Brief communication: An ice-debris avalanche in the Nupchu Valley, Kanchenjunga Conservation Area, eastern Nepal
<p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred,...
Ausführliche Beschreibung
Autor*in: |
A. C. Byers [verfasserIn] M. Somos-Valenzuela [verfasserIn] D. H. Shugar [verfasserIn] D. McGrath [verfasserIn] M. B. Chand [verfasserIn] R. Avtar [verfasserIn] |
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E-Artikel |
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Sprache: |
Englisch |
Erschienen: |
2024 |
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Übergeordnetes Werk: |
In: The Cryosphere - Copernicus Publications, 2007, 18(2024), Seite 711-717 |
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Übergeordnetes Werk: |
volume:18 ; year:2024 ; pages:711-717 |
Links: |
Link aufrufen |
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DOI / URN: |
10.5194/tc-18-711-2024 |
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Katalog-ID: |
DOAJ092647162 |
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10.5194/tc-18-711-2024 doi (DE-627)DOAJ092647162 (DE-599)DOAJ574505ff080e41979a0137d7d968c387 DE-627 ger DE-627 rakwb eng GE1-350 QE1-996.5 A. C. Byers verfasserin aut Brief communication: An ice-debris avalanche in the Nupchu Valley, Kanchenjunga Conservation Area, eastern Nepal 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred, covering an area of 0.6 km<span class="inline-formula"<<sup<2</sup<</span< with a total estimated volume of order 10<span class="inline-formula"<<sup<6</sup<</span< m<span class="inline-formula"<<sup<3</sup<</span<. The area of the debris cone left by the August 2022 event increased the historic debris cone area by 0.2 km<span class="inline-formula"<<sup<2</sup<</span< (total area 0.6 km<span class="inline-formula"<<sup<2</sup<</span<). Although no human or livestock deaths occurred, the increase in torrent-like pulses of debris upon this historic debris cone since 2020 exemplifies a style of mass movement that may become increasingly common as air temperatures rise in the region. Although the magnitude of this event was small compared to events like the 2021 Chamoli avalanche, the widespread distribution and frequency of comparable events present a substantial, and potentially increasing, hazard across High Mountain Asia.</p< Environmental sciences Geology M. Somos-Valenzuela verfasserin aut D. H. Shugar verfasserin aut D. McGrath verfasserin aut M. B. Chand verfasserin aut R. Avtar verfasserin aut In The Cryosphere Copernicus Publications, 2007 18(2024), Seite 711-717 (DE-627)548126011 (DE-600)2393169-3 19940424 nnns volume:18 year:2024 pages:711-717 https://doi.org/10.5194/tc-18-711-2024 kostenfrei https://doaj.org/article/574505ff080e41979a0137d7d968c387 kostenfrei https://tc.copernicus.org/articles/18/711/2024/tc-18-711-2024.pdf kostenfrei https://doaj.org/toc/1994-0416 Journal toc kostenfrei https://doaj.org/toc/1994-0424 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 18 2024 711-717 |
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10.5194/tc-18-711-2024 doi (DE-627)DOAJ092647162 (DE-599)DOAJ574505ff080e41979a0137d7d968c387 DE-627 ger DE-627 rakwb eng GE1-350 QE1-996.5 A. C. Byers verfasserin aut Brief communication: An ice-debris avalanche in the Nupchu Valley, Kanchenjunga Conservation Area, eastern Nepal 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred, covering an area of 0.6 km<span class="inline-formula"<<sup<2</sup<</span< with a total estimated volume of order 10<span class="inline-formula"<<sup<6</sup<</span< m<span class="inline-formula"<<sup<3</sup<</span<. The area of the debris cone left by the August 2022 event increased the historic debris cone area by 0.2 km<span class="inline-formula"<<sup<2</sup<</span< (total area 0.6 km<span class="inline-formula"<<sup<2</sup<</span<). Although no human or livestock deaths occurred, the increase in torrent-like pulses of debris upon this historic debris cone since 2020 exemplifies a style of mass movement that may become increasingly common as air temperatures rise in the region. Although the magnitude of this event was small compared to events like the 2021 Chamoli avalanche, the widespread distribution and frequency of comparable events present a substantial, and potentially increasing, hazard across High Mountain Asia.</p< Environmental sciences Geology M. Somos-Valenzuela verfasserin aut D. H. Shugar verfasserin aut D. McGrath verfasserin aut M. B. Chand verfasserin aut R. Avtar verfasserin aut In The Cryosphere Copernicus Publications, 2007 18(2024), Seite 711-717 (DE-627)548126011 (DE-600)2393169-3 19940424 nnns volume:18 year:2024 pages:711-717 https://doi.org/10.5194/tc-18-711-2024 kostenfrei https://doaj.org/article/574505ff080e41979a0137d7d968c387 kostenfrei https://tc.copernicus.org/articles/18/711/2024/tc-18-711-2024.pdf kostenfrei https://doaj.org/toc/1994-0416 Journal toc kostenfrei https://doaj.org/toc/1994-0424 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 18 2024 711-717 |
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10.5194/tc-18-711-2024 doi (DE-627)DOAJ092647162 (DE-599)DOAJ574505ff080e41979a0137d7d968c387 DE-627 ger DE-627 rakwb eng GE1-350 QE1-996.5 A. C. Byers verfasserin aut Brief communication: An ice-debris avalanche in the Nupchu Valley, Kanchenjunga Conservation Area, eastern Nepal 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred, covering an area of 0.6 km<span class="inline-formula"<<sup<2</sup<</span< with a total estimated volume of order 10<span class="inline-formula"<<sup<6</sup<</span< m<span class="inline-formula"<<sup<3</sup<</span<. The area of the debris cone left by the August 2022 event increased the historic debris cone area by 0.2 km<span class="inline-formula"<<sup<2</sup<</span< (total area 0.6 km<span class="inline-formula"<<sup<2</sup<</span<). Although no human or livestock deaths occurred, the increase in torrent-like pulses of debris upon this historic debris cone since 2020 exemplifies a style of mass movement that may become increasingly common as air temperatures rise in the region. Although the magnitude of this event was small compared to events like the 2021 Chamoli avalanche, the widespread distribution and frequency of comparable events present a substantial, and potentially increasing, hazard across High Mountain Asia.</p< Environmental sciences Geology M. Somos-Valenzuela verfasserin aut D. H. Shugar verfasserin aut D. McGrath verfasserin aut M. B. Chand verfasserin aut R. Avtar verfasserin aut In The Cryosphere Copernicus Publications, 2007 18(2024), Seite 711-717 (DE-627)548126011 (DE-600)2393169-3 19940424 nnns volume:18 year:2024 pages:711-717 https://doi.org/10.5194/tc-18-711-2024 kostenfrei https://doaj.org/article/574505ff080e41979a0137d7d968c387 kostenfrei https://tc.copernicus.org/articles/18/711/2024/tc-18-711-2024.pdf kostenfrei https://doaj.org/toc/1994-0416 Journal toc kostenfrei https://doaj.org/toc/1994-0424 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 18 2024 711-717 |
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10.5194/tc-18-711-2024 doi (DE-627)DOAJ092647162 (DE-599)DOAJ574505ff080e41979a0137d7d968c387 DE-627 ger DE-627 rakwb eng GE1-350 QE1-996.5 A. C. Byers verfasserin aut Brief communication: An ice-debris avalanche in the Nupchu Valley, Kanchenjunga Conservation Area, eastern Nepal 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred, covering an area of 0.6 km<span class="inline-formula"<<sup<2</sup<</span< with a total estimated volume of order 10<span class="inline-formula"<<sup<6</sup<</span< m<span class="inline-formula"<<sup<3</sup<</span<. The area of the debris cone left by the August 2022 event increased the historic debris cone area by 0.2 km<span class="inline-formula"<<sup<2</sup<</span< (total area 0.6 km<span class="inline-formula"<<sup<2</sup<</span<). Although no human or livestock deaths occurred, the increase in torrent-like pulses of debris upon this historic debris cone since 2020 exemplifies a style of mass movement that may become increasingly common as air temperatures rise in the region. Although the magnitude of this event was small compared to events like the 2021 Chamoli avalanche, the widespread distribution and frequency of comparable events present a substantial, and potentially increasing, hazard across High Mountain Asia.</p< Environmental sciences Geology M. Somos-Valenzuela verfasserin aut D. H. Shugar verfasserin aut D. McGrath verfasserin aut M. B. Chand verfasserin aut R. Avtar verfasserin aut In The Cryosphere Copernicus Publications, 2007 18(2024), Seite 711-717 (DE-627)548126011 (DE-600)2393169-3 19940424 nnns volume:18 year:2024 pages:711-717 https://doi.org/10.5194/tc-18-711-2024 kostenfrei https://doaj.org/article/574505ff080e41979a0137d7d968c387 kostenfrei https://tc.copernicus.org/articles/18/711/2024/tc-18-711-2024.pdf kostenfrei https://doaj.org/toc/1994-0416 Journal toc kostenfrei https://doaj.org/toc/1994-0424 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 18 2024 711-717 |
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10.5194/tc-18-711-2024 doi (DE-627)DOAJ092647162 (DE-599)DOAJ574505ff080e41979a0137d7d968c387 DE-627 ger DE-627 rakwb eng GE1-350 QE1-996.5 A. C. Byers verfasserin aut Brief communication: An ice-debris avalanche in the Nupchu Valley, Kanchenjunga Conservation Area, eastern Nepal 2024 Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier <p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred, covering an area of 0.6 km<span class="inline-formula"<<sup<2</sup<</span< with a total estimated volume of order 10<span class="inline-formula"<<sup<6</sup<</span< m<span class="inline-formula"<<sup<3</sup<</span<. The area of the debris cone left by the August 2022 event increased the historic debris cone area by 0.2 km<span class="inline-formula"<<sup<2</sup<</span< (total area 0.6 km<span class="inline-formula"<<sup<2</sup<</span<). Although no human or livestock deaths occurred, the increase in torrent-like pulses of debris upon this historic debris cone since 2020 exemplifies a style of mass movement that may become increasingly common as air temperatures rise in the region. Although the magnitude of this event was small compared to events like the 2021 Chamoli avalanche, the widespread distribution and frequency of comparable events present a substantial, and potentially increasing, hazard across High Mountain Asia.</p< Environmental sciences Geology M. Somos-Valenzuela verfasserin aut D. H. Shugar verfasserin aut D. McGrath verfasserin aut M. B. Chand verfasserin aut R. Avtar verfasserin aut In The Cryosphere Copernicus Publications, 2007 18(2024), Seite 711-717 (DE-627)548126011 (DE-600)2393169-3 19940424 nnns volume:18 year:2024 pages:711-717 https://doi.org/10.5194/tc-18-711-2024 kostenfrei https://doaj.org/article/574505ff080e41979a0137d7d968c387 kostenfrei https://tc.copernicus.org/articles/18/711/2024/tc-18-711-2024.pdf kostenfrei https://doaj.org/toc/1994-0416 Journal toc kostenfrei https://doaj.org/toc/1994-0424 Journal toc kostenfrei GBV_USEFLAG_A SYSFLAG_A GBV_DOAJ GBV_ILN_11 GBV_ILN_20 GBV_ILN_22 GBV_ILN_23 GBV_ILN_24 GBV_ILN_31 GBV_ILN_39 GBV_ILN_40 GBV_ILN_60 GBV_ILN_62 GBV_ILN_63 GBV_ILN_65 GBV_ILN_69 GBV_ILN_70 GBV_ILN_73 GBV_ILN_95 GBV_ILN_105 GBV_ILN_110 GBV_ILN_151 GBV_ILN_161 GBV_ILN_170 GBV_ILN_206 GBV_ILN_213 GBV_ILN_230 GBV_ILN_267 GBV_ILN_285 GBV_ILN_293 GBV_ILN_370 GBV_ILN_602 GBV_ILN_2003 GBV_ILN_2005 GBV_ILN_2009 GBV_ILN_2011 GBV_ILN_2014 GBV_ILN_2055 GBV_ILN_2111 GBV_ILN_4012 GBV_ILN_4037 GBV_ILN_4112 GBV_ILN_4125 GBV_ILN_4126 GBV_ILN_4249 GBV_ILN_4305 GBV_ILN_4306 GBV_ILN_4307 GBV_ILN_4313 GBV_ILN_4322 GBV_ILN_4323 GBV_ILN_4324 GBV_ILN_4325 GBV_ILN_4335 GBV_ILN_4338 GBV_ILN_4367 GBV_ILN_4700 AR 18 2024 711-717 |
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<p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred, covering an area of 0.6 km<span class="inline-formula"<<sup<2</sup<</span< with a total estimated volume of order 10<span class="inline-formula"<<sup<6</sup<</span< m<span class="inline-formula"<<sup<3</sup<</span<. The area of the debris cone left by the August 2022 event increased the historic debris cone area by 0.2 km<span class="inline-formula"<<sup<2</sup<</span< (total area 0.6 km<span class="inline-formula"<<sup<2</sup<</span<). Although no human or livestock deaths occurred, the increase in torrent-like pulses of debris upon this historic debris cone since 2020 exemplifies a style of mass movement that may become increasingly common as air temperatures rise in the region. Although the magnitude of this event was small compared to events like the 2021 Chamoli avalanche, the widespread distribution and frequency of comparable events present a substantial, and potentially increasing, hazard across High Mountain Asia.</p< |
abstractGer |
<p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred, covering an area of 0.6 km<span class="inline-formula"<<sup<2</sup<</span< with a total estimated volume of order 10<span class="inline-formula"<<sup<6</sup<</span< m<span class="inline-formula"<<sup<3</sup<</span<. The area of the debris cone left by the August 2022 event increased the historic debris cone area by 0.2 km<span class="inline-formula"<<sup<2</sup<</span< (total area 0.6 km<span class="inline-formula"<<sup<2</sup<</span<). Although no human or livestock deaths occurred, the increase in torrent-like pulses of debris upon this historic debris cone since 2020 exemplifies a style of mass movement that may become increasingly common as air temperatures rise in the region. Although the magnitude of this event was small compared to events like the 2021 Chamoli avalanche, the widespread distribution and frequency of comparable events present a substantial, and potentially increasing, hazard across High Mountain Asia.</p< |
abstract_unstemmed |
<p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred, covering an area of 0.6 km<span class="inline-formula"<<sup<2</sup<</span< with a total estimated volume of order 10<span class="inline-formula"<<sup<6</sup<</span< m<span class="inline-formula"<<sup<3</sup<</span<. The area of the debris cone left by the August 2022 event increased the historic debris cone area by 0.2 km<span class="inline-formula"<<sup<2</sup<</span< (total area 0.6 km<span class="inline-formula"<<sup<2</sup<</span<). Although no human or livestock deaths occurred, the increase in torrent-like pulses of debris upon this historic debris cone since 2020 exemplifies a style of mass movement that may become increasingly common as air temperatures rise in the region. Although the magnitude of this event was small compared to events like the 2021 Chamoli avalanche, the widespread distribution and frequency of comparable events present a substantial, and potentially increasing, hazard across High Mountain Asia.</p< |
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Byers</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Brief communication: An ice-debris avalanche in the Nupchu Valley, Kanchenjunga Conservation Area, eastern Nepal</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2024</subfield></datafield><datafield tag="336" ind1=" " ind2=" "><subfield code="a">Text</subfield><subfield code="b">txt</subfield><subfield code="2">rdacontent</subfield></datafield><datafield tag="337" ind1=" " ind2=" "><subfield code="a">Computermedien</subfield><subfield code="b">c</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Online-Ressource</subfield><subfield code="b">cr</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a"><p<Beginning in December 2020, a series of small to medium, torrent-like pulses commenced upon a historic debris cone located within the Nupchu Valley, Kanchenjunga Conservation Area (KCA), Nepal. Sometime between 16 and 21 August 2022 a comparatively large ice-debris avalanche event occurred, covering an area of 0.6 km<span class="inline-formula"<<sup<2</sup<</span< with a total estimated volume of order 10<span class="inline-formula"<<sup<6</sup<</span< m<span class="inline-formula"<<sup<3</sup<</span<. The area of the debris cone left by the August 2022 event increased the historic debris cone area by 0.2 km<span class="inline-formula"<<sup<2</sup<</span< (total area 0.6 km<span class="inline-formula"<<sup<2</sup<</span<). Although no human or livestock deaths occurred, the increase in torrent-like pulses of debris upon this historic debris cone since 2020 exemplifies a style of mass movement that may become increasingly common as air temperatures rise in the region. Although the magnitude of this event was small compared to events like the 2021 Chamoli avalanche, the widespread distribution and frequency of comparable events present a substantial, and potentially increasing, hazard across High Mountain Asia.</p<</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Environmental sciences</subfield></datafield><datafield tag="653" ind1=" " ind2="0"><subfield code="a">Geology</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M. Somos-Valenzuela</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">D. H. Shugar</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">D. McGrath</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">M. B. Chand</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="0" ind2=" "><subfield code="a">R. Avtar</subfield><subfield code="e">verfasserin</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">In</subfield><subfield code="t">The Cryosphere</subfield><subfield code="d">Copernicus Publications, 2007</subfield><subfield code="g">18(2024), Seite 711-717</subfield><subfield code="w">(DE-627)548126011</subfield><subfield code="w">(DE-600)2393169-3</subfield><subfield code="x">19940424</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:18</subfield><subfield code="g">year:2024</subfield><subfield code="g">pages:711-717</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doi.org/10.5194/tc-18-711-2024</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://doaj.org/article/574505ff080e41979a0137d7d968c387</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="0"><subfield code="u">https://tc.copernicus.org/articles/18/711/2024/tc-18-711-2024.pdf</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1994-0416</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="856" ind1="4" ind2="2"><subfield code="u">https://doaj.org/toc/1994-0424</subfield><subfield code="y">Journal toc</subfield><subfield code="z">kostenfrei</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_USEFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SYSFLAG_A</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_DOAJ</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">GBV_ILN_11</subfield></datafield><datafield tag="912" 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