Zobrazeno 1 - 10
of 106
pro vyhledávání: '"Onno Bokhove"'
Publikováno v:
Cambridge Prisms: Water, Vol 2 (2024)
Strategies are proposed to cope with uncertainties in a way that all possible kinds of uncertainty are named, recognized, statistically quantified as far as possible and utilized in efficient decision-making in flood risk management (FRM). We elabora
Externí odkaz:
https://doaj.org/article/aa590efd35dd4eaca220ff486c36e5cd
Publikováno v:
International Marine Energy Journal, Vol 3, Iss 1 (2020)
A novel wave-energy device is presented. Both a preliminary proof-of-principle of a working, scaled laboratory version of the energy device is shown as well as the derivation and analysis of a comprehensive mathematical and numerical model of the new
Externí odkaz:
https://doaj.org/article/4233befb2d0949d592303478620df2cb
Publikováno v:
Water, Vol 12, Iss 3, p 652 (2020)
Inspired by the Boxing Day 2015 flood of the River Aire in Leeds, UK, and subsequent attempts to mitigate adverse consequences of flooding, the goals considered are: (i) to revisit the concept of flood-excess volume (FEV) as a complementary diagnosti
Externí odkaz:
https://doaj.org/article/4d3d78f3bad745198b73d850ae11b6f7
Publikováno v:
Tellus: Series A, Dynamic Meteorology and Oceanography, Vol 69, Iss 1 (2017)
An idealized fluid model of convective-scale numerical weather prediction, intended for use in inexpensive data assimilation experiments, is described here and its distinctive dynamics are investigated. The model modifies the rotating shallow water e
Externí odkaz:
https://doaj.org/article/6b12b0e4352b484c8ff2c9cccae10c7d
Publikováno v:
Journal of the Atmospheric Sciences. 79:859-873
An isentropic 1½-layer model based on modified shallow-water equations is presented, including terms mimicking convection and precipitation. This model is an updated version of the isopycnal single-layer modified rotating shallow water (modRSW) mode
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f4b8f7d0c297f949f47ae7ed9ecc1c33
https://doi.org/10.1175/jas-d-21-0022.1
https://doi.org/10.1175/jas-d-21-0022.1
Publikováno v:
Journal of the Atmospheric Sciences. 79:875-886
In this Part II paper we present a fully consistent analytical derivation of the “dry” isentropic 1½-layer shallow-water model described and used in Part I of this study, with no convection and precipitation. The mathematical derivation presente
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9f9b728a6aaf0cae70db0b61e23ca12e
https://doi.org/10.1175/jas-d-21-0023.1
https://doi.org/10.1175/jas-d-21-0023.1
Following the development of the modified rotating shallow water model (modRSW), which includes simplified dynamics of convection and precipitation, we present the results of a series of idealised forecast-assimilation experiments to demonstrate its
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::86e0dfee0acde450e8ef2679f5e178ed
https://gmd.copernicus.org/preprints/gmd-2022-269/
https://gmd.copernicus.org/preprints/gmd-2022-269/
A new, cost-effective and widely applicable tool is developed for simulating three-dimensional (3D) water-wave motion in the context of the maritime-engineering sector, with specific focus on the formation and analysis of extreme waves generated with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36596ada865aaff4ee10e29ff762f10a
https://doi.org/10.31223/x5ws8f
https://doi.org/10.31223/x5ws8f
Extreme waves can randomly arise in crossing seas with waves coming from two or more main directions. Linear superposition with weak nonlinearity has been proposed to explain "every-day'' extreme waves, i.e. waves with an amplitude of at least twice
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01e4c0bf4d0fb2a4b3af68a9ceb8bb59
https://doi.org/10.5194/egusphere-egu22-4143
https://doi.org/10.5194/egusphere-egu22-4143
Approximately 70% of the global dissipation of the barotropic tide occurs in the waters of the continental margins, due to bottom friction on the shelves and internal tide generation at the continental slopes. Here we are interested in the latter pro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15211a2a03eae48f5d70e0e79f663163
https://doi.org/10.5194/egusphere-egu22-1644
https://doi.org/10.5194/egusphere-egu22-1644