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Apparent winter CO2 uptake by a boreal forest due to decoupling.

Authors :
Jocher, Georg
Ottosson Löfvenius, Mikaell
De Simon, Giuseppe
Hörnlund, Thomas
Linder, Sune
Lundmark, Tomas
Marshall, John
Nilsson, Mats B.
Näsholm, Torgny
Tarvainen, Lasse
Öquist, Mats
Peichl, Matthias
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