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geophysical flows

Kühnlein, Christian
  

(2011):


	Solution-adaptive moving mesh solver for geophysical flows.


Dissertation, LMU München: Fakultät für Physik

Kühnlein, Christian (2011): Solution-adaptive moving mesh solver for geophysical flows. Dissertation, LMU München: Fakultät für Physik

... In particular, the recent work by Prusa and Smolarkiewicz (2003) established a generic framework for the implementation of a dynamic mesh adaptation capabil- ity via deforming coordinates. The foundation of the dynamic ...

171

The persistence of balance in geophysical flows

The persistence of balance in geophysical flows

... stratified geophysical flows can exhibit a near ‘balanced’ evolution controlled by the conservative advection of a single scalar quantity, the potential vorticity ...

19

Connection between encounter volume and diffusivity in geophysical flows

Connection between encounter volume and diffusivity in geophysical flows

... diffusive, so the diffusive theoretical formulas work poorly. The breakdown of the long-time asymptotic formula is ev- ident in the fourth row of Fig. 4, which shows the corre- sponding long-time scales, τ (from Eq. 35), ...

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Algorithms for Bed Topography Reconstruction in Geophysical Flows

Algorithms for Bed Topography Reconstruction in Geophysical Flows

... 15]. Thus glaciers are useful not only for the aforementioned purposes but also for meteorological and climate change studies which are indicators of environmental health. The studies of glaciers may range from ...

222

A balanced approach to modelling rotating stably stratified geophysical flows

A balanced approach to modelling rotating stably stratified geophysical flows

... In the shallow-water equations, this is not a major limitation, although it can lead to nonlinear diagnostic equations for the primitive variables depending on the choice of imbalance va[r] ...

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Ergodicity of stochastically forced large scale geophysical flows

Ergodicity of stochastically forced large scale geophysical flows

... The quasigeostrophic equation has been derived as an approximation of the rotating shallow water equations by the conventional asymptotic expansion in small Rossby number [14]. Recently, the randomly forced ...

8

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] ...

134

Time dependent dynamical systems and geophysical flows

Time dependent dynamical systems and geophysical flows

... A general physical lesson from our analysis is that focused Lagrangian predictions for a geophysical flow can be feasible even if global Eulerian (i.e., velocity based) predictions are unrealistic. We need to ...

165

Particle clustering and subclustering as a proxy for  mixing in geophysical flows

Particle clustering and subclustering as a proxy for mixing in geophysical flows

... Abstract. The Eulerian point of view is the traditional theo- retical and numerical tool to describe fluid mechanics. Some modern computational fluid dynamics codes allow for the efficient simulation of particles, in ...

18

A note on Taylor’s hypothesis under large-scale flow variation

A note on Taylor’s hypothesis under large-scale flow variation

... Abstract. Experimental investigations of turbulent velocity fields often invoke Taylor’s hypothesis (also known as frozen turbulence approximation) to evaluate the spatial structure based on time-resolved single-point ...

5

Geophysical mapping of palsa peatland permafrost

Geophysical mapping of palsa peatland permafrost

... of geophysical data requires other types of complementary data, such as sediment ...more geophysical methods comple- mentary information can often be acquired raising the con- fidence in interpretations of ...

14

Capital flow to China and the issue of hot money: an empirical investigation

Capital flow to China and the issue of hot money: an empirical investigation

... equity flows, bank credit flows has a relatively larger share of variance which could be explained by the nonstationary stochastic ...credit flows may be regarded as more persistent than portfolio ...

39

Geophysical investigations of Tasmania at multiple scales

Geophysical investigations of Tasmania at multiple scales

... metamorphosed in the Cambrian Tyennan Orogeny (Chmielowski and Berry, 2012) and are bound to the Heazlewood River Complexes and Luina Group. To the east, the fault bounded Mt Bischoff Inlier comprises pelites, quartz- ...

199

Geophysical Hunt for Chromite in Ophiolite

Geophysical Hunt for Chromite in Ophiolite

... The geophysical exploration for the purpose of exploring economic deposits or finding subsurface geological objects requires two considerations: the data density and strong physical contrast between the target and ...

7

The Analyze of the Risk Management and Control of Internal Audit

The Analyze of the Risk Management and Control of Internal Audit

... cash flows from operations, cash flows from investing and financing cash ...cash flows will equal the change in status of cash at the beginning of the period with the situation at the end of the ...

5

Magnetic airborne survey – geophysical flight

Magnetic airborne survey – geophysical flight

... utilized both magnetic and radiometric methods. The fixed- wing aircraft PBY-5 (Catalina) was used in the survey. It was equipped with a Fluxgate magnetometer in the tail of the air- craft, which measured the total ...

12

Magma plumbing systems: a geophysical perspective

Magma plumbing systems: a geophysical perspective

... Magee, C. and Stevenson, C.T.E and Ebmeier, S.K. and Keir, D. and Hammond, James O.S. and Gottsmann, J.H. and Whaler, K.A. and Schofield, N. and Jackson, C.A.-L. and Petronis, M.S. and O’Driscoll, B. and Morgan, J. and ...

98

Predictability of extreme values in geophysical models

Predictability of extreme values in geophysical models

... typically taking 30 days, (2) transitions from blocked to zonal flows, typically taking 40–80 days, and (3) spiraling be- haviour around the zonal regime, typically lasting more than 200 days. This intermittent ...

11

The Application of Joint Inversion in Geophysical Exploration

The Application of Joint Inversion in Geophysical Exploration

... A common fact in geophysical exploration is that several measured data are connected to one station, e.g. VES (Vertical Electric Sounding) and magnetotelluric data. The simultaneous inversion of two different ...

7

CSIR National Geophysical Research Institute

CSIR National Geophysical Research Institute

... heliborne geophysical surveys to map regional-scale aquifer system in three-dimension and integrating these results with the geological and hydro- geological data have been useful to reliably characterize ...

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