2005
DOI: 10.1016/j.agrformet.2004.11.006
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Objective threshold determination for nighttime eddy flux filtering

Abstract: We recommend an automated statistical method (Moving Point Test, or MPT) to determine the friction velocity (u * ) thresholds in nighttime eddy flux filtering. Our intention is to make the determination of the u * thresholds objective and reproducible and to keep flux treatment consistent over time and across sites. In developing the MPT method, we recognize that both ecosystem respiration and u * exhibit diurnal and seasonal cycles and there are potential correlative changes between them, which must be remove… Show more

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Cited by 258 publications
(203 citation statements)
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“…Daytime was defined when PPFD > 10 μmol m À2 s À1 . Data corresponding to u * < 0.2 m s À1 (threshold determined using the method of Gu et al [2005]) were not included. To limit outliers, g c outside the range 0-300 mmol m À2 s À1 , PET outside the range À10 to 60 mmol m À2 s À1 , or gap-filled PPFD were not included.…”
Section: Discussionmentioning
confidence: 99%
“…Daytime was defined when PPFD > 10 μmol m À2 s À1 . Data corresponding to u * < 0.2 m s À1 (threshold determined using the method of Gu et al [2005]) were not included. To limit outliers, g c outside the range 0-300 mmol m À2 s À1 , PET outside the range À10 to 60 mmol m À2 s À1 , or gap-filled PPFD were not included.…”
Section: Discussionmentioning
confidence: 99%
“…The data set was then separated into day-and nighttime runs. The CO 2 surface fluxes at night were subjected to a moving-point-threshold (MPT) test, similar to that of Gu et al (2005). The purpose of this test was to determine whether undetectable advection below the measurement height in the stable nocturnal surface layer would lead to biased flux estimates, as has been found at a majority of EC sites (Gu et al, 2005;Barr et al, 2013).…”
Section: Moving-point Threshold Detectionmentioning
confidence: 99%
“…The CO 2 surface fluxes at night were subjected to a moving-point-threshold (MPT) test, similar to that of Gu et al (2005). The purpose of this test was to determine whether undetectable advection below the measurement height in the stable nocturnal surface layer would lead to biased flux estimates, as has been found at a majority of EC sites (Gu et al, 2005;Barr et al, 2013). This procedure was performed twice for each site: once with u * as the sorting parameter, as is common practice, and once with the standard deviation of vertical wind (σ w ), as suggested by Acevedo et al (2009) cause σ w is a more direct indicator of turbulence intensity and less likely to be contaminated by low-frequency motion in the boundary layer.…”
Section: Moving-point Threshold Detectionmentioning
confidence: 99%
“…Similar conditions should present problems for Bowen ratio measurements as well, especially owing to the two different sampling heights. Following a methodology similar to Gu et al (2005), we computed the average night-time CO 2 flux over increasing values of wind speed thresholds using several ten-day periods when soil moisture and temperature were fairly uniform and night-time respiration was expected to be constant. Wind speed was used as a surrogate for turbulent intensity since the commonly used friction velocity (u Ł ) was not quantified by the Bowen ratio system.…”
Section: Calculationsmentioning
confidence: 99%