Zobrazeno 1 - 10
of 114
pro vyhledávání: '"Gareth Pender"'
Publikováno v:
Frontiers in Environmental Science, Vol 9 (2021)
Differential parametric values associated with bed load sediment transport, that result at the same discharge levels on the rising and falling limbs of a flood hydrograph, are usually defined as bed load hysteresis. This hysteresis in bed load sedime
Externí odkaz:
https://doaj.org/article/75a48efcd91c4313baa8aceb1236efe1
Publikováno v:
PLoS ONE, Vol 12, Iss 12, p e0188489 (2017)
Conflicts over water resources can be highly dynamic and complex due to the various factors which can affect such systems, including economic, engineering, social, hydrologic, environmental and even political, as well as the inherent uncertainty invo
Externí odkaz:
https://doaj.org/article/0e6f725349e046468701a5e9ff20be12
Publikováno v:
Proceedings of the Institution of Civil Engineers - Water Management. 174:27-41
This paper presents a new data-driven modelling framework for forecasting probabilistic flood inundation maps for real-time applications. The proposed end-to-end (rainfall–inundation) method combines a suite of machine learning (ML) algorithms to f
Publikováno v:
Proceedings of the Institution of Civil Engineers - Water Management. 173:69-86
This paper presents a systematic investigation into modelling capacities of three conventional data-driven modelling techniques, namely, wavelet-based artificial neural network (WANN), support vector regression (SVR) and deep belief network (DBN) for
Publikováno v:
Water Resources Research. 55:5431-5452
Publikováno v:
Advances in Water Resources. 129:338-353
Fluvial sediment-laden flow represents a class of fluid-solid two-phase flows, which typically involve multi grain sizes, interphase and particle-particle interactions, and mass exchange with the bed. However, existing depth-averaged models ignore on
Publikováno v:
Cao, Z, Li, J, Borthwick, A, Liu, Q & Pender, G 2020, ' Grain-energy release governs mobility of debris flow due to solid–liquid mass release ', Earth Surface Processes and Landforms . https://doi.org/10.1002/esp.4939
Debris flows often exhibit high mobility, leading to extensive hazards far from their sources. Although it is known that debris flow mobility increases with initial volume, the underlying mechanism remains uncertain. Here, we reconstruct the mobility
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b9c7a8bbc6cce84cf41cee62c06a2e73
https://www.pure.ed.ac.uk/ws/files/152967214/Borthwick_Accepted_Manuscript.pdf
https://www.pure.ed.ac.uk/ws/files/152967214/Borthwick_Accepted_Manuscript.pdf
Publikováno v:
International Journal of Sediment Research. 33:462-477
A depth-averaged two-phase model is proposed for debris flows over fixed beds, explicitly incorporating interphase and particle-particle interactions, fluid and solid fluctuations and multi grain sizes. A first-order model based on the kinetic theory
Publikováno v:
International Journal of Sediment Research. 33:327-339
Laboratory flume experiments were done to investigate bed load sediment transport by both steady and unsteady flows in a degrading channel. The bed, respectively composed of uniform sand, uniform gravel, or sand-gravel mixtures, always undergoes bulk
Publikováno v:
Borthwick, A, Xia, C, Cao, Z & Pender, G 2017, ' Numerical algorithms for solving shallow water hydro-sediment-morphodynamic equations ', Engineering Computations, vol. 34, no. 8, pp. 2836-2861 . https://doi.org/10.1108/EC-01-2016-0026
Purpose The purpose of this paper is to present a fully conservative numerical algorithm for solving the coupled shallow water hydro-sediment-morphodynamic equations governing fluvial processes, and also to clarify the performance of a conventional a