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International Journal of Fluid Mechanics Research

Publicou 6 edições por ano

ISSN Imprimir: 2152-5102

ISSN On-line: 2152-5110

The Impact Factor measures the average number of citations received in a particular year by papers published in the journal during the two preceding years. 2017 Journal Citation Reports (Clarivate Analytics, 2018) IF: 1.1 To calculate the five year Impact Factor, citations are counted in 2017 to the previous five years and divided by the source items published in the previous five years. 2017 Journal Citation Reports (Clarivate Analytics, 2018) 5-Year IF: 1.3 The Eigenfactor score, developed by Jevin West and Carl Bergstrom at the University of Washington, is a rating of the total importance of a scientific journal. Journals are rated according to the number of incoming citations, with citations from highly ranked journals weighted to make a larger contribution to the eigenfactor than those from poorly ranked journals. Eigenfactor: 0.0002 The Journal Citation Indicator (JCI) is a single measurement of the field-normalized citation impact of journals in the Web of Science Core Collection across disciplines. The key words here are that the metric is normalized and cross-disciplinary. JCI: 0.33 SJR: 0.256 SNIP: 0.49 CiteScore™:: 2.4 H-Index: 23

Indexed in

Spectrum of Turbulent Fluctuations of the Sea-Water Refraction Index

Volume 27, Edição 1, 2000, pp. 82-98
DOI: 10.1615/InterJFluidMechRes.v27.i1.70
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RESUMO

The behavior of the spectrum of fluctuations En of refraction index n in turbulent sea water when the fluctuations of n are controlled by fluctuations T' of the temperature and S' of the salinity is analyzed. The spectrum of En is found for homogeneous and isotropic turbulence as a function of the rate of dissipation (equalization) of temperature and salinity fluctuations which, together with the dissipation rate of the energy of turbulence, control the statistical behavior of fluctuations of n. These rates were parametrized by employing the gradient hypothesis. It was found that, depending on the contributions of temperature and salinity fluctuations to fluctuations of n, one may observe domains of anomal behavior which may include appearance of local extrema.

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