Rockfall activity in the Kangchenjunga area, Nepal Himalaya
Abstract Rockfall activity and related environmental factors (i.e. bedrock thermal regime and precipitation) were monitored through most of one year at elevations between 4600 m and 6800 m in the Kangchenjunga valley of the Nepal Himalaya to identify rockfall dynamics, estimate rockfall frequency fo...
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crwiley:10.1002/ppp.664 2024-09-15T18:30:16+00:00 Rockfall activity in the Kangchenjunga area, Nepal Himalaya Regmi, Dhananjay Watanabe, Teiji Japan Science Society Tokachi Mainichi Newspaper Co., Japan 2009 http://dx.doi.org/10.1002/ppp.664 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.664 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.664 en eng Wiley http://onlinelibrary.wiley.com/termsAndConditions#vor Permafrost and Periglacial Processes volume 20, issue 4, page 390-398 ISSN 1045-6740 1099-1530 journal-article 2009 crwiley https://doi.org/10.1002/ppp.664 2024-08-22T04:16:10Z Abstract Rockfall activity and related environmental factors (i.e. bedrock thermal regime and precipitation) were monitored through most of one year at elevations between 4600 m and 6800 m in the Kangchenjunga valley of the Nepal Himalaya to identify rockfall dynamics, estimate rockfall frequency for different aspects, and assess temporal and spatial variations in rockfall activity. Rockfall activity on north‐facing slopes is mainly controlled by insolation relating to solar elevation and showed an abrupt increase in the pre‐monsoon season. Rockfall activity on east‐, west‐ and south‐facing slopes is controlled by the duration and effectiveness of sunshine and accumulation of snow. The north‐facing slope has a small diurnal range of rock surface temperatures and exhibits seasonal freeze‐thaw, whereas the other aspects show frequent diurnal freeze‐thaw. These differences result in seasonal rockfall activity on the north‐facing slope and the infrequent release of large debris and year‐round rockfall activity on the other aspects. Copyright © 2009 John Wiley & Sons, Ltd. Article in Journal/Newspaper Permafrost and Periglacial Processes Wiley Online Library Permafrost and Periglacial Processes 20 4 390 398 |
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English |
description |
Abstract Rockfall activity and related environmental factors (i.e. bedrock thermal regime and precipitation) were monitored through most of one year at elevations between 4600 m and 6800 m in the Kangchenjunga valley of the Nepal Himalaya to identify rockfall dynamics, estimate rockfall frequency for different aspects, and assess temporal and spatial variations in rockfall activity. Rockfall activity on north‐facing slopes is mainly controlled by insolation relating to solar elevation and showed an abrupt increase in the pre‐monsoon season. Rockfall activity on east‐, west‐ and south‐facing slopes is controlled by the duration and effectiveness of sunshine and accumulation of snow. The north‐facing slope has a small diurnal range of rock surface temperatures and exhibits seasonal freeze‐thaw, whereas the other aspects show frequent diurnal freeze‐thaw. These differences result in seasonal rockfall activity on the north‐facing slope and the infrequent release of large debris and year‐round rockfall activity on the other aspects. Copyright © 2009 John Wiley & Sons, Ltd. |
author2 |
Japan Science Society Tokachi Mainichi Newspaper Co., Japan |
format |
Article in Journal/Newspaper |
author |
Regmi, Dhananjay Watanabe, Teiji |
spellingShingle |
Regmi, Dhananjay Watanabe, Teiji Rockfall activity in the Kangchenjunga area, Nepal Himalaya |
author_facet |
Regmi, Dhananjay Watanabe, Teiji |
author_sort |
Regmi, Dhananjay |
title |
Rockfall activity in the Kangchenjunga area, Nepal Himalaya |
title_short |
Rockfall activity in the Kangchenjunga area, Nepal Himalaya |
title_full |
Rockfall activity in the Kangchenjunga area, Nepal Himalaya |
title_fullStr |
Rockfall activity in the Kangchenjunga area, Nepal Himalaya |
title_full_unstemmed |
Rockfall activity in the Kangchenjunga area, Nepal Himalaya |
title_sort |
rockfall activity in the kangchenjunga area, nepal himalaya |
publisher |
Wiley |
publishDate |
2009 |
url |
http://dx.doi.org/10.1002/ppp.664 https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fppp.664 https://onlinelibrary.wiley.com/doi/pdf/10.1002/ppp.664 |
genre |
Permafrost and Periglacial Processes |
genre_facet |
Permafrost and Periglacial Processes |
op_source |
Permafrost and Periglacial Processes volume 20, issue 4, page 390-398 ISSN 1045-6740 1099-1530 |
op_rights |
http://onlinelibrary.wiley.com/termsAndConditions#vor |
op_doi |
https://doi.org/10.1002/ppp.664 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
20 |
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4 |
container_start_page |
390 |
op_container_end_page |
398 |
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1810471738310393856 |