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Seasonal assessment of cross-shore morphodynamic behaviour of wave-dominated beaches using data-driven analysis
Four years of data-driven analyses—Empirical Orthogonal Function (EOF) analysis and Canonical Correlation Analysis (CCA), were performed for North...
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Frontogenesis and Frontolysis of a Cold Filament Driven by the Cross-Filament Wind and Wave Fields Simulated by a Large Eddy Simulation
The variations of the frontogenetic trend of a cold filament induced by the cross-filament wind and wave fields are studied by a non-hydrostatic...
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Shallow Water Flow
Shallow water flow (SWF) is a drilling disaster caused by overpressure driven upward flow of coarse sediments.
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Macropore Flow and Its Characteristics
Conventional theories of water flow in soil assume local equilibrium at the elementary volume scale. However, in recent years, this assumption has...
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Preliminary analysis of the mechanism in the July 16, 2022 Gaojiashan cascading hazard: a landslide-induced debris flow in Southwest China
Debris flows can be triggered by landslides and lake outbursts, constituting cascading hazards that pose threats to life and property. However,...
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Internal wave-driven mixing: governing processes and consequences for climate
Turbulent mixing from breaking oceanic internal waves drives a vertical transport of water, heat and other climatically important tracers in the...
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Simulating glacier lake outburst floods (GLOFs) with a two-phase/layer debris flow model considering fluid-solid flow transitions
Glacier lake outburst floods (GLOFs) initiate with the rapid outburst of a glacier lake, endangering downstream populations, land, and...
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Sverdrup Flow and Boundary Currents
In his original paper, Sverdrup obtained a steady-state solution to the depth-integrated fluid equations without momentum advection and mixing. That...
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A Tutorial Review, Simple Energy-Flow Calculations, and Basic Definitions
This gives a brief history of the tutorial of simple mechanical energy and its conservation along with the definitions of kinetic and potential...
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Regional Debris-Flow Hazard Assessments
Regional debris-flow hazard assessments provide consistent information on potential hazards over large areas, often with limited available data....
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Ultralow velocity zone and deep mantle flow beneath the Himalayas linked to subducted slab
The origins of ultralow velocity zones, small-scale structures with extremely low seismic velocities found near the core–mantle boundary, remain...
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Experimental and numerical investigation of shelf flow crossing over a strait
Motivated by the phenomenon of Scotian Shelf Crossover events, the problem of a shelf flow that is interrupted by a strait is considered. Laboratory...
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Hydrothermal flow and serpentinization in oceanic core complexes controlled by mafic intrusions
Deep-sea hydrothermal systems at slow/ultraslow-spreading mid-ocean ridges are often located within ultramafic rocks that are part of oceanic core...
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Energy Flow and Magma Generation
Energy in the Earth can rise from deeper levels in the mantle where either excess temperature or compositional variations cause ascent to the...
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Multiphase Flow Modelling Using Smoothed Particle Hydrodynamics: Considerations on Sediment Transport
Environmental applications of multiphase flows include sediment transport and phenomena involving air–water interfaces that are dealt with as either...
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Voellmy-type mixture rheologies for dilatant, two-layer debris flow models
We formulate and test different Voellmy-type mixture rheologies that can be introduced into two-layer debris flow models. The formulations are based...
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Meandering of instantaneous large-scale structures in open-channel flow over longitudinal ridges
The results of large-eddy simulations of open-channel flows over spanwise heterogeneous surface ridges at two representative spanwise spacings are...
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A progressive flow-routing model for rapid assessment of debris-flow inundation
Debris flows pose a significant hazard to communities in mountainous areas, and there is a continued need for methods to delineate hazard zones...
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Numerical Simulation of the Mass Movement Process of the 2018 Sedongpu Glacial Debris Flow by Using the Fluid-Solid Coupling Method
In the context of global warming and intensified human activities, glacier instability in plateau regions has increased, and glacier debris flows...
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Relative dispersion and relative diffusivities in an ocean-wave coupled model of the North Sea
The study analyzes the impact of various wave-induced processes on relative dispersion and diffusivities in the North Sea using OpenDrift, a...
