The dynamics of dense water cascades: from laboratory scales to the Arctic Ocean ...

The sinking of dense shelf waters down the continental slope (or “cascading”) contributes to oceanic water mass formation and carbon cycling. Cascading is therefore of significant importance for the global overturning circulation and thus climate. The occurrence of cascades is highly intermittent in...

Full description

Bibliographic Details
Main Author: Wobus, Fred
Format: Article in Journal/Newspaper
Language:English
Published: University of Plymouth 2013
Subjects:
Online Access:https://dx.doi.org/10.24382/4629
https://pearl.plymouth.ac.uk/handle/10026.1/1610
id ftdatacite:10.24382/4629
record_format openpolar
spelling ftdatacite:10.24382/4629 2024-04-28T08:08:38+00:00 The dynamics of dense water cascades: from laboratory scales to the Arctic Ocean ... Wobus, Fred 2013 https://dx.doi.org/10.24382/4629 https://pearl.plymouth.ac.uk/handle/10026.1/1610 en eng University of Plymouth Mumerical Modelling Dense water cascading Gravity currents Ocean circulation Geophysical fluid dynamics Arctic Ocean Svalbard Spitsbergen Tidal mixing article CreativeWork 2013 ftdatacite https://doi.org/10.24382/4629 2024-04-02T09:44:20Z The sinking of dense shelf waters down the continental slope (or “cascading”) contributes to oceanic water mass formation and carbon cycling. Cascading is therefore of significant importance for the global overturning circulation and thus climate. The occurrence of cascades is highly intermittent in space and time and observations of the process itself (rather than its outcomes) are scarce. Global climate models do not typically resolve cascading owing to numerical challenges concerning turbulence, mixing and faithful representation of bottom boundary layer dynamics. This work was motivated by the need to improve the representation of cascading in numerical ocean circulation models. Typical 3-D hydrostatic ocean circulation models are employed in a series of numerical experiments to investigate the process of dense water cascading in both idealised and realistic model setups. Cascading on steep bottom topography is modelled using POLCOMS, a 3-D ocean circulation model using a terrain-following s-coordinate ... Article in Journal/Newspaper Arctic Arctic Ocean Svalbard Spitsbergen DataCite Metadata Store (German National Library of Science and Technology)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
topic Mumerical Modelling
Dense water cascading
Gravity currents
Ocean circulation
Geophysical fluid dynamics
Arctic Ocean
Svalbard
Spitsbergen
Tidal mixing
spellingShingle Mumerical Modelling
Dense water cascading
Gravity currents
Ocean circulation
Geophysical fluid dynamics
Arctic Ocean
Svalbard
Spitsbergen
Tidal mixing
Wobus, Fred
The dynamics of dense water cascades: from laboratory scales to the Arctic Ocean ...
topic_facet Mumerical Modelling
Dense water cascading
Gravity currents
Ocean circulation
Geophysical fluid dynamics
Arctic Ocean
Svalbard
Spitsbergen
Tidal mixing
description The sinking of dense shelf waters down the continental slope (or “cascading”) contributes to oceanic water mass formation and carbon cycling. Cascading is therefore of significant importance for the global overturning circulation and thus climate. The occurrence of cascades is highly intermittent in space and time and observations of the process itself (rather than its outcomes) are scarce. Global climate models do not typically resolve cascading owing to numerical challenges concerning turbulence, mixing and faithful representation of bottom boundary layer dynamics. This work was motivated by the need to improve the representation of cascading in numerical ocean circulation models. Typical 3-D hydrostatic ocean circulation models are employed in a series of numerical experiments to investigate the process of dense water cascading in both idealised and realistic model setups. Cascading on steep bottom topography is modelled using POLCOMS, a 3-D ocean circulation model using a terrain-following s-coordinate ...
format Article in Journal/Newspaper
author Wobus, Fred
author_facet Wobus, Fred
author_sort Wobus, Fred
title The dynamics of dense water cascades: from laboratory scales to the Arctic Ocean ...
title_short The dynamics of dense water cascades: from laboratory scales to the Arctic Ocean ...
title_full The dynamics of dense water cascades: from laboratory scales to the Arctic Ocean ...
title_fullStr The dynamics of dense water cascades: from laboratory scales to the Arctic Ocean ...
title_full_unstemmed The dynamics of dense water cascades: from laboratory scales to the Arctic Ocean ...
title_sort dynamics of dense water cascades: from laboratory scales to the arctic ocean ...
publisher University of Plymouth
publishDate 2013
url https://dx.doi.org/10.24382/4629
https://pearl.plymouth.ac.uk/handle/10026.1/1610
genre Arctic
Arctic Ocean
Svalbard
Spitsbergen
genre_facet Arctic
Arctic Ocean
Svalbard
Spitsbergen
op_doi https://doi.org/10.24382/4629
_version_ 1797577334699589632