Material derivatives of higher dimension in geophysical fluid dynamics

The familiar operator D/Dt in fluid dynamics defines the material derivative for a fluid particle with dimension zero. In this paper we define and use "macroscopic" or multidimensional material derivatives D1/Dt, D2/Dt and D3/Dt. They are the material derivatives of infinitesimal propertie...

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Main Author: Heinz Fortak
Format: Article
Language:English
Published: Borntraeger 2004-12-01
Series:Meteorologische Zeitschrift
Online Access:http://dx.doi.org/10.1127/0941-2948/2004/0013-0499
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author Heinz Fortak
author_facet Heinz Fortak
author_sort Heinz Fortak
collection DOAJ
description The familiar operator D/Dt in fluid dynamics defines the material derivative for a fluid particle with dimension zero. In this paper we define and use "macroscopic" or multidimensional material derivatives D1/Dt, D2/Dt and D3/Dt. They are the material derivatives of infinitesimal properties of the fluid having dimensions, i.e. when particles build a line, a surface area, or a volume. Simple rules between the three operators are presented that avoid complicated calculations in fluid dynamics. For example, these operators are invariant with respect to solid rotations of coordinate systems. We rewrite a number of equations of fluid dynamics in terms of these operators and show that simple identities involving these operators already contain the structure of known vorticity theorems, especially those given by Hans Ertel. One application deals with the circulation of eddy velocities in atmospheric turbulence, showing that this circutation maybe an almost material invariant with time. Further possible applications (e.g., in electrodynamics of fluids and in radiation hydrodynamics) are also suggested.
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spelling doaj.art-29d6cec391a84a7d829c043b5c36b2ad2024-02-08T08:44:37ZengBorntraegerMeteorologische Zeitschrift0941-29482004-12-0113649951010.1127/0941-2948/2004/0013-049953390Material derivatives of higher dimension in geophysical fluid dynamicsHeinz FortakThe familiar operator D/Dt in fluid dynamics defines the material derivative for a fluid particle with dimension zero. In this paper we define and use "macroscopic" or multidimensional material derivatives D1/Dt, D2/Dt and D3/Dt. They are the material derivatives of infinitesimal properties of the fluid having dimensions, i.e. when particles build a line, a surface area, or a volume. Simple rules between the three operators are presented that avoid complicated calculations in fluid dynamics. For example, these operators are invariant with respect to solid rotations of coordinate systems. We rewrite a number of equations of fluid dynamics in terms of these operators and show that simple identities involving these operators already contain the structure of known vorticity theorems, especially those given by Hans Ertel. One application deals with the circulation of eddy velocities in atmospheric turbulence, showing that this circutation maybe an almost material invariant with time. Further possible applications (e.g., in electrodynamics of fluids and in radiation hydrodynamics) are also suggested.http://dx.doi.org/10.1127/0941-2948/2004/0013-0499
spellingShingle Heinz Fortak
Material derivatives of higher dimension in geophysical fluid dynamics
Meteorologische Zeitschrift
title Material derivatives of higher dimension in geophysical fluid dynamics
title_full Material derivatives of higher dimension in geophysical fluid dynamics
title_fullStr Material derivatives of higher dimension in geophysical fluid dynamics
title_full_unstemmed Material derivatives of higher dimension in geophysical fluid dynamics
title_short Material derivatives of higher dimension in geophysical fluid dynamics
title_sort material derivatives of higher dimension in geophysical fluid dynamics
url http://dx.doi.org/10.1127/0941-2948/2004/0013-0499
work_keys_str_mv AT heinzfortak materialderivativesofhigherdimensioningeophysicalfluiddynamics