The high-frequency response correction of eddy covariance fluxes - Part 1 : An experimental approach and its interdependence with the time-lag estimation

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http://hdl.handle.net/10138/333827

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Peltola , O , Aslan , T , Ibrom , A , Nemitz , E , Rannik , U & Mammarella , I 2021 , ' The high-frequency response correction of eddy covariance fluxes - Part 1 : An experimental approach and its interdependence with the time-lag estimation ' , Atmospheric Measurement Techniques , vol. 14 , no. 7 , pp. 5071-5088 . https://doi.org/10.5194/amt-14-5071-2021

Julkaisun nimi: The high-frequency response correction of eddy covariance fluxes - Part 1 : An experimental approach and its interdependence with the time-lag estimation
Tekijä: Peltola, Olli; Aslan, Toprak; Ibrom, Andreas; Nemitz, Eiko; Rannik, Ullar; Mammarella, Ivan
Tekijän organisaatio: Institute for Atmospheric and Earth System Research (INAR)
Micrometeorology and biogeochemical cycles
Päiväys: 2021-07-28
Kieli: eng
Sivumäärä: 18
Kuuluu julkaisusarjaan: Atmospheric Measurement Techniques
ISSN: 1867-1381
DOI-tunniste: https://doi.org/10.5194/amt-14-5071-2021
URI: http://hdl.handle.net/10138/333827
Tiivistelmä: The eddy covariance (EC) technique has emerged as the prevailing method to observe the ecosystem- atmosphere exchange of gases, heat and momentum. EC measurements require rigorous data processing to derive the fluxes that can be used to analyse exchange processes at the ecosystem-atmosphere interface. Here we show that two common post-processing steps (time-lag estimation via cross-covariance maximisation and correction for limited frequency response of the EC measurement system) are interrelated, and this should be accounted for when processing EC gas flux data. These findings are applicable to EC systems employing closed- or enclosed-path gas analysers which can be approximated to be linear first-order sensors. These EC measurement systems act as low-pass filters on the time series of the scalar chi (e.g. CO2, H2O), and this induces a time lag (t(l)(pf)) between vertical wind speed (omega) and scalar chi time series which is additional to the travel time of the gas signal in the sampling line (tube, filters). Time-lag estimation via cross-covariance maximisation inadvertently accounts also for t(l)(pf) and hence overestimates the travel time in the sampling line. This results in a phase shift between the time series of omega and chi, which distorts the measured cospectra between omega and chi and hence has an effect on the correction for the dampening of the EC flux signal at high frequencies. This distortion can be described with a transfer function related to the phase shift (H-p) which is typically neglected when processing EC flux data. Based on analyses using EC data from two contrasting measurement sites, we show that the low-pass-filtering-induced time lag increases approximately linearly with the time constant of the low-pass filter, and hence the importance of H-p in describing the high-frequency flux loss increases as well. Incomplete description of these processes in EC data processing algorithms results in flux biases of up to 10 %, with the largest biases observed for short towers due to the prevalence of small-scale turbulence. Based on these findings, it is suggested that spectral correction methods implemented in EC data processing algorithms are revised to account for the influence of low-pass-filtering-induced time lag.
Avainsanat: 114 Physical sciences
Vertaisarvioitu: Kyllä
Tekijänoikeustiedot: cc_by
Pääsyrajoitteet: openAccess
Rinnakkaistallennettu versio: publishedVersion


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