Перейти к основному содержанию
AkademIndex

Продукты

Для разработчиков

AkademBaseОткрытый API экосистемы
Статья

Separation of net ecosystem exchange into assimilation and respiration using a light response curve approach: critical issues and global evaluation

Gitta LasslopMax-Planck Institute for Biogeochemistry, Postfach 10 01 64, 07701 Jena, GermanyMarkus ReichsteinMax-Planck Institute for Biogeochemistry, Postfach 10 01 64, 07701 Jena, GermanyDario PapaleDepartment of Forest Environment and Resources, DISAFRI, University of Tuscia, Viterbo, ItalyAndrew D. RichardsonHarvard University, Department of Organismic and Evolutionary Biology, Cambridge, MA 02138, USAAlmut ArnethDepartment of Physical Geography and Ecosystems Analysis, Geobiosphere Science, Centre, Lund University Sölvegatan 12, 223 62 Lund, SwedenAlan BarrClimate Research Division, Environment Canada, 11 Innovation Blvd., Saskatoon, SK, CanadaPaul C. StoySchool of GeoSciences, University of Edinburgh, Edinburgh EH9 3JN, UKGeorg WohlfahrtInstitute of Ecology, University of Innsbruck, Sternwartestraße 15, 6020 Innsbruck, Austria
2009en
ABI

Аннотация

Abstract The measured net ecosystem exchange (NEE) of CO 2 between the ecosystem and the atmosphere reflects the balance between gross CO 2 assimilation [gross primary production (GPP)] and ecosystem respiration (R eco ). For understanding the mechanistic responses of ecosystem processes to environmental change it is important to separate these two flux components. Two approaches are conventionally used: (1) respiration measurements made at night are extrapolated to the daytime or (2) light–response curves are fit to daytime NEE measurements and respiration is estimated from the intercept of the ordinate, which avoids the use of potentially problematic nighttime data. We demonstrate that this approach is subject to biases if the effect of vapor pressure deficit (VPD) modifying the light response is not included. We introduce an algorithm for NEE partitioning that uses a hyperbolic light response curve fit to daytime NEE, modified to account for the temperature sensitivity of respiration and the VPD limitation of photosynthesis. Including the VPD dependency strongly improved the model's ability to reproduce the asymmetric diurnal cycle during periods with high VPD, and enhances the reliability of R eco estimates given that the reduction of GPP by VPD may be otherwise incorrectly attributed to higher R eco . Results from this improved algorithm are compared against estimates based on the conventional nighttime approach. The comparison demonstrates that the uncertainty arising from systematic errors dominates the overall uncertainty of annual sums (median absolute deviation of GPP: 47 g C m −2 yr −1 ), while errors arising from the random error (median absolute deviation: ∼2 g C m −2 yr −1 ) are negligible. Despite site‐specific differences between the methods, overall patterns remain robust, adding confidence to statistical studies based on the FLUXNET database. In particular, we show that the strong correlation between GPP and R eco is not spurious but holds true when quasi‐independent, i.e. daytime and nighttime based estimates are compared.

Перевод пока недоступен

Идентификаторы

Цитирования и источники

Цитирований: 3Использованных источников: 0