000034602 001__ 34602
000034602 041__ $$aEnglish
000034602 100__ $$aWestoby, M. J.
000034602 245__ $$aReconstructing Historic Glacial Lakeoutburst Floods through Numerical Modelling and Geomorphological Assessment: Extreme Events in the Himalaya
000034602 260__ $$c2014
000034602 300__ $$a1675-1692
000034602 507__ $$akdrglof
000034602 520__ $$aRecession of high-mountain glaciers in response to climatic change frequently results in the development of morainedammed glacial lakes. Moraine dam failure is often accompanied by the release of large volumes of water and sediment, termed a Glacial Lake Outburst Flood (GLOF). Chukhung Glacier is a small (~3km2) receding valley glacier in Mt. Everest (Sagarmatha) National Park, Nepal. Unlike many Himalayan glaciers, which possess a thick mantle of supraglacial debris, its surface is relatively clean. The glacier terminus has receded 1.3 km from its maximum Holocene position, and in doing so provided the space for an icecontact moraine-dammed lake to develop. The lake had a maximum volume of 5.5 × 105m3 and drained as a result of breaching of the terminal moraine. An estimated 1.3 × 105m3 of material was removed from the terminal moraine during breach development. Numerical dam-breach modelling, implemented within a Generalised Likelihood Uncertainty Estimation (GLUE) framework, was used to investigate a range of moraine-dam failure scenarios. Reconstructed outflow peak discharges, including failure via overtopping and piping mechanisms, are in the range 146-2200m3 s-1. Results from two-dimensional hydrodynamic GLOF modelling indicate that maximum local flow depths may have exceeded 9m, with maximum flow velocities exceeding 20ms-1 within 700m of the breach. The floodwaters mobilised a significant amount of material, sourced mostly from the expanding breach, forming a 300m long and 100m wide debris fan originating at the breach exit. moraine-dam. These results also suggest that inundation of the entire floodplain may have been achieved within ten minutes of initial breach development, suggesting that debris fan development was rapid. We discuss the key glaciological and geomorphological factors that have determined the evolution of a hazardous moraine-dammed lake complex and the subsequent generation of a GLOF and its geomorphological impact.
000034602 700__ $$aGlasser, N. F.
000034602 700__ $$aHambrey, M. J.
000034602 700__ $$aBrasington, J.
000034602 700__ $$aReynolds, J. M.
000034602 700__ $$aHassan, M. a. a. M.
000034602 773__ $$pEarth Surface Processes and Landforms
000034602 773__ $$v39 (12)
000034602 773__ $$a10.1002/esp.3617
000034602 8564_ $$uhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-84916940061&doi=10.1002%2Fesp.3617&partnerID=40&md5=b73bd7f029f091e2a833d0ea1cbea58e$$yExternal link
000034602 980__ $$aARTICLE