dc.contributor.author
Graaf, S. C. van der
dc.contributor.author
Janssen, T. A. J.
dc.contributor.author
Erisman, J. W.
dc.contributor.author
Schaap, Martijn
dc.date.accessioned
2022-01-11T09:38:55Z
dc.date.available
2022-01-11T09:38:55Z
dc.identifier.uri
https://refubium.fu-berlin.de/handle/fub188/33434
dc.identifier.uri
http://dx.doi.org/10.17169/refubium-33155
dc.description.abstract
Atmospheric reactive nitrogen (N) deposition is an important driver of carbon (C) sequestration in forest ecosystems. Previous studies have focused on N-C interactions in various ecosystems; however, relatively little is known about the impact of N deposition on ecosystem C cycling during climate extremes such as droughts. With the occurrence and severity of droughts likely to be exacerbated by climate change, N deposition—drought interactions remain one of the key uncertainties in process-based models to date. This study aims to contribute to the understanding of N deposition-drought dynamics on gross primary production (GPP) in European forest ecosystems. To do so, different soil water availability indicators (Standardized Precipitation Evapotranspiration Index (SPEI), soil volumetric water) and GPP measurements from European FLUXNET forest sites were used to quantify the response of forest GPP to drought. The computed drought responses of the forest GPP to drought were linked to modelled N deposition estimates for varying edaphic, physiological, and climatic conditions. Our result showed a differential response of forest ecosystems to the drought indicators. Although all FLUXNET forest sites showed a coherent dependence of GPP on N deposition, no consistent or significant N deposition effect on the response of forest GPP to drought could be isolated. The mean response of forest GPP to drought could be predicted for forests with Pinus trees as dominant species (R2 = 0.85, RMSE = 8.1). After extracting the influence of the most prominent parameters (mean annual temperature and precipitation, forest age), however, the variability remained too large to significantly substantiate hypothesized N deposition effects. These results suggest that, while N deposition clearly affects forest productivity, N deposition is not a major nor consistent driver of forest productivity responses to drought in European forest ecosystems.
en
dc.format.extent
19 Seiten
dc.rights.uri
https://creativecommons.org/licenses/by/4.0/
dc.subject
nitrogen deposition-drought interactions
en
dc.subject
nitrogen deposition
en
dc.subject
European forests
en
dc.subject.ddc
500 Naturwissenschaften und Mathematik::550 Geowissenschaften, Geologie::550 Geowissenschaften
dc.title
Nitrogen deposition shows no consistent negative nor positive effect on the response of forest productivity to drought across European FLUXNET forest sites
dc.type
Wissenschaftlicher Artikel
dcterms.bibliographicCitation.articlenumber
125003
dcterms.bibliographicCitation.doi
10.1088/2515-7620/ac2b7d
dcterms.bibliographicCitation.journaltitle
Environmental Research Communications
dcterms.bibliographicCitation.number
12
dcterms.bibliographicCitation.volume
3
dcterms.bibliographicCitation.url
https://doi.org/10.1088/2515-7620/ac2b7d
refubium.affiliation
Geowissenschaften
refubium.affiliation.other
Institut für Meteorologie
refubium.resourceType.isindependentpub
no
dcterms.accessRights.openaire
open access
dcterms.isPartOf.eissn
2515-7620
refubium.resourceType.provider
WoS-Alert