Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Daniel E. J. Hobley"'
Autor:
Sai S. Nudurupati, Erkan Istanbulluoglu, Gregory E. Tucker, Nicole M. Gasparini, Daniel E. J. Hobley, Eric W. H. Hutton, Katherine R. Barnhart, Jordan M. Adams
Publikováno v:
Water Resources Research. 59
Publikováno v:
Earth Surface Processes and Landforms. 47:1599-1614
Mass movement deposit grain-size distributions (GSDs) record initiation, transport and deposition mechanisms, and contribute to the rate at which sediment is exported from hillslopes to channels. Defining the GSD of a mass movement deposit is a signi
Autor:
Richard G. Taylor, Japhet J. Kashaigili, Mark O. Cuthbert, Alan MacDonald, R. Swift, Daniel E. J. Hobley, E. Zarate, Jonathan Chambers, Edmund Mutayoba
Publikováno v:
Journal of Hydrology: Regional Studies, Vol 36, Iss, Pp 100833-(2021)
Study region\ud Little Kinyasungwe River Catchment, central semi-arid Tanzania.\ud \ud Study focus\ud The structure and hydraulic properties of superficial geology can play a crucial role in controlling groundwater recharge in drylands. However, the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8dd772e3bd80abaa1ff194be16664e48
https://orca.cardiff.ac.uk/id/eprint/141548/2/1-s2.0-S2214581821000628-main.pdf
https://orca.cardiff.ac.uk/id/eprint/141548/2/1-s2.0-S2214581821000628-main.pdf
Publikováno v:
Nature Geoscience. 11:901-904
On Earth, the sublimation of massive ice deposits at equatorial latitudes under cold and dry conditions in the absence of any liquid melt leads to the formation of spiked and bladed textures eroded into the surface of the ice. These sublimation-sculp
Autor:
Tristram Hales, Runqiu Huang, Erin Harvey, Xuanmei Fan, Qiang Xu, Jie Liu, Daniel E. J. Hobley
Large, catchment transitioning debris flows are an important mechanism for transporting sediment from hillslopes into higher order channels. Extremely large flows can exceed volumes of 109 m3, however even flows with volumes of ~103 m3 can lead to fa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8df65991a1f026c38c6b3f4c5ecad96d
https://doi.org/10.5194/egusphere-egu21-7389
https://doi.org/10.5194/egusphere-egu21-7389
Autor:
Tristram Hales, Daniel E. J. Hobley, Qiang Xu, Xuanmei Fan, Erin Harvey, Jie Liu, Runqiu Huang
Publikováno v:
Geological Society of America Abstracts with Programs.
Autor:
Tristram Hales, Daniel E. J. Hobley, Runqiu Huang, Jie Liu, Erin Harvey, Xuanmei Fan, Qiang Xu
Co-seismic landslides can mobilise up to 3 km3 of loose sediment within minutes. However, the export rate of this sediment is largely unconstrained. For example, it is estimated that a decade after the 2008 Wenchuan earthquake at least 90% of the co-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ffac69b9e55fb4e3dede92b3d1728c02
https://doi.org/10.5194/egusphere-egu2020-19439
https://doi.org/10.5194/egusphere-egu2020-19439
In tectonically active landscapes, fault movement drives both the creation of accommodation space (i.e., basins), and the production of topography on which geomorphic processes act (i.e., mountains). The action of fluvial processes on those mountains
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f6e571d384499d5518de6a61554de2f2
https://doi.org/10.5194/egusphere-egu2020-10229
https://doi.org/10.5194/egusphere-egu2020-10229