Weather, pollution and biotic factors drive net forest atmosphere exchange of CO2 at different temporal scales in a temperate-zone mixed forest

0532137 - ÚVGZ 2021 RIV NL eng J - Článek v odborném periodiku
Horemans, J. A. - Janssens, I. A. - Gielen, B. - Roland, M. - Deckmyn, G. - Verstraeten, A. - Neirynck, J. - Ceulemans, Reinhart
Weather, pollution and biotic factors drive net forest atmosphere exchange of CO2 at different temporal scales in a temperate-zone mixed forest.
Agricultural and Forest Meteorology. Roč. 291, SEP (2020), č. článku 108059. ISSN 0168-1923. E-ISSN 1873-2240
Institucionální podpora: RVO:86652079
Klíčová slova: gross primary productivity * carbon-dioxide exchange * interannual variability * functional-changes * european forests * fluxes * patterns * climate * trends * respiration * Eddy covariance flux * Random forests * Time series decomposition * Ozone pollution * Carbon
Obor OECD: Agriculture
Impakt faktor: 5.734, rok: 2020
Způsob publikování: Omezený přístup
https://www.sciencedirect.com/science/article/pii/S0168192320301611?via%3Dihub

Understanding the drivers of net ecosystem exchange of carbon (NEE) between forests and the atmosphere is crucial for the prediction of future global carbon dynamics. We therefore analyzed the long-term (1999-2014) ecosystem carbon fluxes of a mixed coniferous/deciduous forest (Brasschaat forest) in the Campine ecoregion of Belgium. The carbon uptake of this forest increased over the 16-year study period. By consecutively performing time series decomposition and the statistical technique of random forests, the correlative strength between multiple meteorological drivers, tropospheric pollutants and biotic indices with NEE was quantified at different time scales: i.e., long-term, seasonal and weekly, and separately for day- and nighttime NEE fluxes. The drivers that were most correlated with the trend in carbon sink capacity were the increasing atmospheric CO2 level and soil recovery from acidification. The radiation-saturated carbon uptake increased remarkably and explained much of the long-term variability of daytime NEE. When the long-term and seasonal variation were extracted the remaining weekly variation in daytime NEE was most strongly correlated with variation in the incoming radiation and cloudiness, and to a lesser extent by variation in vapor pressure deficit. In contrast to daytime NEE, nighttime NEE did not show a steady trend over time, but fluctuated, peaking in 1999 and in 2011. The long-term variability in nighttime NEE was most strongly correlated with the groundwater table depth. Air temperature was highly correlated to the seasonal as well as to the remaining weekly variation, i.e., after removal of the long-term and seasonal variability, in nighttime NEE. Biotic drivers (e.g., quantum yield and radiation saturated carbon uptake) explained less of the variation in NEE on a seasonal and short-term scale, but were more important at the long term.
Trvalý link: http://hdl.handle.net/11104/0310733