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000908764 1001_ $$00000-0002-6570-3837$$aTempler, P. H.$$b0$$eCorresponding author
000908764 245__ $$aAtmospheric deposition and precipitation are important predictors of inorganic nitrogen export to streams from forest and grassland watersheds: a large-scale data synthesis
000908764 260__ $$aDordrecht [u.a.]$$bSpringer Science + Business Media B.V.$$c2022
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000908764 520__ $$aPrevious studies have evaluated how changes in atmospheric nitrogen (N) inputs and climate affect stream N concentrations and fluxes, but none have synthesized data from sites around the globe. We identified variables controlling stream inorganic N concentrations and fluxes, and how they have changed, by synthesizing 20 time series ranging from 5 to 51 years of data collected from forest and grassland dominated watersheds across Europe, North America, and East Asia and across four climate types (tropical, temperate, Mediterranean, and boreal) using the International Long-Term Ecological Research Network. We hypothesized that sites with greater atmospheric N deposition have greater stream N export rates, but that climate has taken a stronger role as atmospheric deposition declines in many regions of the globe. We found declining trends in bulk ammonium and nitrate deposition, especially in the longest time-series, with ammonium contributing relatively more to atmospheric N deposition over time. Among sites, there were statistically significant positive relationships between (1) annual rates of precipitation and stream ammonium and nitrate fluxes and (2) annual rates of atmospheric N inputs and stream nitrate concentrations and fluxes. There were no significant relationships between air temperature and stream N export. Our long-term data shows that although N deposition is declining over time, atmospheric N inputs and precipitation remain important predictors for inorganic N exported from forested and grassland watersheds. Overall, we also demonstrate that long-term monitoring provides understanding of ecosystems and biogeochemical cycling that would not be possible with short-term studies alone.
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000908764 7001_ $$0P:(DE-HGF)0$$aHarrison, J. L.$$b1
000908764 7001_ $$0P:(DE-HGF)0$$aPilotto, F.$$b2
000908764 7001_ $$0P:(DE-HGF)0$$aFlores-Díaz, A.$$b3
000908764 7001_ $$0P:(DE-HGF)0$$aHaase, P.$$b4
000908764 7001_ $$0P:(DE-HGF)0$$aMcDowell, W. H.$$b5
000908764 7001_ $$0P:(DE-HGF)0$$aSharif, R.$$b6
000908764 7001_ $$0P:(DE-HGF)0$$aShibata, H.$$b7
000908764 7001_ $$0P:(DE-HGF)0$$aBlankman, D.$$b8
000908764 7001_ $$0P:(DE-HGF)0$$aAvila, A.$$b9
000908764 7001_ $$0P:(DE-HGF)0$$aBaatar, U.$$b10
000908764 7001_ $$0P:(DE-Juel1)129440$$aBogena, Heye$$b11
000908764 7001_ $$0P:(DE-HGF)0$$aBourgeois, I.$$b12
000908764 7001_ $$0P:(DE-HGF)0$$aCampbell, J.$$b13
000908764 7001_ $$0P:(DE-HGF)0$$aDirnböck, T.$$b14
000908764 7001_ $$0P:(DE-HGF)0$$aDodds, W. K.$$b15
000908764 7001_ $$0P:(DE-HGF)0$$aHauken, M.$$b16
000908764 7001_ $$0P:(DE-HGF)0$$aKokorite, I.$$b17
000908764 7001_ $$0P:(DE-HGF)0$$aLajtha, K.$$b18
000908764 7001_ $$0P:(DE-HGF)0$$aLai, I.-L.$$b19
000908764 7001_ $$0P:(DE-HGF)0$$aLaudon, H.$$b20
000908764 7001_ $$0P:(DE-Juel1)162420$$aLin, T. C.$$b21
000908764 7001_ $$0P:(DE-HGF)0$$aLins, S. R. M.$$b22
000908764 7001_ $$0P:(DE-HGF)0$$aMeesenburg, H.$$b23
000908764 7001_ $$0P:(DE-HGF)0$$aPinho, P.$$b24
000908764 7001_ $$0P:(DE-HGF)0$$aRobison, A.$$b25
000908764 7001_ $$0P:(DE-HGF)0$$aRogora, M.$$b26
000908764 7001_ $$0P:(DE-HGF)0$$aScheler, B.$$b27
000908764 7001_ $$0P:(DE-HGF)0$$aSchleppi, P.$$b28
000908764 7001_ $$0P:(DE-HGF)0$$aSommaruga, R.$$b29
000908764 7001_ $$0P:(DE-HGF)0$$aStaszewski, T.$$b30
000908764 7001_ $$0P:(DE-HGF)0$$aTaka, M.$$b31
000908764 773__ $$0PERI:(DE-600)1478541-9$$a10.1007/s10533-022-00951-7$$p23$$tBiogeochemistry$$v1$$x0168-2563$$y2022
000908764 8564_ $$uhttps://juser.fz-juelich.de/record/908764/files/Templer%20et%20al_Biogeochemistry_Proofs.pdf$$yOpenAccess
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