Unified multifractal atmospheric dynamics tested in the tropics: part I, horizontal scaling and self criticality

In this paper we test the Unified Mulifractal model of atmospheric dynamics in the tropics. In the first part, we empirically investigate the scaling behaviour along the horizontal, in the second part along the vertical. Here we concentrate on the presentation of basic multifractal notions and techn...

Full description

Bibliographic Details
Main Authors: Y. Chigirinskaya, D. Schertzer, S. Lovejoy, A. Lazarev, A. Ordanovich
Format: Article
Language:English
Published: Copernicus Publications 1994-01-01
Series:Nonlinear Processes in Geophysics
Online Access:http://www.nonlin-processes-geophys.net/1/105/1994/npg-1-105-1994.pdf
id doaj-6002b177c6d645f6b9d4c00abc460f26
record_format Article
spelling doaj-6002b177c6d645f6b9d4c00abc460f262020-11-24T22:54:28ZengCopernicus PublicationsNonlinear Processes in Geophysics1023-58091607-79461994-01-0112/3105114Unified multifractal atmospheric dynamics tested in the tropics: part I, horizontal scaling and self criticalityY. ChigirinskayaY. ChigirinskayaD. SchertzerS. LovejoyS. LovejoyA. LazarevA. OrdanovichIn this paper we test the Unified Mulifractal model of atmospheric dynamics in the tropics. In the first part, we empirically investigate the scaling behaviour along the horizontal, in the second part along the vertical. Here we concentrate on the presentation of basic multifractal notions and techniques and on how they give rise to self-organized critical structures. Indeed, we point out a rather simple and clear characterisation of these structures which may help to clarify both the nature of the oft-cited coherent structures and the generation of cyclones. Using 30 aircraft series of horizontal wind and temperature, we find rather remarkable constancy of the three universal multifractal indices <i>H</i>, <i>C<sub>1</sub></i> and α as well as the value of critical exponents <i>q<sub>D</sub></i>, <i>γ<sub>D</sub></i> associated with multifractal phase transitions and self-organized critical structures. This constancy extends not only from wind tunnel and mid-latitude to the tropics, but also to multifractals generated by Navier-Stokes like equations.http://www.nonlin-processes-geophys.net/1/105/1994/npg-1-105-1994.pdf
collection DOAJ
language English
format Article
sources DOAJ
author Y. Chigirinskaya
Y. Chigirinskaya
D. Schertzer
S. Lovejoy
S. Lovejoy
A. Lazarev
A. Ordanovich
spellingShingle Y. Chigirinskaya
Y. Chigirinskaya
D. Schertzer
S. Lovejoy
S. Lovejoy
A. Lazarev
A. Ordanovich
Unified multifractal atmospheric dynamics tested in the tropics: part I, horizontal scaling and self criticality
Nonlinear Processes in Geophysics
author_facet Y. Chigirinskaya
Y. Chigirinskaya
D. Schertzer
S. Lovejoy
S. Lovejoy
A. Lazarev
A. Ordanovich
author_sort Y. Chigirinskaya
title Unified multifractal atmospheric dynamics tested in the tropics: part I, horizontal scaling and self criticality
title_short Unified multifractal atmospheric dynamics tested in the tropics: part I, horizontal scaling and self criticality
title_full Unified multifractal atmospheric dynamics tested in the tropics: part I, horizontal scaling and self criticality
title_fullStr Unified multifractal atmospheric dynamics tested in the tropics: part I, horizontal scaling and self criticality
title_full_unstemmed Unified multifractal atmospheric dynamics tested in the tropics: part I, horizontal scaling and self criticality
title_sort unified multifractal atmospheric dynamics tested in the tropics: part i, horizontal scaling and self criticality
publisher Copernicus Publications
series Nonlinear Processes in Geophysics
issn 1023-5809
1607-7946
publishDate 1994-01-01
description In this paper we test the Unified Mulifractal model of atmospheric dynamics in the tropics. In the first part, we empirically investigate the scaling behaviour along the horizontal, in the second part along the vertical. Here we concentrate on the presentation of basic multifractal notions and techniques and on how they give rise to self-organized critical structures. Indeed, we point out a rather simple and clear characterisation of these structures which may help to clarify both the nature of the oft-cited coherent structures and the generation of cyclones. Using 30 aircraft series of horizontal wind and temperature, we find rather remarkable constancy of the three universal multifractal indices <i>H</i>, <i>C<sub>1</sub></i> and α as well as the value of critical exponents <i>q<sub>D</sub></i>, <i>γ<sub>D</sub></i> associated with multifractal phase transitions and self-organized critical structures. This constancy extends not only from wind tunnel and mid-latitude to the tropics, but also to multifractals generated by Navier-Stokes like equations.
url http://www.nonlin-processes-geophys.net/1/105/1994/npg-1-105-1994.pdf
work_keys_str_mv AT ychigirinskaya unifiedmultifractalatmosphericdynamicstestedinthetropicspartihorizontalscalingandselfcriticality
AT ychigirinskaya unifiedmultifractalatmosphericdynamicstestedinthetropicspartihorizontalscalingandselfcriticality
AT dschertzer unifiedmultifractalatmosphericdynamicstestedinthetropicspartihorizontalscalingandselfcriticality
AT slovejoy unifiedmultifractalatmosphericdynamicstestedinthetropicspartihorizontalscalingandselfcriticality
AT slovejoy unifiedmultifractalatmosphericdynamicstestedinthetropicspartihorizontalscalingandselfcriticality
AT alazarev unifiedmultifractalatmosphericdynamicstestedinthetropicspartihorizontalscalingandselfcriticality
AT aordanovich unifiedmultifractalatmosphericdynamicstestedinthetropicspartihorizontalscalingandselfcriticality
_version_ 1725659642533511168