The purpose of this short communication is to present a method that aims to express the turbulent variables in the atmospheric surface-layer in function of the stability of the atmosphere. The case of very stable conditions (strong stratification), where theoretical approaches provide conflicting results (see Luhar et al. [11]), is analysed in detail to provide some insight into the limits of applicability for some of the most popular models of turbulence. The problem of the existence of the critical flux Richardson number is also taken into account.
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Univ Paris Est, Ecole Ponts ParisTech, LEESU, F-77455 Marne La Vallee, FranceUniv Paris Est, Ecole Ponts ParisTech, LEESU, F-77455 Marne La Vallee, France
Fitton, G.
Tchiguirinskaia, I.
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Univ Paris Est, Ecole Ponts ParisTech, LEESU, F-77455 Marne La Vallee, FranceUniv Paris Est, Ecole Ponts ParisTech, LEESU, F-77455 Marne La Vallee, France
Tchiguirinskaia, I.
Schertzer, D.
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Univ Paris Est, Ecole Ponts ParisTech, LEESU, F-77455 Marne La Vallee, FranceUniv Paris Est, Ecole Ponts ParisTech, LEESU, F-77455 Marne La Vallee, France
Schertzer, D.
Lovejoy, S.
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机构:Univ Paris Est, Ecole Ponts ParisTech, LEESU, F-77455 Marne La Vallee, France
Lovejoy, S.
13TH EUROPEAN TURBULENCE CONFERENCE (ETC13): GEOPHYSICAL AND MAGNETOHYDRODYNAMIC TURBULENCE,
2011,
318