Mapping Mountain Permafrost Landscapes in Siberia Using Landsat Thermal Imagery

Intensive development of South Yakutia, a mountainous area in the Russian sporadic permafrost zone, must be founded on knowledge about regional permafrost conditions. New permafrost maps for mountainous areas in South Yakutia (the Elkon Mountains and the Olekma-Chara Upland) are presented that provi...

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Main Authors: Svetlana V. Kalinicheva, Alexander N. Fedorov, Mikhail N. Zhelezniak
Format: Article
Language:English
Published: MDPI AG 2018-12-01
Series:Geosciences
Subjects:
LST
Online Access:https://www.mdpi.com/2076-3263/9/1/4
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spelling doaj-07a9c9849a5b4168a84ec04ee42eb7202020-11-24T23:41:10ZengMDPI AGGeosciences2076-32632018-12-0191410.3390/geosciences9010004geosciences9010004Mapping Mountain Permafrost Landscapes in Siberia Using Landsat Thermal ImagerySvetlana V. Kalinicheva0Alexander N. Fedorov1Mikhail N. Zhelezniak2Melnikov Permafrost Institute SB RAS, Merzlotnaya str.,36, 677010 Yakutsk, RussiaMelnikov Permafrost Institute SB RAS, Merzlotnaya str.,36, 677010 Yakutsk, RussiaMelnikov Permafrost Institute SB RAS, Merzlotnaya str.,36, 677010 Yakutsk, RussiaIntensive development of South Yakutia, a mountainous area in the Russian sporadic permafrost zone, must be founded on knowledge about regional permafrost conditions. New permafrost maps for mountainous areas in South Yakutia (the Elkon Mountains and the Olekma-Chara Upland) are presented that provide a more detailed and updated description of permafrost distribution in the area than those that were hitherto available. These maps are based on the previously-developed and tested method of detecting permafrost and unfrozen ground using Landsat-5/TM satellite data with relatively high resolution. The method represents a scheme for permafrost identification based on a set of landscape indicators: terrain elevation, slope angle and exposition, vegetation, snow cover, and land surface temperature (LST). A correlation analysis of satellite data to full-scale field data has been carried out for the two areas under consideration. Indicator properties of LST obtained by Landsat-5/TM Band 6 Infrared have been characterized in detail for detection and regional mapping of permafrost. The effect of landscape factors (landscape cryo-indicators) on ground temperature and condition, frozen or unfrozen reflected in LST intensity, is demonstrated.https://www.mdpi.com/2076-3263/9/1/4South Yakutialandscape indication methodpermafrost mappingLandsatsatellite imagesthermal infrared imageryLST
collection DOAJ
language English
format Article
sources DOAJ
author Svetlana V. Kalinicheva
Alexander N. Fedorov
Mikhail N. Zhelezniak
spellingShingle Svetlana V. Kalinicheva
Alexander N. Fedorov
Mikhail N. Zhelezniak
Mapping Mountain Permafrost Landscapes in Siberia Using Landsat Thermal Imagery
Geosciences
South Yakutia
landscape indication method
permafrost mapping
Landsat
satellite images
thermal infrared imagery
LST
author_facet Svetlana V. Kalinicheva
Alexander N. Fedorov
Mikhail N. Zhelezniak
author_sort Svetlana V. Kalinicheva
title Mapping Mountain Permafrost Landscapes in Siberia Using Landsat Thermal Imagery
title_short Mapping Mountain Permafrost Landscapes in Siberia Using Landsat Thermal Imagery
title_full Mapping Mountain Permafrost Landscapes in Siberia Using Landsat Thermal Imagery
title_fullStr Mapping Mountain Permafrost Landscapes in Siberia Using Landsat Thermal Imagery
title_full_unstemmed Mapping Mountain Permafrost Landscapes in Siberia Using Landsat Thermal Imagery
title_sort mapping mountain permafrost landscapes in siberia using landsat thermal imagery
publisher MDPI AG
series Geosciences
issn 2076-3263
publishDate 2018-12-01
description Intensive development of South Yakutia, a mountainous area in the Russian sporadic permafrost zone, must be founded on knowledge about regional permafrost conditions. New permafrost maps for mountainous areas in South Yakutia (the Elkon Mountains and the Olekma-Chara Upland) are presented that provide a more detailed and updated description of permafrost distribution in the area than those that were hitherto available. These maps are based on the previously-developed and tested method of detecting permafrost and unfrozen ground using Landsat-5/TM satellite data with relatively high resolution. The method represents a scheme for permafrost identification based on a set of landscape indicators: terrain elevation, slope angle and exposition, vegetation, snow cover, and land surface temperature (LST). A correlation analysis of satellite data to full-scale field data has been carried out for the two areas under consideration. Indicator properties of LST obtained by Landsat-5/TM Band 6 Infrared have been characterized in detail for detection and regional mapping of permafrost. The effect of landscape factors (landscape cryo-indicators) on ground temperature and condition, frozen or unfrozen reflected in LST intensity, is demonstrated.
topic South Yakutia
landscape indication method
permafrost mapping
Landsat
satellite images
thermal infrared imagery
LST
url https://www.mdpi.com/2076-3263/9/1/4
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AT alexandernfedorov mappingmountainpermafrostlandscapesinsiberiausinglandsatthermalimagery
AT mikhailnzhelezniak mappingmountainpermafrostlandscapesinsiberiausinglandsatthermalimagery
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