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[PDF] Top 20 Dynamics of laboratory models of the wind-driven ocean circulation

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Dynamics of laboratory models of the wind-driven ocean circulation

Dynamics of laboratory models of the wind-driven ocean circulation

... the laboratory sliced cylinder and sliced cone results of Griffiths (Griffiths & Kiss, 1999) and Griffiths & Veronis (1997), ...the dynamics responsible for the observed laboratory ...linear ... See full document

10

On wind-driven mid-latitude convection in ocean general circulation models

On wind-driven mid-latitude convection in ocean general circulation models

... state-of-the-art ocean general circulation model to identify the northward directed Ekman transport of Antarctic and Subantarctic origin surface water as a mechanism which forces mid-latitude ...the ... See full document

16

The Role of diapycnal mixing in coupled atmosphere ocean general circulation models

The Role of diapycnal mixing in coupled atmosphere ocean general circulation models

... The ocean circulation consists of two main motions, as described by Wunsch ...is driven by the wind in the upper ocean, which is also responsible for the surface ...the wind on ... See full document

153

Laboratory models of geophysical flows : lava domes on slopes and wind-driven convection at ocean fronts

Laboratory models of geophysical flows : lava domes on slopes and wind-driven convection at ocean fronts

... Laser induced fluorescence was used to measure the density field before and after the forcing event and empirical formulas are given for the increase in the mass and volume of mixed flui[r] ... See full document

134

On stochastic stability of regional ocean models with uncertainty in wind forcing

On stochastic stability of regional ocean models with uncertainty in wind forcing

... that wind is one of the main energy sources of ocean currents and that, naturally, prediction errors associated with wind forcing un- certainty may grow quickly in numerical models (Robinson ... See full document

16

Ocean circulation drifts in multi-millennial climate simulations: the role of salinity corrections and climate feedbacks

Ocean circulation drifts in multi-millennial climate simulations: the role of salinity corrections and climate feedbacks

... et al. 2011). FAMOUS has previously been tuned both systematically (Jones et al. 2005; Gregoire et al. 2011; Williams et al. 2013) and manually (Smith et al. 2008), with the focus being on the tuneable parameters that ... See full document

21

Computational models for the dynamics of early mouse embryogenesis

Computational models for the dynamics of early mouse embryogenesis

... The question of how cells are directed to the appropriate fate was later addressed by Holmes et al., (2017) who considered the same ODE description of the core GRN for TE/ICM specification. However, instead of ... See full document

13

Large eddy simulation model for wind-driven sea circulation in coastal areas

Large eddy simulation model for wind-driven sea circulation in coastal areas

... of wind-driven circulation, water renewal and vertical mixing in the Muggia bay, the industrial harbor of the city of Trieste (Italy), for three typical wind ...the wind velocity used ... See full document

18

The impact of different glacial boundary conditions on atmospheric dynamics and precipitation in the North Atlantic region

The impact of different glacial boundary conditions on atmospheric dynamics and precipitation in the North Atlantic region

... This study contributes to the long history of scientific lit- erature that investigates the impact of glacial topographic changes on the atmosphere (e.g. Manabe and Broccoli, 1985; Kutzbach and Guetter, 1986; Felzer et ... See full document

15

Southern ocean circulation

Southern ocean circulation

... Southern Ocean south of 50° S into the mixed layer, where ocean-atmosphere-ice interactions can change the density of the water, completing the Deacon and deep overturning meridional ...available ... See full document

18

An Adaptive Multi-Analysis Technique and Software Architecture for Ocean Circulation Models.

An Adaptive Multi-Analysis Technique and Software Architecture for Ocean Circulation Models.

... accommodate ocean models with different numerical methods and formula- tions, and the second level is implementation-specific source code that is specialized for the details of the model to be ... See full document

160

Freshening of the Labrador Sea as a trigger for Little Ice Age development

Freshening of the Labrador Sea as a trigger for Little Ice Age development

... SPG circulation was in the strong mode during that time interval ...SPG circulation en- hances the supply of warm Atlantic Intermediate water to the East Greenland coast, which promotes calving and, subse- ... See full document

15

Sequential assimilation of multi-mission dynamical topography into a global finite-element ocean model

Sequential assimilation of multi-mission dynamical topography into a global finite-element ocean model

... Further, an open problem is how to project the assimilation update derived from the altimetry data into the interior of the ocean. In order to resolve this problem De Mey and Robin- son (1987); Dombrowsky and De ... See full document

12

Interannual evolution of (sub)mesoscale dynamics in the Bay of Biscay

Interannual evolution of (sub)mesoscale dynamics in the Bay of Biscay

... In Fig. 9, the surface relative vorticity from analysed simu- lations at different contrasted time steps is represented. From these maps, different patterns can be noticed. First, the con- trast between the deep open ... See full document

21

Numerical Simulation of Currents and Volume Transport in the Malacca Strait and Part of South China Sea

Numerical Simulation of Currents and Volume Transport in the Malacca Strait and Part of South China Sea

... Abstract. This work aimed to determine the hydrodynamics of the Malacca Strait (MS) and the part of the South China Sea (SCS). The study uses the two-dimensional numerical model with a finite-difference method. The ... See full document

15

Wind Driven Dynamics of Beach Cast Wrack in a Tide Free System

Wind Driven Dynamics of Beach Cast Wrack in a Tide Free System

... To further understand the dependence of wrack decomposition, significantly contributing to spatio-temporal dynamics of wrack (c.f. [5]), on wrack fragment size and its position on the beach, mass of the most ... See full document

12

Antarctic intermediate water mass formation in ocean general circulation models

Antarctic intermediate water mass formation in ocean general circulation models

... Southern Ocean. In many ocean general circulation model simulations with coarse resolution and a z-coordinate, a mid-depth salinity minimum characteristic of this intermediate water is ...real ... See full document

33

Modeling Of Tow Wrinkling In Automated Fiber Placement Based On Geometrical Considerations

Modeling Of Tow Wrinkling In Automated Fiber Placement Based On Geometrical Considerations

... examples include the polynyas in polar regions, the Mediterranean salty outflow (Parilla et al., 1993), and the subtropical south-west Australian inner shelf undergoing winter cooling (Pattiaratchi et al., 2011). Along ... See full document

241

Ocean Circulation Dynamics and Transport Connectivity in the Intra-Americas Sea on Inter-annual, Seasonal, Synoptic and Inertial Time Scales.

Ocean Circulation Dynamics and Transport Connectivity in the Intra-Americas Sea on Inter-annual, Seasonal, Synoptic and Inertial Time Scales.

... surface wind field and Loop Current conditions when hurricane Ida was passing through our study ...simulated ocean response from November 1, 2009 to December 7, 2009, a period encompassing the entire life ... See full document

158

Overturning circulation driven by breaking internal waves
in the deep ocean

Overturning circulation driven by breaking internal waves in the deep ocean

... upper ocean on density surfaces corresponding to the Antarctic Intermediate Water to 15 – 20 Sv at mid-depth on density surfaces corresponding to NADW and ...upper ocean is smaller than the transformation ... See full document

5

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