蚀的湖相热岩溶平原的形态模式数学模型,用于确定热岩溶过程不同步启动并不断产生新的热岩溶洼地的问题。通过对模型假设的数学分析,得出了河流侵蚀热岩溶平原的形态分布规律,包括喀什湖地区的指数分布、湖泊地区的积分指数分布以及关键遗址内喀什湖或湖泊数量的泊松分布。此外,利用景观数学形态学的方法分析了该地区的发展情况,发现在非常一般的条件下,在非同步启动的情况下,热岩溶湖的产生和长时间后变成喀斯特湖的过程建立了动态平衡。同时,热岩溶焦点的分布密度和大小,以及过程损伤和khasyreis的尺寸都趋向于上述表达式所规定的最终水平。在17个关键位点对所得结果进行了实证检验。总的来说,经验检验表明,非同步启动发生在有足够数量的河流侵蚀的热岩溶平原内,理论得到的规律是有效的。将所得规律用于求解河流侵蚀热岩溶平原线性结构破坏的概率任务。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
自引率
0.00%
发文量
0
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:604180095
Book学术官方微信