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Shelf-Life Prediction of Shrimp Gravlax Using Machine Learning: Integrating Traditional Processing with AI Modeling. [PDF]
FoodsEmir Coban O +3 more
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Code and Data for "Towards Frazil Ice Crystal Size Measurements in Ice Shelf Water"
Caldarella, Nina +8 more
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Spatial distribution of Ice Shelf Water in front of the Amery Ice Shelf, Antarctica in summer
Chinese Journal of Oceanology and Limnology, 2011As a unique low-temperature water mass in Antarctic coastal region, the Ice Shelf Water (ISW) is an important component for the formation of the Antarctic Bottom Water (AABW). In this paper, we present a criterion for ISW identification based on freezing point at the sea surface, and we study spatial distribution of ISW in front of the Amery Ice Shelf (
Shaojun Zheng +3 more
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Oxygen 18 and helium as tracers of ice shelf water and water/ice interaction in the Weddell Sea
Journal of Geophysical Research: Oceans, 1990Oxygen 18 and helium isotope data from stations located in the Filchner Depression, on the continental slope of the southern Weddell Sea, and in the central Weddell Sea are presented and discussed. The 18O and 4He signals imprinted on the water circulating under the Filchner/Ronne Ice Shelf (Ice Shelf Water, or ISW) due to melting of glacial ice at the
Peter Schlosser +5 more
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A model for the spreading and sinking of the Deep Ice Shelf Water in the Ross Sea
Antarctic Science, 2003Spreading and sinking of the Deep Ice Shelf Water (DISW) in the Ross Sea are analysed using in situ observations and the results of a nonlinear, reduced gravity, layered numerical model, which is able to simulate the motion of a bottom trapped current over realistic topography.
RUBINO A. +3 more
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Journal of Geophysical Research: Oceans, 1995
The seawater that comes into contact with the base of a floating ice shelf is modified as a result of the phase changes that occur. Melting is prevalent in the deepest parts of the subice cavity, and this drives a buoyant flow of Ice Shelf Water (ISW) along the sloping ice shelf base.
Jenkins, Adrian, Bombosch, Andreas
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The seawater that comes into contact with the base of a floating ice shelf is modified as a result of the phase changes that occur. Melting is prevalent in the deepest parts of the subice cavity, and this drives a buoyant flow of Ice Shelf Water (ISW) along the sloping ice shelf base.
Jenkins, Adrian, Bombosch, Andreas
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Towards Frazil Ice Crystal Size Measurements in Ice Shelf Water
Frazil ice forms in supercooled water beneath ice shelves, where direct observations are needed to constrain ice–ocean heat and mass exchange. This study presents the design, testing, and initial deployment of a prototype optical frazil ice imaging system in McMurdo Sound, Antarctica, in 2022.Nina Caldarella +8 more
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Journal of Physical Oceanography, 1979
Abstract Steady-state conditions are assumed to exist everywhere in the case of melting of the underside of an infinite slab of ice floating in sea water. Basic transfer equations for heat and salt are established and solutions derived for the interior corresponding to given far field values of the temperature and salinity of the water.
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Abstract Steady-state conditions are assumed to exist everywhere in the case of melting of the underside of an infinite slab of ice floating in sea water. Basic transfer equations for heat and salt are established and solutions derived for the interior corresponding to given far field values of the temperature and salinity of the water.
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Doklady Earth Sciences, 2011
The authors develop a model of shelf water convection and cascading in the Arctic basin. The motion of more saline water along the slope takes place in the Ekman layer near the bottom. The salt balance equation across slope is analogous to the heat balance equation.
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The authors develop a model of shelf water convection and cascading in the Arctic basin. The motion of more saline water along the slope takes place in the Ekman layer near the bottom. The salt balance equation across slope is analogous to the heat balance equation.
openaire +2 more sources