Geomorphic effects of recurrent outburst superfloods in the Yigong River on the southeastern margin of Tibet

Abstract Landslide dam outburst floods have a significant impact on landform evolution in high mountainous areas. Historic landslide dams on the Yigong River, southeastern Tibet, generated two outburst superfloods > 105 m3/s in 1902 and 2000 AD. One of the slackwater deposits, which was newly fou...

Descripción completa

Guardado en:
Detalles Bibliográficos
Autores principales: Kaiheng Hu, Chaohua Wu, Li Wei, Xiaopeng Zhang, Qiyuan Zhang, Weiming Liu, Brian J. Yanites
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2021
Materias:
R
Q
Acceso en línea:https://doaj.org/article/170e3f7d61e74127b7a653b9abafa666
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
id oai:doaj.org-article:170e3f7d61e74127b7a653b9abafa666
record_format dspace
spelling oai:doaj.org-article:170e3f7d61e74127b7a653b9abafa6662021-12-02T17:06:32ZGeomorphic effects of recurrent outburst superfloods in the Yigong River on the southeastern margin of Tibet10.1038/s41598-021-95194-12045-2322https://doaj.org/article/170e3f7d61e74127b7a653b9abafa6662021-08-01T00:00:00Zhttps://doi.org/10.1038/s41598-021-95194-1https://doaj.org/toc/2045-2322Abstract Landslide dam outburst floods have a significant impact on landform evolution in high mountainous areas. Historic landslide dams on the Yigong River, southeastern Tibet, generated two outburst superfloods > 105 m3/s in 1902 and 2000 AD. One of the slackwater deposits, which was newly found immediately downstream of the historic dams, has been dated to 7 ka BP. The one-dimensional backwater stepwise method gives an estimate of 225,000 m3/s for the peak flow related to the paleo-stage indicator of 7 ka BP. The recurrence of at least three large landslide dam impoundments and super-outburst floods at the exit of Yigong Lake during the Holocene greatly changed the morphology of the Yigong River. More than 0.26 billion m3 of sediment has been aggraded in the dammed lake while the landslide sediment doubles the channel slope behind the dam. Repeated landslide damming may be a persistent source of outburst floods and impede the upstream migration of river knickpoints in the southeastern margin of Tibet.Kaiheng HuChaohua WuLi WeiXiaopeng ZhangQiyuan ZhangWeiming LiuBrian J. YanitesNature PortfolioarticleMedicineRScienceQENScientific Reports, Vol 11, Iss 1, Pp 1-11 (2021)
institution DOAJ
collection DOAJ
language EN
topic Medicine
R
Science
Q
spellingShingle Medicine
R
Science
Q
Kaiheng Hu
Chaohua Wu
Li Wei
Xiaopeng Zhang
Qiyuan Zhang
Weiming Liu
Brian J. Yanites
Geomorphic effects of recurrent outburst superfloods in the Yigong River on the southeastern margin of Tibet
description Abstract Landslide dam outburst floods have a significant impact on landform evolution in high mountainous areas. Historic landslide dams on the Yigong River, southeastern Tibet, generated two outburst superfloods > 105 m3/s in 1902 and 2000 AD. One of the slackwater deposits, which was newly found immediately downstream of the historic dams, has been dated to 7 ka BP. The one-dimensional backwater stepwise method gives an estimate of 225,000 m3/s for the peak flow related to the paleo-stage indicator of 7 ka BP. The recurrence of at least three large landslide dam impoundments and super-outburst floods at the exit of Yigong Lake during the Holocene greatly changed the morphology of the Yigong River. More than 0.26 billion m3 of sediment has been aggraded in the dammed lake while the landslide sediment doubles the channel slope behind the dam. Repeated landslide damming may be a persistent source of outburst floods and impede the upstream migration of river knickpoints in the southeastern margin of Tibet.
format article
author Kaiheng Hu
Chaohua Wu
Li Wei
Xiaopeng Zhang
Qiyuan Zhang
Weiming Liu
Brian J. Yanites
author_facet Kaiheng Hu
Chaohua Wu
Li Wei
Xiaopeng Zhang
Qiyuan Zhang
Weiming Liu
Brian J. Yanites
author_sort Kaiheng Hu
title Geomorphic effects of recurrent outburst superfloods in the Yigong River on the southeastern margin of Tibet
title_short Geomorphic effects of recurrent outburst superfloods in the Yigong River on the southeastern margin of Tibet
title_full Geomorphic effects of recurrent outburst superfloods in the Yigong River on the southeastern margin of Tibet
title_fullStr Geomorphic effects of recurrent outburst superfloods in the Yigong River on the southeastern margin of Tibet
title_full_unstemmed Geomorphic effects of recurrent outburst superfloods in the Yigong River on the southeastern margin of Tibet
title_sort geomorphic effects of recurrent outburst superfloods in the yigong river on the southeastern margin of tibet
publisher Nature Portfolio
publishDate 2021
url https://doaj.org/article/170e3f7d61e74127b7a653b9abafa666
work_keys_str_mv AT kaihenghu geomorphiceffectsofrecurrentoutburstsuperfloodsintheyigongriveronthesoutheasternmarginoftibet
AT chaohuawu geomorphiceffectsofrecurrentoutburstsuperfloodsintheyigongriveronthesoutheasternmarginoftibet
AT liwei geomorphiceffectsofrecurrentoutburstsuperfloodsintheyigongriveronthesoutheasternmarginoftibet
AT xiaopengzhang geomorphiceffectsofrecurrentoutburstsuperfloodsintheyigongriveronthesoutheasternmarginoftibet
AT qiyuanzhang geomorphiceffectsofrecurrentoutburstsuperfloodsintheyigongriveronthesoutheasternmarginoftibet
AT weimingliu geomorphiceffectsofrecurrentoutburstsuperfloodsintheyigongriveronthesoutheasternmarginoftibet
AT brianjyanites geomorphiceffectsofrecurrentoutburstsuperfloodsintheyigongriveronthesoutheasternmarginoftibet
_version_ 1718381540425072640