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pro vyhledávání: '"Mikael Attal"'
Any tectonic forcing acting on a mountain range consists of vertical uplift motion and horizontal advection motion. In landscapes with a high advective component, such as those affected by low angle normal faults, advection can form a substantial por
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c0666887e865624322846e83200e1fb6
https://doi.org/10.5194/egusphere-egu23-7602
https://doi.org/10.5194/egusphere-egu23-7602
Pebbles become rounded during fluvial transport. Roundness, along with other shape factors, size and lithology, are commonly used in sedimentology to link the fluvial transport distance and consequent abrasion prior to deposition. Although roundness
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe4426ac00cc1e9b958ac218f25c802e
https://doi.org/10.5194/egusphere-egu23-14016
https://doi.org/10.5194/egusphere-egu23-14016
Due to the limited resolution of freely available digital elevation models (DEM), DEM-derived river products cannot provide accurate flow lines in inland and lowland areas. Stream burning is used to improve the accuracy of extracted flowlines in addi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::376be640c1e0200db21fd2456159a8bb
https://doi.org/10.5194/egusphere-egu23-7453
https://doi.org/10.5194/egusphere-egu23-7453
Inferring erosion rates from 10Be or 26Al concentrations in stream sediments has become standard practice in geomorphology. In formerly glaciated landscapes, however, this technique is problematic because repeated phases of shielding and exposure dur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d55187aa64380aec1fd0098eca1604e
https://doi.org/10.5194/egusphere-egu23-6922
https://doi.org/10.5194/egusphere-egu23-6922
Publikováno v:
Journal of Geophysical Research: Earth Surface 127 (2022) 4
East, A E, Attal, M, Hoitink, A J F & Sergienko, O V 2022, ' Strategic Plan for the Journal of Geophysical Research—Earth Surface ', Journal of Geophysical Research: Earth Surface, vol. 127, no. 4, e2022JF006692 . https://doi.org/10.1029/2022JF006692
Journal of Geophysical Research: Earth Surface, 127(4)
East, A E, Attal, M, Hoitink, A J F & Sergienko, O V 2022, ' Strategic Plan for the Journal of Geophysical Research—Earth Surface ', Journal of Geophysical Research: Earth Surface, vol. 127, no. 4, e2022JF006692 . https://doi.org/10.1029/2022JF006692
Journal of Geophysical Research: Earth Surface, 127(4)
The Editors of the Journal of Geophysical Research—Earth Surface present a new strategic plan for the journal. The journal will contribute to the objectives of AGU to embrace advancing Earth and space science for the benefit of human societies and
Autor:
Hugh Sinclair, Noel Gourmelen, Maggie Creed, Alistair G.L. Borthwick, Dilip Gautam, Mikael Attal, Elizabeth Dingle
Publikováno v:
Dingle, E H, Creed, M J, Sinclair, H D, Gautam, D, Gourmelen, N, Borthwick, A G L & Attal, M 2020, ' Dynamic flood topographies in the Terai region of Nepal ', Earth Surface Processes and Landforms, vol. 45, no. 13, pp. 3092-3102 . https://doi.org/10.1002/esp.4953
Flood hazard maps used to inform and build resilience in remote communities in the Terai region of southern Nepal are based on outdated and static digital elevation models (DEMs), which do not reflect dynamic river configuration or hydrology. Episodi
Publikováno v:
Fieman, D M, Attal, M & Addy, S 2020, ' Geomorphic response of a mountain gravel-bed river to an extreme flood in Aberdeenshire, Scotland ', Scottish Journal of Geology, pp. sjg2019-005 . https://doi.org/10.1144/sjg2019-005
This study uses the 2015 ‘Storm Frank’ flood on the River Dee, Aberdeenshire, to assess the impact of extreme events on river dynamics. The Storm Frank flood (>200 year recurrence interval) caused significant local morphological change that was c
Autor:
Saraswati Thapa, Hugh D. Sinclair, Maggie Creed, Simon M. Mudd, Mikael Attal, Manoranjan Muthusamy, Bholanath Sharma
Climate change and land-use change impact the sediment flux and grainsize delivered to rivers which influences channel morphologies and hence modifies flood risk; this is particularly the case where channels are fed by high mountain catchments. Here,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f7256202521b090043139593de04742e
https://doi.org/10.5194/egusphere-egu22-6865
https://doi.org/10.5194/egusphere-egu22-6865
Large earthquakes can contribute to mountain growth by building topography, but also contribute to mass removal from mountain ranges through widespread mass wasting. On a shorter timescale, large earthquakes also have the potential to significantly a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f1b28a821ced5809ca356a93bc5be77
https://doi.org/10.5194/egusphere-egu22-8709
https://doi.org/10.5194/egusphere-egu22-8709
The gravel-sand transition is a distinct morphological boundary in continental foreland basins characterised by an abrupt downstream reduction in grainsize and lowering of channel gradients. Tectonic convergence between foreland basins and mountain f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::df12c87af816a6bf5fe6f02b08b31ff2
https://doi.org/10.5194/egusphere-egu22-11457
https://doi.org/10.5194/egusphere-egu22-11457