Monitoring boreal forest biomass and carbon storage change by integrating airborne laser scanning, biometry and eddy covariance data

REMOTE SENSING OF ENVIRONMENT

卷:181

Article

Hopkinson, C.¹  Chasmer, L.¹  Barr, A. G.²  Kljun, N.³  Black, T. A.^4,5  McCaughey, J. H.⁶ 

[1] Univ Lethbridge, Dept Geog, Lethbridge, AB T1K 3M4, Canada

[2] Environm Canada, 11 Innovat Blvd, Saskatoon, SK S7N 3H5, Canada

[3] Swansea Univ, Dept Geog, Swansea, W Glam, Wales

[4] Univ British Columbia, Dept Appl Biol, Vancouver, BC V6T 1Z4, Canada

[5] Univ British Columbia, Dept Soil Sci, Vancouver, BC V6T 1Z4, Canada

[6] Queens Univ, Dept Geog, Kingston, ON K7L 3N6, Canada

关键词: Net ecosystem production (NEP);    Gross primary production (GPP);    Stand growth;    Change detection;    Airborne laser scanning;    Multi-temporal LiDAR;    Jack pine chronosequence;    Boreal forest;    Carbon balance;    Monitoring framework;   

DOI  :  10.1016/j.rse.2016.04.010

来源: Elsevier

【 摘 要 】

This study presents a comparison and integration of three methods commonly used to estimate the amount of forest ecosystem carbon (C) available for storage. In particular, we examine the representation of living above and below-ground biomass change (net accumulation) using plot-level biometry and repeat airborne laser scanning (ALS) of three dimensional forest plot structure. These are compared with cumulative net CO2 fluxes (net ecosystem production, NEP) from eddy covariance (EC) over a six-year period within a jack pine chronosequence of four stands (similar to 94, 30, 14 and 3 years since establishment from 2005) located in central Saskatchewan, Canada. Combining the results of the two methods yield valuable observations on the partitioning of C within ecosystems. Subtracting total living biomass C accumulation from NEP results in a residual that represents change in soil and litter C storage. When plotted against time for the stands investigated, the curve produced is analogous to the soil C dynamics described in Covington (1981). Here, ALS biomass accumulation exceeds EC-based NEP measured in young stands, with the residual declining with age as stands regenerate and litter decomposition stabilizes. During the 50-70 year age-period, NEP and live biomass accumulation come into balance, with the soil and litter pools of stands 70-100 years post-disturbance becoming a net store of C. Biomass accumulation was greater in 2008-2011 compared to 2005-2008, with the smallest increase in the 94-year-old old jack pine stand and greatest in the 14-year-old harvested jack pine 1994 stand, with values of 1.4 (+/- 3.2) tC ha(-1) and 12.0 (+/- 1.6) tC ha(-1), respectively. The efficiency with which CO2 was stored in accumulated biomass was lowest in the youngest and oldest stands, but peaked during rapid regeneration following harvest (14-year-old stand). The analysis highlights that the primary source of uncertainty in the data integration workflow is in the calculation of biomass expansion factors, and this aspect of the workflow needs to be implemented with caution to avoid large error propagations. We suggest that the adoption of integrated ALS, in situ and atmospheric flux monitoring frameworks is needed to improve spatio-temporal partitioning of C balance components at sub-decadal scale within rapidly changing forest ecosystems and for use in national carbon accounting programs. (C) 2016 The Authors. Published by Elsevier Inc.

【 授权许可】

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