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首页> 外文期刊>Izvestiya Atmospheric and Oceanic Physics >Temperature Fluctuations in the Atmospheric Surface Layer over the Thermally Inhomogeneous Underlying Surface
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Temperature Fluctuations in the Atmospheric Surface Layer over the Thermally Inhomogeneous Underlying Surface

机译:热非均质下垫面大气表层的温度波动

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摘要

The influence of both spatial and temporal temperature inhomogeneities of the underlying surface on the temperature field in an unstably stratified atmospheric surface layer is considered.The methods of correlation and spectral analyses are proposed to estimate statistical characteristics of surface-air temperature fluctuations caused by both turbulent mixing and inhomogeneities in the temperature of the underlying surface.Analysis of experimental data obtained from measurements in the atmospheric surface layer yields estimates for the contribution made by the time-dependent thermal properties of the underlying surface to the total variance of air-temperature fluctuations.It is shown that the additional air-temperature fluctuations generated by surface-temperature inhomogeneities and unrelated to shear flow may reach 70% and 30% of the total variance of measured fluctuations under variable cloudiness and clear skies,respectively.For the height z = 2 m within the wave-number range 2 x 10~(-3) rad m~(-1) < k < 0.1 rad m~(-1),the contribution made by a spatial surface-temperature inhomogeneity to the variance of air-temperature fluctuations does not exceed 10% of the total variance.Correlation and spectral analyses of experimental data make it possible to isolate the spectra of properly turbulent fluctuations from the measured fluctuations and thus to obtain more accurate values of the universal function of similarity theory for temperature in the range of small wave numbers beyond the inertial range.
机译:考虑了地表表面时空温度不均匀性对不稳定地层大气表层温度场的影响,提出了相关和频谱分析的方法来估算湍流引起的地表温度波动的统计特征。从大气表面层的测量获得的实验数据的分析得出的估算值是由底层表面随时间变化的热性质对空气温度波动的总方差的贡献估计的。结果表明,在变高的云层和晴朗的天空下,由表面温度不均匀性产生的与剪切流无关的额外气温波动可能分别达到所测得波动总变化的70%和30%。对于高度z = 2 m在波数范围2 x 1之内0〜(-3)rad m〜(-1)

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