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Sökning: id:"swepub:oai:DiVA.org:kth-320550" > Modelling impacts o...

Modelling impacts of lateral N flows and seasonal warming on an arctic footslope ecosystem N budget and N2O emissions based on species-level responses

Rasmussen, L. H. (författare)
University of Copenhagen
Zhang, Wenxin (författare)
Lund University,Lunds universitet,BECC: Biodiversity and Ecosystem services in a Changing Climate,Centrum för miljö- och klimatvetenskap (CEC),Naturvetenskapliga fakulteten,MERGE: ModElling the Regional and Global Earth system,Institutionen för naturgeografi och ekosystemvetenskap,Centre for Environmental and Climate Science (CEC),Faculty of Science,Dept of Physical Geography and Ecosystem Science,University of Copenhagen
Ambus, P. (författare)
University of Copenhagen
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Jansson, Per-Erik (författare)
KTH Royal Institute of Technology,KTH,Hållbar utveckling, miljövetenskap och teknik,Department of Geosciences and Natural Resource Management, Center for Permafrost (CENPERM), University of Copenhagen, Øster Voldgade 10, 1350 København K, Copenhagen, Denmark
Kitzler, B. (författare)
Federal Research And Training Centre For Forests, Natural Hazards And Landscape
Elberling, B. (författare)
University of Copenhagen
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 (creator_code:org_t)
2022-02-09
2022
Engelska.
Ingår i: Biogeochemistry. - : Springer Nature. - 0168-2563 .- 1573-515X. ; 158:2, s. 195-213
  • Tidskriftsartikel (refereegranskat)
Abstract Ämnesord
Stäng  
  • Future Arctic tundra primary productivity and vegetation community composition will partly be determined by nitrogen (N) availability in a warmer climate. N mineralization rates are predicted to increase in both winter and summer, but because N demand and –mobility varies across seasons, the fate of mineralized N remains uncertain. N mineralized in winter is released in a “pulse” upon snowmelt and soil thaw, with the potential for lateral redistribution in the landscape. In summer, the release is into an active rhizosphere with high local biological N demand. In this study, we investigated the ecosystem sensitivity to increased lateral N input and near-surface warming, respectively and in combination, with a numerical ecosystem model (CoupModel) parameterized to simulate ecosystem biogeochemistry for a tundra heath ecosystem in West Greenland. Both measurements and model results indicated that plants were poor utilizers of increased early-season lateral N input, indicating that higher winter N mineralization rates may have limited impact on plant growth and carbon (C) sequestration for a hillslope ecosystem. The model further suggested that, although deciduous shrubs were the plant type with overall most lateral N gain, evergreen shrubs appear to have a comparative advantage utilizing early-season N. In contrast, near-surface summer warming increased plant biomass and N uptake, moving N from soil to plant N pools, and offered an advantage to deciduous plants. Neither simulated high lateral N fluxes nor near-surface soil warming suggests that mesic tundra heaths will be important sources of N2O under warmer conditions. Our work highlights how winter and summer warming may play different roles in tundra ecosystem N and C budgets depending on plant community composition.

Ämnesord

NATURVETENSKAP  -- Biologi -- Ekologi (hsv//swe)
NATURAL SCIENCES  -- Biological Sciences -- Ecology (hsv//eng)
NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Klimatforskning (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Climate Research (hsv//eng)

Nyckelord

Arctic tundra
Climate change
CoupModel
Solute transport
Winter N mineralization
biogeochemistry
biomass
community composition
comparative advantage
hillslope
mineralization
nitrogen
nutrient availability
plant community
rhizosphere
snowmelt
tundra
winter
Arctic
Greenland
Arctic tundra
Climate change
CoupModel
Solute transport
Winter N mineralization

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