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Application of remote sensing and mathematical morphology of landscape for studying thermokarst processes

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Języki publikacji
EN
Abstrakty
EN
The purpose of this work is to study the development and regularity of morphological structures associated with thermokarst processes. An attempt is made to solve two problems, by analyzing the spatial regularity of morphological structures associated with thermokarst, and that of their dynamics. We use the method of landscape mathematical morphology - a branch of landscape science, investigating quantitative laws of landscape mosaics using methods of mathematical analysis of these mosaics. Investigation was carried out for five parcels in Siberia and Alaska. The analysis shows that a number of deductions from the proposed mathematical model for thermokarst lake plains are generally corroborated by empirical data.
Czasopismo
Rocznik
Tom
Strony
9--16
Opis fizyczny
Bibliogr. 13 poz., rys.
Twórcy
  • Sergeev Institute of Environmental Geoscience, Russian Academy of Sciences, Moscow, Russia,, vkapralova@gmail.com
Bibliografia
  • Are F.E., Balobaev V.T & Bosikov N.P., 1974. Fea¬tures of conversion of shores thermokarst lakes of the Central Yakutia. Lakes of permafrost of Siberia. Nauka, Novosibirsk (Арэ Ф.Э., Балобаев В.Т., Босиков Н.П., 1974. Особенности переработки берегов термокарстовых озер Центральной Якутии. Озера криолитозоны Сибири. Наука, Новосибирск).
  • Burn C.R. & Smith M.W., 1990. Development of Thermokarst Lakes During the Holocene at Sites Near Mayo, Yukon Territory. Permafrost and Periglacial Processes 1: 161-176.
  • Bartleman A.-P., Miyanishi K., Burn C.R. & Cote M.M., 2000. Development of Vegetation Communities in a Retrogressive Thaw Slump near Mayo, Yukon Territory: A 10-Year Assessment. Arctic 54(2): 149-156.
  • Ivashutina L.I. & Nikolaev V.A., 1969. About analysis of landscape structure of natural regions. Moscow University bulletin, Geography 4: 49-59. Ивашутина Л.И., Николаев В.А., 1969. К анализу ландшафтной структуры физико-географических регионов. Вестник МГУ, сер. геогр. 4: 49-59).
  • Kachurin S.P., 1961. Thermokarst overthe territory of the USSR. Moscow. Publishing house of Academy of Science of the USSR (Качурин СП., 1961. Термокарст на территории СССР. Издательство АН СССР, МоскЬа).
  • Perlstein G.Z., Levashov A.V. & Sergeev D.O., 2005. Analysis of thermokarst's early stage with deterministic methods. Transactions of the Second European Permafrost Conference. Potsdam.
  • Romanovsky N.N., 1977. Formation of polygon-vein structures. Nauka, Novosibirsk (Романовский Н.Н. Формирование полигонально-жильных структур. Наука, Новосибирск).
  • Simonov Yu.G., 1972. Regional geomorphological analysis. Moscow University: Moscow: 251 (Симонов Ю.Г., 1972. Региональный геоморфологический анализ. МГУ, МоскЬа: 251 с).
  • Viktorov A.S., 1998. Mathematical morphology of a landscape. Tratec, Moscow: 180 (Викторов А.С., 1998. Математическая морфология ландшафта. МоскЬа: 180 с).
  • Viktorov A.S., 2006. Main problems in mathematical morphology of a landscape. Nauka: Moscow: 252 (Викторов А.С, 2006. Основные проблемы математической морфологии ландшафта. МоскЬа, Наука: 252 с).
  • Viktorov A.S., 2007. Risk Assessment Based on the Mathematical Model of Diffuse Exogenous Geological Processes. Mathematical Geology. 39(8): 735-748.
  • Viktorov A.S., 2008. Methods of mathematical morphology of landscape. In: V. Andrejczuk (ed.) Methodology of landscape research. Pr. Kom. Krajobrazu Kulturowego PTG 9: 104-127.
  • Zolotarev G.S., 1983. Engineering geodynamics. Moscow University, Moscow: 328 (Золотарев Г.С., 1983. Инженерная геодинамика. МоскЬа, Изд-во МГУЮ: 328 с).
Typ dokumentu
Bibliografia
Identyfikator YADDA
bwmeta1.element.baztech-article-BUJ8-0026-0060
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