Thinning turned boreal forest to a temporary carbon source- short term effects of partial harvest on carbon dioxide and water vapor fluxes

被引:0
|
作者
Aslan, Toprak [1 ,4 ]
Launiainen, Samuli [2 ]
Kolari, Pasi [1 ]
Peltola, Olli [2 ]
Aalto, Juho [3 ]
Back, Jaana [3 ]
Vesala, Timo [1 ,3 ]
Mammarella, Ivan [1 ]
机构
[1] Inst Atmospher & Earth Syst Res INAR Phys, Fac Sci, POB 64, Helsinki 00014, Finland
[2] Nat Resources Inst Finland Luke, Latokartanonkaari 9, Helsinki 00790, Finland
[3] Inst Atmospher & Earth Syst Res INAR, Forest Sci, POB 27, Helsinki 00014, Finland
[4] Finnish Meteorol Inst, POB 503, Helsinki 00101, Finland
关键词
Eddy covariance; Net ecosystem exchange; Even-aged forestry; Thinning; Boreal forest; TEMPERATE MIXED FOREST; EDDY COVARIANCE; CLIMATE-CHANGE; NORWAY SPRUCE; CO2; EXCHANGE; PINE FORESTS; SCOTS PINE; VEGETATION; CANOPY; TRANSPIRATION;
D O I
10.1016/j.agrformet.2024.110061
中图分类号
S3 [农学(农艺学)];
学科分类号
0901 ;
摘要
Even though the effect of thinning on CO 2 and H 2 O fluxes has been widely investigated, a holistic description of thinning -induced responses is yet to be provided. Here, we present a comprehensive study, investigating the impact of commercial thinning in an even -aged boreal forest in southern Finland using concurrent aboveand sub -canopy eddy -covariance measurements and a process -based ecosystem model. The thinning was done from below and removed ca. 40% of the basal area. The forest turned from a strong sink ( - 271 gCm -2 yr -1 ) to a moderate carbon source (+115 gCm -2 yr -1 ) during the year of thinning due to decreased ecosystem gross primary productivity (GPP eco ) and simultaneous increase in ecosystem respiration (R eco ). The reduced canopy density increased the light availability, near -ground air temperature and wind speed. This improved the photosynthetic efficiency of the remaining trees, resulting in only a moderate reduction in GPP eco (ca. 20%) compared to the foliage loss (ca. 45%). The decomposition of cutting residue likely increased the heterotrophic respiration that compensated for the reduced autotrophic respiration of removed trees, leading to R eco exceeding long-term average by ca. 10% during the year of thinning. Interestingly, thinning did not affect ecosystem evapotranspiration but changed its partitioning: both stand transpiration and interception evaporation decreased, whereas forest floor evapotranspiration increased. The inter -annual weather variability did not notably affect annual fluxes, which enabled robust quantification of thinning impacts. Our results show a strong qualitative resemblance with previously reported short-term responses of boreal forest to thinning. This is presumably due to similar management practices and species composition among the studies, and low variability of inter -annual weather and fluxes. Our study showed that sub -canopy eddy covariance measurements and process -based model can play a pivotal role in disentangling the confounding responses of forest floor and canopy to thinning.
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