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Interocean exchange of water masses
Journal of Geophysical Research: Oceans, 1995A new method for calculating water mass transport between different ocean basins from the velocity fields obtained by numerical models is presented. The method is applied to the velocity field of the Southern Ocean simulated by a primitive equation model (fine resolution Antarctic model).
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Lateral mixing of water masses
Deep Sea Research and Oceanographic Abstracts, 1967Abstract The vertical transport of heat and salt in the “salt-finger” convective regime can be enhanced by the vertical shear of a “medium” scale motion. A weak shear converts compensating temperature-salinity variations on isopycnal surfaces into strong vertical T-S gradients.
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Dynamics of Atmospheres and Oceans, 1999
We have derived a water mass model for the Strait of Sicily, based on 1994 and 1995 cruise data. The model consists of seven water masses, suggested by the measured shapes of the vertical temperature and salinity distributions. The core of the Atlantic water is distributed below the surface as a shallow layer, in a depth range of 40 to 100 m, with a ...
A Warn-Varnas +4 more
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We have derived a water mass model for the Strait of Sicily, based on 1994 and 1995 cruise data. The model consists of seven water masses, suggested by the measured shapes of the vertical temperature and salinity distributions. The core of the Atlantic water is distributed below the surface as a shallow layer, in a depth range of 40 to 100 m, with a ...
A Warn-Varnas +4 more
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Journal of Geophysical Research, 1970
The theory of mass transport in water waves is re-examined. Boundary-layer arguments are incorporated into the Lagrangian equations of motion, and the mass transport velocity is conveniently derived for both monochromatic and random waves. For finite depth, Longuet-Higgins' result is confirmed.
Ümit Ünlüata, Chiang C. Mei
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The theory of mass transport in water waves is re-examined. Boundary-layer arguments are incorporated into the Lagrangian equations of motion, and the mass transport velocity is conveniently derived for both monochromatic and random waves. For finite depth, Longuet-Higgins' result is confirmed.
Ümit Ünlüata, Chiang C. Mei
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Water masses and faunal movements
Proceedings of the Royal Society of London. Series B. Biological Sciences, 1960H. Brattström (Zoology Department, University of Bergen) I should like to underline what Professor Dahl and Professor Knox have said: that there seems not to exist, in western South America, a marked border between a cold and a warm temperate zone.
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1994
The water in the shallow parts of the Huanghai (Yellow) and East China seas is affected greatly by climatic and geographical conditions; it does not have the homogeneity and conservativeness of ocean water. Temperature and salinity data gained in 1978–1980 monthly sectional observations were used to study the water masses in these areas.
Su Yu-song, Weng Xue-chuan
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The water in the shallow parts of the Huanghai (Yellow) and East China seas is affected greatly by climatic and geographical conditions; it does not have the homogeneity and conservativeness of ocean water. Temperature and salinity data gained in 1978–1980 monthly sectional observations were used to study the water masses in these areas.
Su Yu-song, Weng Xue-chuan
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Water mass exchange and diapycnal mixing at Bussol’ Strait revealed by water mass properties
Journal of Oceanography, 2007Intensive CTD observations that resolve the mean and tidal components were done with a total of 129 casts in summer of 2001 at Bussol’ Strait. Based on these data and all the available historical data, we have revealed the outflow from Bussol’ Strait to the Pacific and the significant diapycnal mixing in the strait. In the range 27.0−27.3σ
Kazuya Ono +6 more
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Philosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1953
It was shown by Stokes that in a water wave the particles of fluid possess, apart from their orbital motion, a steady second-order drift velocity (usually called the mass-transport velocity). Recent experiments, however, have indicated that the mass-transport velocity can be very different from that predicted by Stokes on the assumption of
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It was shown by Stokes that in a water wave the particles of fluid possess, apart from their orbital motion, a steady second-order drift velocity (usually called the mass-transport velocity). Recent experiments, however, have indicated that the mass-transport velocity can be very different from that predicted by Stokes on the assumption of
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Water Security and Mass Migration
2020Abstract The world faces an unprecedented human migration crisis, as hundreds of thousands flee famine, poverty, and violence in many parts of the globe. While the movement of these people from one country to another can appear, on the surface, as a response to current events, these migrations can perhaps be best understood with an ...
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Water mass transfer in W/O emulsions
Journal of Colloid and Interface Science, 2006Water transportation through the oil phase in W/O emulsions and in W1/O/W2 systems (W/O emulsion in contact with water) was examined. Substance diffusion through interfaces led to interface instability and spontaneous emulsification which caused nanodispersion formation.
Marina Yu, Koroleva, Evgeny V, Yurtov
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