Outburst floods from moraine-dammed lakes in the Himalayas : detection, frequency, and hazard

The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent dec...
Ausführliche Beschreibung

Gespeichert in:

Autor*in:	Veh, Georg [verfasserIn] Walz, Ariane [akademischer betreuerIn] Korup, Oliver [akademischer betreuerIn] Haeberli, Wilfried - 1947- [akademischer betreuerIn]
Körperschaften:	Universität Potsdam [Grad-verleihende Institution]
Hochschulschrift:	Dissertation ; Universität Potsdam ; 2019

Format:	E-Book
Sprache:	Englisch

Erschienen:	Potsdam: 2019

Schlagwörter:	Himalaja / Gletschersee / Eis / Dammbruch / Paläohydrologie / Fluviale Sedimentation Himalaja / Gletschersee / Hochwasser / Fernerkundung / Satellitenbildauswertung / Naturgefahr Himalaja / Überschwemmungsgefahr
Formangabe:	Hochschulschrift

Anmerkung:	Kumulative Dissertation Volltext: PDF
Umfang:	1 Online-Ressource (IX, 124 Seiten, 15028 KB) ; Illustrationen, Diagramme

Weitere Ausgabe:	Erscheint auch als Druck-Ausgabe Veh, Georg: Outburst floods from moraine-dammed lakes in the Himalayas - Potsdam, 2019

Links:	Link aufrufen Link aufrufen Link aufrufen Link aufrufen Link aufrufen Link aufrufen

DOI / URN:	urn:nbn:de:kobv:517-opus4-436071 10.25932/publishup-43607

Katalog-ID:	1683809327

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520			\|a The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. [...]
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building	20 21 22:u 23 30 40:s 60 63 65 70:d 105 110 132 151 161 285 293 370 2027:0 2403:0
topic_facet	Himalaja Gletschersee Eis Dammbruch Paläohydrologie Fluviale Sedimentation Hochwasser Fernerkundung Satellitenbildauswertung Naturgefahr Überschwemmungsgefahr
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language_de	englisch
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callnumber-first	D - World History
dewey-ones	551 - Geology, hydrology & meteorology 550 - Earth sciences
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illustrated	Not Illustrated
topic_title	551.489 DE-101 550 DE-101 38.49 bkl 43.48 bkl 2027 01 DE-105 00 s ebook Outburst floods from moraine-dammed lakes in the Himalayas detection, frequency, and hazard by Georg Veh g (DE-588)4024923-2 (DE-627)106295578 (DE-576)208958347 Himalaja gnd s (DE-588)4334136-6 (DE-627)148293980 (DE-576)211346373 Gletschersee gnd s (DE-588)4013994-3 (DE-627)106341448 (DE-576)208906185 Eis gnd s (DE-588)4333511-1 (DE-627)148059600 (DE-576)211340960 Dammbruch gnd s (DE-588)4173111-6 (DE-627)105382388 (DE-576)209947934 Paläohydrologie gnd s (DE-588)4113593-3 (DE-627)105828300 (DE-576)209477741 Fluviale Sedimentation gnd (DE-627) s (DE-588)4025289-9 (DE-627)104141689 (DE-576)208959963 Hochwasser gnd s (DE-588)4016796-3 (DE-627)104213418 (DE-576)208917411 Fernerkundung gnd s (DE-588)4116326-6 (DE-627)104458615 (DE-576)20950062X Satellitenbildauswertung gnd s (DE-588)4123823-0 (DE-627)105752304 (DE-576)209562978 Naturgefahr gnd s (DE-588)4453039-0 (DE-627)227482166 (DE-576)212592750 Überschwemmungsgefahr gnd
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title_full	Outburst floods from moraine-dammed lakes in the Himalayas detection, frequency, and hazard by Georg Veh
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title_sort	outburst floods from moraine-dammed lakes in the himalayasdetection, frequency, and hazard
title_auth	Outburst floods from moraine-dammed lakes in the Himalayas detection, frequency, and hazard
abstract	The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. [...] Kumulative Dissertation Volltext: PDF
abstractGer	The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. [...] Kumulative Dissertation Volltext: PDF
abstract_unstemmed	The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. [...] Kumulative Dissertation Volltext: PDF
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author2	Walz, Ariane Korup, Oliver Haeberli, Wilfried 1947- Universität Potsdam
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This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. 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spelling	121840518X DE-101 urn:nbn:de:kobv:517-opus4-436071 urn 10.25932/publishup-43607 doi (DE-627)1683809327 (DE-599)KXP1683809327 (OCoLC)1175587017 DE-627 ger DE-627 rda eng XA-DE-BB 551.489 DE-101 550 DE-101 38.49 bkl 43.48 bkl Veh, Georg verfasserin (DE-588)1200673247 (DE-627)1683831292 aut Outburst floods from moraine-dammed lakes in the Himalayas detection, frequency, and hazard by Georg Veh Übersetzung des Haupttitels Ausbruchsfluten von moränen-gestauten Seen im Himalaya Potsdam 2019 1 Online-Ressource (IX, 124 Seiten, 15028 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kumulative Dissertation Volltext: PDF Dissertation Universität Potsdam 2019 The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. 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allfields_unstemmed	121840518X DE-101 urn:nbn:de:kobv:517-opus4-436071 urn 10.25932/publishup-43607 doi (DE-627)1683809327 (DE-599)KXP1683809327 (OCoLC)1175587017 DE-627 ger DE-627 rda eng XA-DE-BB 551.489 DE-101 550 DE-101 38.49 bkl 43.48 bkl Veh, Georg verfasserin (DE-588)1200673247 (DE-627)1683831292 aut Outburst floods from moraine-dammed lakes in the Himalayas detection, frequency, and hazard by Georg Veh Übersetzung des Haupttitels Ausbruchsfluten von moränen-gestauten Seen im Himalaya Potsdam 2019 1 Online-Ressource (IX, 124 Seiten, 15028 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kumulative Dissertation Volltext: PDF Dissertation Universität Potsdam 2019 The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. [...] Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4024923-2 (DE-627)106295578 (DE-576)208958347 Himalaja gnd s (DE-588)4334136-6 (DE-627)148293980 (DE-576)211346373 Gletschersee gnd s (DE-588)4013994-3 (DE-627)106341448 (DE-576)208906185 Eis gnd s (DE-588)4333511-1 (DE-627)148059600 (DE-576)211340960 Dammbruch gnd s (DE-588)4173111-6 (DE-627)105382388 (DE-576)209947934 Paläohydrologie gnd s (DE-588)4113593-3 (DE-627)105828300 (DE-576)209477741 Fluviale Sedimentation gnd (DE-627) g (DE-588)4024923-2 (DE-627)106295578 (DE-576)208958347 Himalaja gnd s (DE-588)4334136-6 (DE-627)148293980 (DE-576)211346373 Gletschersee gnd s (DE-588)4025289-9 (DE-627)104141689 (DE-576)208959963 Hochwasser gnd s (DE-588)4016796-3 (DE-627)104213418 (DE-576)208917411 Fernerkundung gnd s (DE-588)4116326-6 (DE-627)104458615 (DE-576)20950062X Satellitenbildauswertung gnd s (DE-588)4123823-0 (DE-627)105752304 (DE-576)209562978 Naturgefahr gnd (DE-627) g (DE-588)4024923-2 (DE-627)106295578 (DE-576)208958347 Himalaja gnd s (DE-588)4453039-0 (DE-627)227482166 (DE-576)212592750 Überschwemmungsgefahr gnd (DE-627) Walz, Ariane akademischer betreuerin (DE-588)1067570802 (DE-627)818958308 (DE-576)426753275 dgs Korup, Oliver akademischer betreuerin (DE-588)1163322091 (DE-627)1027617646 (DE-576)507909135 dgs Haeberli, Wilfried 1947- akademischer betreuerin (DE-588)1070038822 (DE-627)823205509 (DE-576)429715129 dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Veh, Georg Outburst floods from moraine-dammed lakes in the Himalayas Potsdam, 2019 IX, 124 Seiten (DE-627)1683809904 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-436071 Resolving-System kostenfrei https://doi.org/10.25932/publishup-43607 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-436071 2020-10-07 Resolving-System https://d-nb.info/121840518X/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/43607 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER 38.49 Glazialmorphologie (DE-627)181571145 43.48 Regionale Umweltprobleme (DE-627)181569981 BO 045F 551.489 20 01 0084 3782409132 x 20-10-20 21 01 0046 3782448340 z 20-10-20 22 01 0018 3782487591 SUBolrd xu 20-10-20 23 01 0830 3782525655 olr-d x 20-10-20 30 01 0104 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allfieldsGer	121840518X DE-101 urn:nbn:de:kobv:517-opus4-436071 urn 10.25932/publishup-43607 doi (DE-627)1683809327 (DE-599)KXP1683809327 (OCoLC)1175587017 DE-627 ger DE-627 rda eng XA-DE-BB 551.489 DE-101 550 DE-101 38.49 bkl 43.48 bkl Veh, Georg verfasserin (DE-588)1200673247 (DE-627)1683831292 aut Outburst floods from moraine-dammed lakes in the Himalayas detection, frequency, and hazard by Georg Veh Übersetzung des Haupttitels Ausbruchsfluten von moränen-gestauten Seen im Himalaya Potsdam 2019 1 Online-Ressource (IX, 124 Seiten, 15028 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kumulative Dissertation Volltext: PDF Dissertation Universität Potsdam 2019 The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. 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2020-10-07 Resolving-System https://d-nb.info/121840518X/34 2020-10-07 Langzeitarchivierung Nationalbibliothek https://publishup.uni-potsdam.de/frontdoor/index/index/docId/43607 application/pdf 2020-10-07 Verlag kostenfrei GBV-ODiss GBV_ILN_20 ISIL_DE-84 SYSFLAG_1 GBV_KXP SSG-OPC-GGO GBV_ILN_21 ISIL_DE-46 GBV_ILN_22 ISIL_DE-18 GBV_ILN_23 ISIL_DE-830 GBV_ILN_30 ISIL_DE-104 GBV_ILN_40 ISIL_DE-7 GBV_ILN_60 ISIL_DE-705 GBV_ILN_63 ISIL_DE-Wim2 GBV_ILN_65 ISIL_DE-3 GBV_ILN_70 ISIL_DE-89 GBV_ILN_105 ISIL_DE-841 GBV_ILN_110 ISIL_DE-Luen4 GBV_ILN_132 ISIL_DE-959 GBV_ILN_151 ISIL_DE-546 GBV_ILN_161 ISIL_DE-960 GBV_ILN_285 ISIL_DE-517 GBV_ILN_293 ISIL_DE-960-3 GBV_ILN_370 ISIL_DE-1373 GBV_ILN_2027 ISIL_DE-105 GBV_ILN_2403 ISIL_DE-LFER 38.49 Glazialmorphologie (DE-627)181571145 43.48 Regionale Umweltprobleme (DE-627)181569981 BO 045F 551.489 20 01 0084 3782409132 x 20-10-20 21 01 0046 3782448340 z 20-10-20 22 01 0018 3782487591 SUBolrd xu 20-10-20 23 01 0830 3782525655 olr-d x 20-10-20 30 01 0104 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allfieldsSound	121840518X DE-101 urn:nbn:de:kobv:517-opus4-436071 urn 10.25932/publishup-43607 doi (DE-627)1683809327 (DE-599)KXP1683809327 (OCoLC)1175587017 DE-627 ger DE-627 rda eng XA-DE-BB 551.489 DE-101 550 DE-101 38.49 bkl 43.48 bkl Veh, Georg verfasserin (DE-588)1200673247 (DE-627)1683831292 aut Outburst floods from moraine-dammed lakes in the Himalayas detection, frequency, and hazard by Georg Veh Übersetzung des Haupttitels Ausbruchsfluten von moränen-gestauten Seen im Himalaya Potsdam 2019 1 Online-Ressource (IX, 124 Seiten, 15028 KB) Illustrationen, Diagramme Text txt rdacontent Computermedien c rdamedia Online-Ressource cr rdacarrier Kumulative Dissertation Volltext: PDF Dissertation Universität Potsdam 2019 The Himalayas are a region that is most dependent, but also frequently prone to hazards from changing meltwater resources. This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. [...] Hochschulschrift (DE-588)4113937-9 (DE-627)105825778 (DE-576)209480580 gnd-content g (DE-588)4024923-2 (DE-627)106295578 (DE-576)208958347 Himalaja gnd s (DE-588)4334136-6 (DE-627)148293980 (DE-576)211346373 Gletschersee gnd s (DE-588)4013994-3 (DE-627)106341448 (DE-576)208906185 Eis gnd s (DE-588)4333511-1 (DE-627)148059600 (DE-576)211340960 Dammbruch gnd s (DE-588)4173111-6 (DE-627)105382388 (DE-576)209947934 Paläohydrologie gnd s (DE-588)4113593-3 (DE-627)105828300 (DE-576)209477741 Fluviale Sedimentation gnd (DE-627) g (DE-588)4024923-2 (DE-627)106295578 (DE-576)208958347 Himalaja gnd s (DE-588)4334136-6 (DE-627)148293980 (DE-576)211346373 Gletschersee gnd s (DE-588)4025289-9 (DE-627)104141689 (DE-576)208959963 Hochwasser gnd s (DE-588)4016796-3 (DE-627)104213418 (DE-576)208917411 Fernerkundung gnd s (DE-588)4116326-6 (DE-627)104458615 (DE-576)20950062X Satellitenbildauswertung gnd s (DE-588)4123823-0 (DE-627)105752304 (DE-576)209562978 Naturgefahr gnd (DE-627) g (DE-588)4024923-2 (DE-627)106295578 (DE-576)208958347 Himalaja gnd s (DE-588)4453039-0 (DE-627)227482166 (DE-576)212592750 Überschwemmungsgefahr gnd (DE-627) Walz, Ariane akademischer betreuerin (DE-588)1067570802 (DE-627)818958308 (DE-576)426753275 dgs Korup, Oliver akademischer betreuerin (DE-588)1163322091 (DE-627)1027617646 (DE-576)507909135 dgs Haeberli, Wilfried 1947- akademischer betreuerin (DE-588)1070038822 (DE-627)823205509 (DE-576)429715129 dgs Universität Potsdam Grad-verleihende Institution (DE-588)2120681-8 (DE-627)101653735 (DE-576)193975041 dgg Potsdam (DE-588)4046948-7 (DE-627)106196332 (DE-576)209071575 uvp Erscheint auch als Druck-Ausgabe Veh, Georg Outburst floods from moraine-dammed lakes in the Himalayas Potsdam, 2019 IX, 124 Seiten (DE-627)1683809904 http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-436071 Resolving-System kostenfrei https://doi.org/10.25932/publishup-43607 Resolving-System kostenfrei https://nbn-resolving.org/urn:nbn:de:kobv:517-opus4-436071 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authorswithroles_txt_mv	Veh, Georg @@aut@@ Walz, Ariane @@dgs@@ Korup, Oliver @@dgs@@ Haeberli, Wilfried @@dgs@@
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This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. 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title	Outburst floods from moraine-dammed lakes in the Himalayas detection, frequency, and hazard
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title_alt	Ausbruchsfluten von moränen-gestauten Seen im Himalaya
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This mountain belt hosts the highest mountain peaks on earth, has the largest reserve of ice outside the polar regions, and is home to a rapidly growing population in recent decades. One source of hazard has attracted scientific research in particular in the past two decades: glacial lake outburst floods (GLOFs) occurred rarely, but mostly with fatal and catastrophic consequences for downstream communities and infrastructure. Such GLOFs can suddenly release several million cubic meters of water from naturally impounded meltwater lakes. Glacial lakes have grown in number and size by ongoing glacial mass losses in the Himalayas. Theory holds that enhanced meltwater production may increase GLOF frequency, but has never been tested so far. The key challenge to test this notion are the high altitudes of >4000 m, at which lakes occur, making field work impractical. Moreover, flood waves can attenuate rapidly in mountain channels downstream, so that many GLOFs have likely gone unnoticed in past decades. Our knowledge on GLOFs is hence likely biased towards larger, destructive cases, which challenges a detailed quantification of their frequency and their response to atmospheric warming. Robustly quantifying the magnitude and frequency of GLOFs is essential for risk assessment and management along mountain rivers, not least to implement their return periods in building design codes. 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Outburst floods from moraine-dammed lakes in the Himalayas : detection, frequency, and hazard

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