A new method for forming approximately neutral surfaces

We introduce a simple algorithm to improve existing density surfaces to ensure that the resulting surfaces are as close to neutral as possible. This means the slopes at any point on the surfaces are close to neutral tangent planes – the directions along which layered stirring and mixing occurs – min...

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Main Authors: A. Klocker, T. J. McDougall, D. R. Jackett
Format: Article
Language:English
Published: Copernicus Publications 2009-05-01
Series:Ocean Science
Online Access:http://www.ocean-sci.net/5/155/2009/os-5-155-2009.pdf
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author A. Klocker
T. J. McDougall
D. R. Jackett
author_facet A. Klocker
T. J. McDougall
D. R. Jackett
author_sort A. Klocker
collection DOAJ
description We introduce a simple algorithm to improve existing density surfaces to ensure that the resulting surfaces are as close to neutral as possible. This means the slopes at any point on the surfaces are close to neutral tangent planes – the directions along which layered stirring and mixing occurs – minimizing the fictitious diapycnal diffusivity. Inverse techniques and layered models have been used for decades to understand ocean circulation. The most-used density surfaces are potential density or neutral density surfaces. Both these density surfaces and all others produce a fictitious diapycnal diffusivity to some degree due to the helical nature of neutral trajectories – with the magnitude of this artificial diffusivity in some cases being larger than the values measured in the ocean. Here we show how this error can be reduced by up to four orders of magnitude and therefore becomes insignificant compared to measured values, thus providing surfaces which would produce more accurate results when used for inverse techniques.
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spelling doaj.art-ec15bb12ac4640f38c461f78e1d44ee42022-12-22T01:08:04ZengCopernicus PublicationsOcean Science1812-07841812-07922009-05-0152155172A new method for forming approximately neutral surfacesA. KlockerT. J. McDougallD. R. JackettWe introduce a simple algorithm to improve existing density surfaces to ensure that the resulting surfaces are as close to neutral as possible. This means the slopes at any point on the surfaces are close to neutral tangent planes – the directions along which layered stirring and mixing occurs – minimizing the fictitious diapycnal diffusivity. Inverse techniques and layered models have been used for decades to understand ocean circulation. The most-used density surfaces are potential density or neutral density surfaces. Both these density surfaces and all others produce a fictitious diapycnal diffusivity to some degree due to the helical nature of neutral trajectories – with the magnitude of this artificial diffusivity in some cases being larger than the values measured in the ocean. Here we show how this error can be reduced by up to four orders of magnitude and therefore becomes insignificant compared to measured values, thus providing surfaces which would produce more accurate results when used for inverse techniques.http://www.ocean-sci.net/5/155/2009/os-5-155-2009.pdf
spellingShingle A. Klocker
T. J. McDougall
D. R. Jackett
A new method for forming approximately neutral surfaces
Ocean Science
title A new method for forming approximately neutral surfaces
title_full A new method for forming approximately neutral surfaces
title_fullStr A new method for forming approximately neutral surfaces
title_full_unstemmed A new method for forming approximately neutral surfaces
title_short A new method for forming approximately neutral surfaces
title_sort new method for forming approximately neutral surfaces
url http://www.ocean-sci.net/5/155/2009/os-5-155-2009.pdf
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