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Relevant bibliographies by topics / Stratification thermohaline

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Journal articles

Academic literature on the topic 'Stratification thermohaline'

Author: Grafiati

Published: 23 September 2022

Last updated: 28 January 2023

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Journal articles on the topic "Stratification thermohaline"

1

Schladow, S. Geoffrey, Ellen Thomas, and Jeffrey R. Koseff. "The dynamics of intrusions into a thermohaline stratification." Journal of Fluid Mechanics 236 (March 1992): 127–65. http://dx.doi.org/10.1017/s002211209200137x.

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Physical and numerical experiments were performed for a linearly stratified heat—salt system, uniformly heated at one endwall. The initial stratification was in the diffusive sense. Intrusions formed at the heated endwall and propagated out into the interior fluid. Three classes of flow were identified, based upon the gravitational stability ratio, Rp, and a lateral stability parameter, R1, For R1 > 1, a vertical lengthscale for the initial intrusion thickness was developed which agreed well with that observed in the physical experiments. In all cases, a region of salt fingering developed d

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2

Gong, Ye-Jun, Ying-Ying Luo, and Jie-Min Zhan. "Three-dimensional buoyancy-driven convection structures in thermohaline stratification." AIP Advances 6, no. 4 (2016): 045303. http://dx.doi.org/10.1063/1.4946783.

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3

Gordon, Arnold L., and Julie L. McClean. "Thermohaline Stratification of the Indonesian Seas: Model and Observations*." Journal of Physical Oceanography 29, no. 2 (1999): 198–216. http://dx.doi.org/10.1175/1520-0485(1999)029<0198:tsotis>2.0.co;2.

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4

Radko, Timour. "Thermohaline layering on the microscale." Journal of Fluid Mechanics 862 (January 14, 2019): 672–95. http://dx.doi.org/10.1017/jfm.2018.976.

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A theoretical model is developed which illustrates the dynamics of layering instability, frequently realized in ocean regions with active fingering convection. Thermohaline layering is driven by the interplay between large-scale stratification and primary double-diffusive instabilities operating at the microscale – temporal and spatial scales set by molecular dissipation. This interaction is described by a combination of direct numerical simulations and an asymptotic multiscale model. The multiscale theory is used to formulate explicit and dynamically consistent flux laws, which can be readily

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5

Stein, M. "Impacts of "Storis" on the Thermohaline Stratification off West Greenland." Journal of Northwest Atlantic Fishery Science 43 (March 17, 2010): 1–12. http://dx.doi.org/10.2960/j.v43.m655.

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6

Wright, J., and W. Shyy. "Numerical simulation of unsteady convective intrusions in a thermohaline stratification." International Journal of Heat and Mass Transfer 39, no. 6 (1996): 1183–201. http://dx.doi.org/10.1016/0017-9310(95)00214-6.

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7

Morin, P., P. Le Corre, and J. Le Févre. "Assimilation Aand Regeneration of Nutrients off the West Coast of Brittany." Journal of the Marine Biological Association of the United Kingdom 65, no. 3 (1985): 677–95. http://dx.doi.org/10.1017/s0025315400052528.

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A high degree of variation in hydrographic conditions is found in the so-called Iroise Sea, within less than 100 km of the west coast of Brittany. Tidal current maximal velocity, especially, ranges there from about 0·5 knot to more than 8 knots (locally, near the island of Ushant), i.e. practically as wide a range as found over the whole of north-west European shelf seas. Pelagic ecosystems accordingly exhibit a high degree of variety, related not only to classical inshore-offshore gradients, but also to the extent of vertical mixing or stratification. Areas where different physical and biolog

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8

Radko, Timour. "Thermohaline layering in dynamically and diffusively stable shear flows." Journal of Fluid Mechanics 805 (September 16, 2016): 147–70. http://dx.doi.org/10.1017/jfm.2016.547.

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In this study we examine two-component shear flows that are stable with respect to Kelvin–Helmholtz and to double-diffusive instabilities individually. Our focus is on diffusively stratified ocean regions, where relatively warm and salty water masses are located below cool fresh ones. It is shown that such systems may be destabilized by the interplay between shear and thermohaline effects, caused by unequal molecular diffusivities of density components. Linear stability analysis suggests that parallel two-component flows can be unstable for Richardson numbers exceeding the critical value for n

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9

Arnon, A., J. S. Selker, and N. G. Lensky. "Thermohaline stratification and double diffusion diapycnal fluxes in the hypersaline Dead Sea." Limnology and Oceanography 61, no. 4 (2016): 1214–31. http://dx.doi.org/10.1002/lno.10285.

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10

Liblik, T., and U. Lips. "Variability of synoptic-scale quasi-stationary thermohaline stratification patterns in the Gulf of Finland in summer 2009." Ocean Science 8, no. 4 (2012): 603–14. http://dx.doi.org/10.5194/os-8-603-2012.

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Abstract. We present and analyze high-resolution observational data of thermohaline structure and currents acquired in the Gulf of Finland (Baltic Sea), using an autonomous buoy profiler and bottom-mounted acoustic Doppler current profiler during July–August 2009. Vertical profiles of temperature and salinity were measured in the upper 50-m layer with a 3 h time resolution, and vertical profiles of current velocity and direction were recorded with a 10 min time resolution. Although large temporal variations of vertical temperature and salinity distributions were revealed, it was possible to de

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