Assessment of rock glaciers and permafrost distribution in Uttarakhand, India

Abstract We have compiled an inventory of 1004 rock glaciers for Uttarakhand State, India, using high‐resolution satellite data freely available on Google Earth. The inventory is used to analyze the origin, spatial distribution, geometry and dynamics of rock glaciers using a combination of optical r...

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Published in:Permafrost and Periglacial Processes
Main Authors: Baral, Prashant, Haq, Mohd Anul, Yaragal, Shivaprakash
Other Authors: NIIT University
Format: Article in Journal/Newspaper
Language:English
Published: Wiley 2019
Subjects:
Online Access:http://dx.doi.org/10.1002/ppp.2008
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spelling crwiley:10.1002/ppp.2008 2024-10-06T13:52:05+00:00 Assessment of rock glaciers and permafrost distribution in Uttarakhand, India Baral, Prashant Haq, Mohd Anul Yaragal, Shivaprakash NIIT University 2019 http://dx.doi.org/10.1002/ppp.2008 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.2008 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.2008 https://onlinelibrary.wiley.com/doi/full-xml/10.1002/ppp.2008 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 31, issue 1, page 31-56 ISSN 1045-6740 1099-1530 journal-article 2019 crwiley https://doi.org/10.1002/ppp.2008 2024-09-23T04:37:41Z Abstract We have compiled an inventory of 1004 rock glaciers for Uttarakhand State, India, using high‐resolution satellite data freely available on Google Earth. The inventory is used to analyze the origin, spatial distribution, geometry and dynamics of rock glaciers using a combination of optical remote sensing techniques with a geographic information system (GIS). Results show that development of rock glaciers in this region depends strongly on high elevation (> 4000 m a.s.l.) and slope aspect. Rock glaciers are more dominant towards the southern quadrant (S, SE, SW) than the northern quadrant (N, NE, NW). A large number ( n = 608) of small (<0.5 km 2 ) rock glaciers originating from glacial moraine indicates glacial retreat in this region as one of the major causes for the formation of such a large number of rock glaciers. Median elevation of intact rock glaciers indicates that climatic conditions above 4600 m a.s.l. are suitable for the existence of permafrost in this region and that the lower limit of discontinuous permafrost gradually increases from west to east. Despite mean annual air temperatures below 0°C, increasing mean temperatures during warmest quarter of the year could be a strong controlling factor for permafrost thawing in the region. Logistic regression modeling using WorldClim version 2 climate data sets and Moderate Resolution Imaging Spectroradiometer (MODIS) land surface temperature (LST) data show that these models can produce fairly reliable estimates of permafrost probability in the studied area. MODIS LST climate data sets can be crucial for mapping and monitoring permafrost in the region. Article in Journal/Newspaper permafrost Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 31 1 31 56
institution Open Polar
collection Wiley Online Library
op_collection_id crwiley
language English
description Abstract We have compiled an inventory of 1004 rock glaciers for Uttarakhand State, India, using high‐resolution satellite data freely available on Google Earth. The inventory is used to analyze the origin, spatial distribution, geometry and dynamics of rock glaciers using a combination of optical remote sensing techniques with a geographic information system (GIS). Results show that development of rock glaciers in this region depends strongly on high elevation (> 4000 m a.s.l.) and slope aspect. Rock glaciers are more dominant towards the southern quadrant (S, SE, SW) than the northern quadrant (N, NE, NW). A large number ( n = 608) of small (<0.5 km 2 ) rock glaciers originating from glacial moraine indicates glacial retreat in this region as one of the major causes for the formation of such a large number of rock glaciers. Median elevation of intact rock glaciers indicates that climatic conditions above 4600 m a.s.l. are suitable for the existence of permafrost in this region and that the lower limit of discontinuous permafrost gradually increases from west to east. Despite mean annual air temperatures below 0°C, increasing mean temperatures during warmest quarter of the year could be a strong controlling factor for permafrost thawing in the region. Logistic regression modeling using WorldClim version 2 climate data sets and Moderate Resolution Imaging Spectroradiometer (MODIS) land surface temperature (LST) data show that these models can produce fairly reliable estimates of permafrost probability in the studied area. MODIS LST climate data sets can be crucial for mapping and monitoring permafrost in the region.
author2 NIIT University
format Article in Journal/Newspaper
author Baral, Prashant
Haq, Mohd Anul
Yaragal, Shivaprakash
spellingShingle Baral, Prashant
Haq, Mohd Anul
Yaragal, Shivaprakash
Assessment of rock glaciers and permafrost distribution in Uttarakhand, India
author_facet Baral, Prashant
Haq, Mohd Anul
Yaragal, Shivaprakash
author_sort Baral, Prashant
title Assessment of rock glaciers and permafrost distribution in Uttarakhand, India
title_short Assessment of rock glaciers and permafrost distribution in Uttarakhand, India
title_full Assessment of rock glaciers and permafrost distribution in Uttarakhand, India
title_fullStr Assessment of rock glaciers and permafrost distribution in Uttarakhand, India
title_full_unstemmed Assessment of rock glaciers and permafrost distribution in Uttarakhand, India
title_sort assessment of rock glaciers and permafrost distribution in uttarakhand, india
publisher Wiley
publishDate 2019
url http://dx.doi.org/10.1002/ppp.2008
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genre permafrost
Permafrost and Periglacial Processes
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Permafrost and Periglacial Processes
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volume 31, issue 1, page 31-56
ISSN 1045-6740 1099-1530
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op_doi https://doi.org/10.1002/ppp.2008
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