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Apparent winter CO2 uptake by a boreal forest due to decoupling.
- Source :
-
Agricultural & Forest Meteorology . Jan2017, Vol. 232, p23-34. 12p. - Publication Year :
- 2017
-
Abstract
- Net uptake of carbon dioxide (CO 2 ) was observed during the winter when using the eddy covariance (EC) technique above a ∼90-year-old Scots pine ( Pinus sylvestris L.) stand in northern Sweden. This uptake occurred despite photosynthetic dormancy. This discrepancy led us to investigate the potential impact of decoupling of below- and above-canopy air mass flow and accompanying below-canopy horizontal advection on these measurements. We used the correlation of above- and below-canopy standard deviation of vertical wind speed (σ w ), derived from EC measurements above and below the canopy, as the main mixing criterion. We identified 0.33 m s −1 and 0.06 m s −1 as site-specific σ w thresholds for above and below canopy, respectively, to reach the fully coupled state. Decoupling was observed in 45% of all cases during the measurement period (5.11.2014–25.2.2015). After filtering out decoupled periods the above-canopy mean winter NEE shifted from −0.52 μmol m −2 s −1 to a more reasonable positive value of 0.31 μmol m −2 s −1 . None of the above-canopy data filtering criteria we tested (i.e., friction velocity threshold; horizontal wind speed threshold; single-level σ w threshold) ensured sufficient mixing. All missed critical periods that were detected only by the two-level filtering approach. Tower-surrounding topography induced a predominant below-canopy wind direction and consequent wind shear between above- and below-canopy air masses. These processes may foster decoupling and below-canopy removal of CO 2 rich air. To determine how broadly such a topographical influence might apply, we compared the topography surrounding our tower to that surrounding other forest flux sites worldwide. Medians of maximum elevation differences within 300 m and 1000 m around 110 FLUXNET forest EC towers were 24 m and 66 m, respectively, compared to 24 m and 114 m, respectively, at our site. Consequently, below-canopy flow may influence above-canopy NEE detections at many forested EC sites. Based on our findings we suggest below-canopy measurements as standard procedure at sites evaluating forest CO 2 budgets. [ABSTRACT FROM AUTHOR]
Details
- Language :
- English
- ISSN :
- 01681923
- Volume :
- 232
- Database :
- Academic Search Index
- Journal :
- Agricultural & Forest Meteorology
- Publication Type :
- Academic Journal
- Accession number :
- 119651322
- Full Text :
- https://doi.org/10.1016/j.agrformet.2016.08.002