Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau
Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper...
Ausführliche Beschreibung
Gespeichert in:
| Autor*in: |
Ma, Junxue [verfasserIn] |
|---|
| Format: |
Artikel |
|---|---|
| Sprache: |
Englisch |
| Erschienen: |
2022 |
|---|
| Schlagwörter: |
|---|
| Anmerkung: |
© The Author(s), under exclusive licence to Springer Nature B.V. 2022 |
|---|
| Übergeordnetes Werk: |
Enthalten in: Natural hazards - Springer Netherlands, 1988, 112(2022), 2 vom: 06. Feb., Seite 1191-1221 |
|---|---|
| Übergeordnetes Werk: |
volume:112 ; year:2022 ; number:2 ; day:06 ; month:02 ; pages:1191-1221 |
| Links: |
|---|
| DOI / URN: |
10.1007/s11069-022-05223-z |
|---|
| Katalog-ID: |
OLC2078737674 |
|---|
| LEADER | 01000caa a22002652 4500 | ||
|---|---|---|---|
| 001 | OLC2078737674 | ||
| 003 | DE-627 | ||
| 005 | 20230506024149.0 | ||
| 007 | tu | ||
| 008 | 221220s2022 xx ||||| 00| ||eng c | ||
| 024 | 7 | |a 10.1007/s11069-022-05223-z |2 doi | |
| 035 | |a (DE-627)OLC2078737674 | ||
| 035 | |a (DE-He213)s11069-022-05223-z-p | ||
| 040 | |a DE-627 |b ger |c DE-627 |e rakwb | ||
| 041 | |a eng | ||
| 082 | 0 | 4 | |a 550 |q VZ |
| 084 | |a 14 |2 ssgn | ||
| 100 | 1 | |a Ma, Junxue |e verfasserin |0 (orcid)0000-0002-1922-2880 |4 aut | |
| 245 | 1 | 0 | |a Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau |
| 264 | 1 | |c 2022 | |
| 336 | |a Text |b txt |2 rdacontent | ||
| 337 | |a ohne Hilfsmittel zu benutzen |b n |2 rdamedia | ||
| 338 | |a Band |b nc |2 rdacarrier | ||
| 500 | |a © The Author(s), under exclusive licence to Springer Nature B.V. 2022 | ||
| 520 | |a Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years. | ||
| 650 | 4 | |a Landslide dam | |
| 650 | 4 | |a Ancient dammed lake | |
| 650 | 4 | |a Landslide-dammed lake outburst floods (LLOFs) | |
| 650 | 4 | |a Peak discharge | |
| 650 | 4 | |a Uncertainty assessment | |
| 700 | 1 | |a Chen, Jian |0 (orcid)0000-0002-3323-7560 |4 aut | |
| 700 | 1 | |a Cui, Zhijiu |0 (orcid)0000-0003-0306-0909 |4 aut | |
| 700 | 1 | |a Zhou, Wendy |4 aut | |
| 700 | 1 | |a Chen, Ruichen |0 (orcid)0000-0001-7988-8900 |4 aut | |
| 700 | 1 | |a Wang, Chengbiao |4 aut | |
| 773 | 0 | 8 | |i Enthalten in |t Natural hazards |d Springer Netherlands, 1988 |g 112(2022), 2 vom: 06. Feb., Seite 1191-1221 |w (DE-627)131010271 |w (DE-600)1088547-X |w (DE-576)03285272X |x 0921-030X |7 nnns |
| 773 | 1 | 8 | |g volume:112 |g year:2022 |g number:2 |g day:06 |g month:02 |g pages:1191-1221 |
| 856 | 4 | 1 | |u https://doi.org/10.1007/s11069-022-05223-z |z lizenzpflichtig |3 Volltext |
| 912 | |a GBV_USEFLAG_A | ||
| 912 | |a SYSFLAG_A | ||
| 912 | |a GBV_OLC | ||
| 912 | |a SSG-OLC-PHY | ||
| 912 | |a SSG-OLC-MAT | ||
| 912 | |a SSG-OPC-GGO | ||
| 912 | |a SSG-OPC-MAT | ||
| 951 | |a AR | ||
| 952 | |d 112 |j 2022 |e 2 |b 06 |c 02 |h 1191-1221 | ||
| author_variant |
j m jm j c jc z c zc w z wz r c rc c w cw |
|---|---|
| matchkey_str |
article:0921030X:2022----::eosrcinfaatohcubrtlosfhdeininlnsieamdaenhupri |
| hierarchy_sort_str |
2022 |
| publishDate |
2022 |
| allfields |
10.1007/s11069-022-05223-z doi (DE-627)OLC2078737674 (DE-He213)s11069-022-05223-z-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Ma, Junxue verfasserin (orcid)0000-0002-1922-2880 aut Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years. Landslide dam Ancient dammed lake Landslide-dammed lake outburst floods (LLOFs) Peak discharge Uncertainty assessment Chen, Jian (orcid)0000-0002-3323-7560 aut Cui, Zhijiu (orcid)0000-0003-0306-0909 aut Zhou, Wendy aut Chen, Ruichen (orcid)0000-0001-7988-8900 aut Wang, Chengbiao aut Enthalten in Natural hazards Springer Netherlands, 1988 112(2022), 2 vom: 06. Feb., Seite 1191-1221 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:112 year:2022 number:2 day:06 month:02 pages:1191-1221 https://doi.org/10.1007/s11069-022-05223-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 112 2022 2 06 02 1191-1221 |
| spelling |
10.1007/s11069-022-05223-z doi (DE-627)OLC2078737674 (DE-He213)s11069-022-05223-z-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Ma, Junxue verfasserin (orcid)0000-0002-1922-2880 aut Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years. Landslide dam Ancient dammed lake Landslide-dammed lake outburst floods (LLOFs) Peak discharge Uncertainty assessment Chen, Jian (orcid)0000-0002-3323-7560 aut Cui, Zhijiu (orcid)0000-0003-0306-0909 aut Zhou, Wendy aut Chen, Ruichen (orcid)0000-0001-7988-8900 aut Wang, Chengbiao aut Enthalten in Natural hazards Springer Netherlands, 1988 112(2022), 2 vom: 06. Feb., Seite 1191-1221 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:112 year:2022 number:2 day:06 month:02 pages:1191-1221 https://doi.org/10.1007/s11069-022-05223-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 112 2022 2 06 02 1191-1221 |
| allfields_unstemmed |
10.1007/s11069-022-05223-z doi (DE-627)OLC2078737674 (DE-He213)s11069-022-05223-z-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Ma, Junxue verfasserin (orcid)0000-0002-1922-2880 aut Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years. Landslide dam Ancient dammed lake Landslide-dammed lake outburst floods (LLOFs) Peak discharge Uncertainty assessment Chen, Jian (orcid)0000-0002-3323-7560 aut Cui, Zhijiu (orcid)0000-0003-0306-0909 aut Zhou, Wendy aut Chen, Ruichen (orcid)0000-0001-7988-8900 aut Wang, Chengbiao aut Enthalten in Natural hazards Springer Netherlands, 1988 112(2022), 2 vom: 06. Feb., Seite 1191-1221 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:112 year:2022 number:2 day:06 month:02 pages:1191-1221 https://doi.org/10.1007/s11069-022-05223-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 112 2022 2 06 02 1191-1221 |
| allfieldsGer |
10.1007/s11069-022-05223-z doi (DE-627)OLC2078737674 (DE-He213)s11069-022-05223-z-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Ma, Junxue verfasserin (orcid)0000-0002-1922-2880 aut Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years. Landslide dam Ancient dammed lake Landslide-dammed lake outburst floods (LLOFs) Peak discharge Uncertainty assessment Chen, Jian (orcid)0000-0002-3323-7560 aut Cui, Zhijiu (orcid)0000-0003-0306-0909 aut Zhou, Wendy aut Chen, Ruichen (orcid)0000-0001-7988-8900 aut Wang, Chengbiao aut Enthalten in Natural hazards Springer Netherlands, 1988 112(2022), 2 vom: 06. Feb., Seite 1191-1221 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:112 year:2022 number:2 day:06 month:02 pages:1191-1221 https://doi.org/10.1007/s11069-022-05223-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 112 2022 2 06 02 1191-1221 |
| allfieldsSound |
10.1007/s11069-022-05223-z doi (DE-627)OLC2078737674 (DE-He213)s11069-022-05223-z-p DE-627 ger DE-627 rakwb eng 550 VZ 14 ssgn Ma, Junxue verfasserin (orcid)0000-0002-1922-2880 aut Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau 2022 Text txt rdacontent ohne Hilfsmittel zu benutzen n rdamedia Band nc rdacarrier © The Author(s), under exclusive licence to Springer Nature B.V. 2022 Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years. Landslide dam Ancient dammed lake Landslide-dammed lake outburst floods (LLOFs) Peak discharge Uncertainty assessment Chen, Jian (orcid)0000-0002-3323-7560 aut Cui, Zhijiu (orcid)0000-0003-0306-0909 aut Zhou, Wendy aut Chen, Ruichen (orcid)0000-0001-7988-8900 aut Wang, Chengbiao aut Enthalten in Natural hazards Springer Netherlands, 1988 112(2022), 2 vom: 06. Feb., Seite 1191-1221 (DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X 0921-030X nnns volume:112 year:2022 number:2 day:06 month:02 pages:1191-1221 https://doi.org/10.1007/s11069-022-05223-z lizenzpflichtig Volltext GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT AR 112 2022 2 06 02 1191-1221 |
| language |
English |
| source |
Enthalten in Natural hazards 112(2022), 2 vom: 06. Feb., Seite 1191-1221 volume:112 year:2022 number:2 day:06 month:02 pages:1191-1221 |
| sourceStr |
Enthalten in Natural hazards 112(2022), 2 vom: 06. Feb., Seite 1191-1221 volume:112 year:2022 number:2 day:06 month:02 pages:1191-1221 |
| format_phy_str_mv |
Article |
| institution |
findex.gbv.de |
| topic_facet |
Landslide dam Ancient dammed lake Landslide-dammed lake outburst floods (LLOFs) Peak discharge Uncertainty assessment |
| dewey-raw |
550 |
| isfreeaccess_bool |
false |
| container_title |
Natural hazards |
| authorswithroles_txt_mv |
Ma, Junxue @@aut@@ Chen, Jian @@aut@@ Cui, Zhijiu @@aut@@ Zhou, Wendy @@aut@@ Chen, Ruichen @@aut@@ Wang, Chengbiao @@aut@@ |
| publishDateDaySort_date |
2022-02-06T00:00:00Z |
| hierarchy_top_id |
131010271 |
| dewey-sort |
3550 |
| id |
OLC2078737674 |
| language_de |
englisch |
| fullrecord |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2078737674</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230506024149.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">221220s2022 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11069-022-05223-z</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2078737674</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11069-022-05223-z-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Ma, Junxue</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-1922-2880</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s), under exclusive licence to Springer Nature B.V. 2022</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Landslide dam</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ancient dammed lake</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Landslide-dammed lake outburst floods (LLOFs)</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Peak discharge</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Uncertainty assessment</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Jian</subfield><subfield code="0">(orcid)0000-0002-3323-7560</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cui, Zhijiu</subfield><subfield code="0">(orcid)0000-0003-0306-0909</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhou, Wendy</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Ruichen</subfield><subfield code="0">(orcid)0000-0001-7988-8900</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Chengbiao</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Natural hazards</subfield><subfield code="d">Springer Netherlands, 1988</subfield><subfield code="g">112(2022), 2 vom: 06. Feb., Seite 1191-1221</subfield><subfield code="w">(DE-627)131010271</subfield><subfield code="w">(DE-600)1088547-X</subfield><subfield code="w">(DE-576)03285272X</subfield><subfield code="x">0921-030X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:112</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:2</subfield><subfield code="g">day:06</subfield><subfield code="g">month:02</subfield><subfield code="g">pages:1191-1221</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11069-022-05223-z</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</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_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">112</subfield><subfield code="j">2022</subfield><subfield code="e">2</subfield><subfield code="b">06</subfield><subfield code="c">02</subfield><subfield code="h">1191-1221</subfield></datafield></record></collection>
|
| author |
Ma, Junxue |
| spellingShingle |
Ma, Junxue ddc 550 ssgn 14 misc Landslide dam misc Ancient dammed lake misc Landslide-dammed lake outburst floods (LLOFs) misc Peak discharge misc Uncertainty assessment Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau |
| authorStr |
Ma, Junxue |
| ppnlink_with_tag_str_mv |
@@773@@(DE-627)131010271 |
| format |
Article |
| dewey-ones |
550 - Earth sciences |
| delete_txt_mv |
keep |
| author_role |
aut aut aut aut aut aut |
| collection |
OLC |
| remote_str |
false |
| illustrated |
Not Illustrated |
| issn |
0921-030X |
| topic_title |
550 VZ 14 ssgn Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau Landslide dam Ancient dammed lake Landslide-dammed lake outburst floods (LLOFs) Peak discharge Uncertainty assessment |
| topic |
ddc 550 ssgn 14 misc Landslide dam misc Ancient dammed lake misc Landslide-dammed lake outburst floods (LLOFs) misc Peak discharge misc Uncertainty assessment |
| topic_unstemmed |
ddc 550 ssgn 14 misc Landslide dam misc Ancient dammed lake misc Landslide-dammed lake outburst floods (LLOFs) misc Peak discharge misc Uncertainty assessment |
| topic_browse |
ddc 550 ssgn 14 misc Landslide dam misc Ancient dammed lake misc Landslide-dammed lake outburst floods (LLOFs) misc Peak discharge misc Uncertainty assessment |
| format_facet |
Aufsätze Gedruckte Aufsätze |
| format_main_str_mv |
Text Zeitschrift/Artikel |
| carriertype_str_mv |
nc |
| hierarchy_parent_title |
Natural hazards |
| hierarchy_parent_id |
131010271 |
| dewey-tens |
550 - Earth sciences & geology |
| hierarchy_top_title |
Natural hazards |
| isfreeaccess_txt |
false |
| familylinks_str_mv |
(DE-627)131010271 (DE-600)1088547-X (DE-576)03285272X |
| title |
Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau |
| ctrlnum |
(DE-627)OLC2078737674 (DE-He213)s11069-022-05223-z-p |
| title_full |
Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau |
| author_sort |
Ma, Junxue |
| journal |
Natural hazards |
| journalStr |
Natural hazards |
| lang_code |
eng |
| isOA_bool |
false |
| dewey-hundreds |
500 - Science |
| recordtype |
marc |
| publishDateSort |
2022 |
| contenttype_str_mv |
txt |
| container_start_page |
1191 |
| author_browse |
Ma, Junxue Chen, Jian Cui, Zhijiu Zhou, Wendy Chen, Ruichen Wang, Chengbiao |
| container_volume |
112 |
| class |
550 VZ 14 ssgn |
| format_se |
Aufsätze |
| author-letter |
Ma, Junxue |
| doi_str_mv |
10.1007/s11069-022-05223-z |
| normlink |
(ORCID)0000-0002-1922-2880 (ORCID)0000-0002-3323-7560 (ORCID)0000-0003-0306-0909 (ORCID)0000-0001-7988-8900 |
| normlink_prefix_str_mv |
(orcid)0000-0002-1922-2880 (orcid)0000-0002-3323-7560 (orcid)0000-0003-0306-0909 (orcid)0000-0001-7988-8900 |
| dewey-full |
550 |
| title_sort |
reconstruction of catastrophic outburst floods of the diexi ancient landslide-dammed lake in the upper minjiang river, eastern tibetan plateau |
| title_auth |
Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau |
| abstract |
Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years. © The Author(s), under exclusive licence to Springer Nature B.V. 2022 |
| abstractGer |
Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years. © The Author(s), under exclusive licence to Springer Nature B.V. 2022 |
| abstract_unstemmed |
Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years. © The Author(s), under exclusive licence to Springer Nature B.V. 2022 |
| collection_details |
GBV_USEFLAG_A SYSFLAG_A GBV_OLC SSG-OLC-PHY SSG-OLC-MAT SSG-OPC-GGO SSG-OPC-MAT |
| container_issue |
2 |
| title_short |
Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau |
| url |
https://doi.org/10.1007/s11069-022-05223-z |
| remote_bool |
false |
| author2 |
Chen, Jian Cui, Zhijiu Zhou, Wendy Chen, Ruichen Wang, Chengbiao |
| author2Str |
Chen, Jian Cui, Zhijiu Zhou, Wendy Chen, Ruichen Wang, Chengbiao |
| ppnlink |
131010271 |
| mediatype_str_mv |
n |
| isOA_txt |
false |
| hochschulschrift_bool |
false |
| doi_str |
10.1007/s11069-022-05223-z |
| up_date |
2024-07-03T21:53:12.644Z |
| _version_ |
1803596430201323521 |
| fullrecord_marcxml |
<?xml version="1.0" encoding="UTF-8"?><collection xmlns="http://www.loc.gov/MARC21/slim"><record><leader>01000caa a22002652 4500</leader><controlfield tag="001">OLC2078737674</controlfield><controlfield tag="003">DE-627</controlfield><controlfield tag="005">20230506024149.0</controlfield><controlfield tag="007">tu</controlfield><controlfield tag="008">221220s2022 xx ||||| 00| ||eng c</controlfield><datafield tag="024" ind1="7" ind2=" "><subfield code="a">10.1007/s11069-022-05223-z</subfield><subfield code="2">doi</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-627)OLC2078737674</subfield></datafield><datafield tag="035" ind1=" " ind2=" "><subfield code="a">(DE-He213)s11069-022-05223-z-p</subfield></datafield><datafield tag="040" ind1=" " ind2=" "><subfield code="a">DE-627</subfield><subfield code="b">ger</subfield><subfield code="c">DE-627</subfield><subfield code="e">rakwb</subfield></datafield><datafield tag="041" ind1=" " ind2=" "><subfield code="a">eng</subfield></datafield><datafield tag="082" ind1="0" ind2="4"><subfield code="a">550</subfield><subfield code="q">VZ</subfield></datafield><datafield tag="084" ind1=" " ind2=" "><subfield code="a">14</subfield><subfield code="2">ssgn</subfield></datafield><datafield tag="100" ind1="1" ind2=" "><subfield code="a">Ma, Junxue</subfield><subfield code="e">verfasserin</subfield><subfield code="0">(orcid)0000-0002-1922-2880</subfield><subfield code="4">aut</subfield></datafield><datafield tag="245" ind1="1" ind2="0"><subfield code="a">Reconstruction of catastrophic outburst floods of the Diexi ancient landslide-dammed lake in the Upper Minjiang River, Eastern Tibetan Plateau</subfield></datafield><datafield tag="264" ind1=" " ind2="1"><subfield code="c">2022</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">ohne Hilfsmittel zu benutzen</subfield><subfield code="b">n</subfield><subfield code="2">rdamedia</subfield></datafield><datafield tag="338" ind1=" " ind2=" "><subfield code="a">Band</subfield><subfield code="b">nc</subfield><subfield code="2">rdacarrier</subfield></datafield><datafield tag="500" ind1=" " ind2=" "><subfield code="a">© The Author(s), under exclusive licence to Springer Nature B.V. 2022</subfield></datafield><datafield tag="520" ind1=" " ind2=" "><subfield code="a">Abstract Landslide-dammed lake outburst floods (LLOFs) may pose serious safety threats to nearby residents and their livelihoods, as well as cause major damages to the downstream areas in mountainous regions. This study presents the Diexi ancient landslide-dammed lake (DALL), located along the Upper Minjiang River, in the eastern margins of the Tibetan Plateau. The DALL is known to have an estimated previous maximal lake area of 1.1 × $ 10^{7} $ $ m^{2} $ and an impounded volume of 2.9 × $ 10^{9} $ $ m^{3} $. At approximately 27 ka BP, the ancient landslide dam failed, and catastrophic LLOFs occurred. It was determined that the peak discharge of the Diexi ancient LLOFs could be reconstructed using regression, parametric, and boulder competence approaches. The reconstructed average maximum peak discharge was approximately 79,500 $ m^{3} $/s, with an estimated uncertainty bound of 70,000 to 90,000 $ m^{3} $/s. This indicated that the Diexi ancient LLOFs were the largest outburst floods to have occurred in the Upper Minjiang River Valley since the Late Pleistocene Period. The differences in the widths and slopes within the former and latter reaches of the dam indicated that the geomorphic influences on the river channel resulting from the DALL and its LLOFs have been present for tens of thousands of years. These findings were of major significance in deepening the understanding of the existence and disappearances of important river knickpoints on a time scale of tens of thousands of years.</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Landslide dam</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Ancient dammed lake</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Landslide-dammed lake outburst floods (LLOFs)</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Peak discharge</subfield></datafield><datafield tag="650" ind1=" " ind2="4"><subfield code="a">Uncertainty assessment</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Jian</subfield><subfield code="0">(orcid)0000-0002-3323-7560</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Cui, Zhijiu</subfield><subfield code="0">(orcid)0000-0003-0306-0909</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Zhou, Wendy</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Chen, Ruichen</subfield><subfield code="0">(orcid)0000-0001-7988-8900</subfield><subfield code="4">aut</subfield></datafield><datafield tag="700" ind1="1" ind2=" "><subfield code="a">Wang, Chengbiao</subfield><subfield code="4">aut</subfield></datafield><datafield tag="773" ind1="0" ind2="8"><subfield code="i">Enthalten in</subfield><subfield code="t">Natural hazards</subfield><subfield code="d">Springer Netherlands, 1988</subfield><subfield code="g">112(2022), 2 vom: 06. Feb., Seite 1191-1221</subfield><subfield code="w">(DE-627)131010271</subfield><subfield code="w">(DE-600)1088547-X</subfield><subfield code="w">(DE-576)03285272X</subfield><subfield code="x">0921-030X</subfield><subfield code="7">nnns</subfield></datafield><datafield tag="773" ind1="1" ind2="8"><subfield code="g">volume:112</subfield><subfield code="g">year:2022</subfield><subfield code="g">number:2</subfield><subfield code="g">day:06</subfield><subfield code="g">month:02</subfield><subfield code="g">pages:1191-1221</subfield></datafield><datafield tag="856" ind1="4" ind2="1"><subfield code="u">https://doi.org/10.1007/s11069-022-05223-z</subfield><subfield code="z">lizenzpflichtig</subfield><subfield code="3">Volltext</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_OLC</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-PHY</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OLC-MAT</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-GGO</subfield></datafield><datafield tag="912" ind1=" " ind2=" "><subfield code="a">SSG-OPC-MAT</subfield></datafield><datafield tag="951" ind1=" " ind2=" "><subfield code="a">AR</subfield></datafield><datafield tag="952" ind1=" " ind2=" "><subfield code="d">112</subfield><subfield code="j">2022</subfield><subfield code="e">2</subfield><subfield code="b">06</subfield><subfield code="c">02</subfield><subfield code="h">1191-1221</subfield></datafield></record></collection>
|
| score |
7.399935 |