Comparing methods for partitioning a decade of carbon dioxide and water vapor fluxes in a temperate forest

•Multiple methods were used to partition CO2 and H2O fluxes from a temperate forest.•Between methods, daytime summer evaporation was 6–18% of evapotranspiration.•Daytime summer respiration was 7–22% of gross primary production.•A method based on flux variance similarity compared well with other meth...

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Veröffentlicht in:Agricultural and forest meteorology 2016-10, Vol.226-227 (C), p.229-245
Hauptverfasser: Sulman, Benjamin N., Roman, D. Tyler, Scanlon, Todd M., Wang, Lixin, Novick, Kimberly A.
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Sprache:eng
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Zusammenfassung:•Multiple methods were used to partition CO2 and H2O fluxes from a temperate forest.•Between methods, daytime summer evaporation was 6–18% of evapotranspiration.•Daytime summer respiration was 7–22% of gross primary production.•A method based on flux variance similarity compared well with other methods.•The flux variance similarity method was sensitive to estimated water use efficiency. The eddy covariance (EC) method is routinely used to measure net ecosystem fluxes of carbon dioxide (CO2) and evapotranspiration (ET) in terrestrial ecosystems. It is often desirable to partition CO2 flux into gross primary production (GPP) and ecosystem respiration (RE), and to partition ET into evaporation and transpiration. We applied multiple partitioning methods, including the recently-developed flux variance similarity (FVS) partitioning method, to a ten-year record of ET and CO2 fluxes measured using EC at Morgan Monroe State Forest, a temperate, deciduous forest located in south-central Indiana, USA. While the FVS method has previously been demonstrated in croplands and grasslands, this is the first evaluation of the method in a forest. CO2 fluxes were partitioned using nonlinear regressions, FVS, and sub-canopy EC measurements. ET was partitioned using FVS and sub-canopy EC measurements, and sub-canopy potential evapotranspiration was calculated as an additional constraint on forest floor evaporation. Leaf gas exchange measurements were used to parameterize a model of water use efficiency (WUE) necessary for the FVS method. Scaled leaf gas exchange measurements also provided additional independent estimates of GPP and transpiration. There was good agreement among partitioning methods for transpiration and GPP, which also agreed well with scaled leaf gas exchange measurements. There was higher variability among methods for RE and evaporation. The sub-canopy flux method yielded lower estimates of evaporation and RE than FVS and lower estimates of RE than the nonlinear regression method, likely due to the exclusion of flux sources within the canopy but above the top of the sub-canopy tower for the sub-canopy flux method. Based on a sensitivity test, FVS flux partitioning was moderately sensitive to errors in WUE values, and underestimates of WUE significantly reduced the rate at which the algorithm was able to produce a physically valid solution. FVS partitioning has unique potential for retroactive ET partitioning at EC sites, because it relies on the same continuous
ISSN:0168-1923
1873-2240
DOI:10.1016/j.agrformet.2016.06.002