On the double-diffusive and cabbeling environments of the Arctic Front, West Spitsbergen

This paper describes the thermohaline characteristics of the Arctic Front to the west of Spitsbergen, in terms of the double-diffusive environment and the potential for densification through cabbeling. The front separates the warm, saline Atlantic water in the West Spitsbergen Current from the coole...

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Bibliographic Details
Published in:Polar Research
Main Authors: Cottier, Finlo, Venables, Emily
Format: Article in Journal/Newspaper
Language:English
Published: 2007
Subjects:
Geosciences
Multidisciplinary
Environmental Sciences
FRAM STRAIT
ATLANTIC WATER
HEAT-TRANSPORT
Oceanography
HYDROGRAPHY
SVALBARD
PACIFIC INTERMEDIATE WATER
Ecology
MASS
KONGSFJORDEN
Geography
Physical
THERMOHALINE INTRUSIONS
OCEAN
Arctic
Pacific
Svalbard
Fram Strait
Kongsfjord*
Kongsfjorden
Spitsbergen
Online Access:https://pure.uhi.ac.uk/en/publications/bf1f4b55-bc7d-4f42-8d46-7e2886913939
https://doi.org/10.1111/j.1751-8369.2007.00024.x
Description
Summary:This paper describes the thermohaline characteristics of the Arctic Front to the west of Spitsbergen, in terms of the double-diffusive environment and the potential for densification through cabbeling. The front separates the warm, saline Atlantic water in the West Spitsbergen Current from the cooler, fresher water on the West Spitsbergen Shelf. We have investigated processes at the front that can contribute to, or enhance, mixing and water mass modification in relation to heat transport to the Arctic. Hydrographic data were collected along a cross-shelf section in September 2005. The double-diffusive properties along the section were determined by calculating Turner angles, and cabbeling was investigated with a simple linear mixing scheme. Double diffusion, in the form of diffusive layering, was found to be active within the Arctic Front, with considerable interleaving between water masses. Furthermore, mixing of water masses across the front was found to generate a potential increase in density of more than 0.03 kg m(-3) through cabbeling, which would then promote sinking and convergence. Our analyses indicate that the two processes of double diffusion and cabbeling are active at the Arctic Front. We discuss their potential contribution to maintaining the density-compensated nature of the front, and conclude that they will promote isopycnal mixing and subsequent modification of the core water of the West Spitsbergen Current.

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