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A stochastic model for the polygonal tundra based on Poisson-Voronoi diagrams

Aleina, F. C. (author)
Max Planck Gesellschaft zur Förderung der Wissenschaften e.V. (MPG),Max Planck Society for the Advancement of Science (MPG)
Brovkin, V. (author)
Max Planck Gesellschaft zur Förderung der Wissenschaften e.V. (MPG),Max Planck Society for the Advancement of Science (MPG)
Muster, S. (author)
Helmholtz Zentrum,Helmholtz Center
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Boike, J. (author)
Helmholtz Zentrum,Helmholtz Center
Kutzbach, L. (author)
Universität Hamburg,University of Hamburg
Sachs, T. (author)
Deutsches GeoForschungsZentrum (GFZ),German Research Centre for Geosciences (GFZ)
Zuyev, Sergei, 1962 (author)
Gothenburg University,Göteborgs universitet,Institutionen för matematiska vetenskaper, matematisk statistik,Department of Mathematical Sciences, Mathematical Statistics,Chalmers tekniska högskola,Chalmers University of Technology,University of Gothenburg
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Max Planck Gesellschaft zur Förderung der Wissenschaften eV. (MPG) Helmholtz Zentrum (creator_code:org_t)
2013-07-11
2013
English.
In: Earth System Dynamics. - : Copernicus GmbH. - 2190-4979 .- 2190-4987. ; 4:2, s. 187-198
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Subgrid processes occur in various ecosystems and landscapes but, because of their small scale, they are not represented or poorly parameterized in climate models. These local heterogeneities are often important or even fundamental for energy and carbon balances. This is especially true for northern peatlands and in particular for the polygonal tundra, where methane emissions are strongly influenced by spatial soil heterogeneities. We present a stochastic model for the surface topography of polygonal tundra using Poisson-Voronoi diagrams and we compare the results with available recent field studies. We analyze seasonal dynamics of water table variations and the landscape response under different scenarios of precipitation income. We upscale methane fluxes by using a simple idealized model for methane emission. Hydraulic interconnectivities and large-scale drainage may also be investigated through percolation properties and thresholds in the Voronoi graph. The model captures the main statistical characteristics of the landscape topography, such as polygon area and surface properties as well as the water balance. This approach enables us to statistically relate large-scale properties of the system to the main small-scale processes within the single polygons.

Subject headings

NATURVETENSKAP  -- Matematik (hsv//swe)
NATURAL SCIENCES  -- Mathematics (hsv//eng)

Keyword

DERIVE METHANE EMISSIONS
SURFACE-ENERGY BALANCE
NORTHERN SIBERIA
NATURAL WETLANDS
CLIMATE-CHANGE
VEGETATION
WATER
ECOSYSTEMS
ATMOSPHERE
FEEDBACKS
ATMOSPHERE

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ref (subject category)
art (subject category)

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