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Atmospheric Chemistry and Physics An interactive open-access journal of the European Geosciences Union
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The ergodic theorem of stationary random processes is introduced to analyse and verify the ergodicity of atmospheric turbulence measured using the eddy-covariance technique with two sets of field observational data. The results show that the ergodicity of atmospheric turbulence in atmospheric boundary layer is relative not only to the atmospheric stratification but also to the eddy scale of atmospheric turbulence.
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Articles | Volume 15, issue 17
Atmos. Chem. Phys., 15, 9929–9944, 2015
https://doi.org/10.5194/acp-15-9929-2015
Atmos. Chem. Phys., 15, 9929–9944, 2015
https://doi.org/10.5194/acp-15-9929-2015

Research article 04 Sep 2015

Research article | 04 Sep 2015

Ergodicity test of the eddy-covariance technique

J. Chen et al.

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Short summary
The ergodic theorem of stationary random processes is introduced to analyse and verify the ergodicity of atmospheric turbulence measured using the eddy-covariance technique with two sets of field observational data. The results show that the ergodicity of atmospheric turbulence in atmospheric boundary layer is relative not only to the atmospheric stratification but also to the eddy scale of atmospheric turbulence.
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