http://www.cnr.it/ontology/cnr/individuo/prodotto/ID44505
Statistics of temperature fluctuactions in a buoyancy dominated boundary layer flow simulated by a large eddy simulation model (Articolo in rivista)
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- Label
- Statistics of temperature fluctuactions in a buoyancy dominated boundary layer flow simulated by a large eddy simulation model (Articolo in rivista) (literal)
- Anno
- 2003-01-01T00:00:00+01:00 (literal)
- Http://www.cnr.it/ontology/cnr/pubblicazioni.owl#doi
- 10.1175/1520-0469(2003)060<0215:SOTFIA>2.0.CO;2 (literal)
- Alternative label
Antonelli M., Mazzino A., Rizza U. (2003)
Statistics of temperature fluctuactions in a buoyancy dominated boundary layer flow simulated by a large eddy simulation model
in Journal of the atmospheric sciences
(literal)
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- Antonelli M., Mazzino A., Rizza U. (literal)
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- Rivista
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- Research letter su JAS (literal)
- Note
- ISI Web of Science (WOS) (literal)
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- Andrea Mazzino : Università di Genova
Marta Antonelli : Università di Genova
Umberto Rizza : ISAC-CNR / Sezione di Lecce (literal)
- Titolo
- Statistics of temperature fluctuactions in a buoyancy dominated boundary layer flow simulated by a large eddy simulation model (literal)
- Abstract
- Temperature fluctuations in an atmospheric convective boundary layer are investigated by means of large eddy simulations (LES). A novel statistical characterization for both weak temperature fluctuations and strong
temperature fluctuations has been found. Despite the nontriviality of the dynamics of temperature fluctuations, the data presented here support the idea that the most relevant statistical properties can be captured solely in terms of two scaling exponents, characterizing the entire mixed layer. Such exponents control asymptotic (i.e., core and tails) rescaling properties of the probability density functions of equal-time temperature differences Dr ubetween points separated by a distance r. A link between statistical properties of large temperature fluctuations and geometrical properties of the set hosting such fluctuations is also provided. Finally, a possible application of these new findings to the problem of subgrid-scale parameterizations for the temperature field in a convective
boundary layer is discussed. (literal)
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