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dc.contributor.author Krusche, Nisia
dc.contributor.author Oliveira, Amauri Pereira de
dc.date.accessioned 2015-05-30T00:21:11Z
dc.date.available 2015-05-30T00:21:11Z
dc.date.issued 2004
dc.identifier.citation KRUSCHE, Nisia; OLIVEIRA, Amauri Pereira de. Characterization of coherent structures in the atmospheric surface layer. Boundary-Layer Meteorology, v. 110, n. 2, 2004. Disponível em: <http://link.springer.com/article/10.1023%2FA%3A1026096805679>. Acesso em: 24 abr. 2015. pt_BR
dc.identifier.issn 0006-8314
dc.identifier.issn 1573-1472
dc.identifier.uri http://repositorio.furg.br/handle/1/4956
dc.description.abstract The ramplike coherent structures, observed in the temporal series of temperature and humidity in the atmospheric surface layer, are analyzed using the intermittency function and the wavelet transforms, with Haar, D4 and Mexican Hat functions as mother wavelets, in order to find the most efficient conditional sampling technique. It was found that the intermittency function and the wavelet transform, using Mexican Hat as mother wavelet, are the only ones that sample structures that fulfill the ramplike coherent structures definition of a slow rise followed by a sudden drop in the temporal series. The conditionally averaged structures detected by both techniques were similar for temperature, humidity, and vertical velocity at heights of 3, 5, and 9.4 m. Significant discrepancies were found among the conditional averaged structures detected by both techniques for zonal and meridional components of the wind at 11.5 m. Considering both techniques, it was observed that the averaged coherent-structure duration ranged from 23.7 ± 0.5 s to 37.8 ± 3.0 s. Furthermore, the averaged number of events per 20-minute period ranged from 20.0 ± 1.0 to 28.5 ± 1.1, and the averaged intermittency factor from 45.0 ± 0.4% to 59.1 ± 1.3%. It was also observed that the averaged duration of the ramplike coherent structures increases with height, while their intensity, number, and intermittency factor decrease. Despite the good matching obtained for temperature and humidity, the coherent-structure properties did not show the expected variation with wind speed, stability parameter, and friction velocity. The Kolmogorov–Smirnov test indicated that the intermittent function and the wavelet transform did not detect coherent structures belonging to the same population. pt_BR
dc.language.iso eng pt_BR
dc.rights restrict access pt_BR
dc.subject Atmospheric turbulence pt_BR
dc.subject Coherent structures pt_BR
dc.subject Conditional sampling pt_BR
dc.subject Surface layer pt_BR
dc.subject Intermittency pt_BR
dc.subject Wavelet transform pt_BR
dc.title Characterization of coherent structures in the atmospheric surface layer pt_BR
dc.type article pt_BR
dc.identifier.doi 10.1023/A:1026096805679 pt_BR


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