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WeightNameValue
1000 Titel
  • Simulating net ecosystem exchange under seasonal snow cover at an Arctic tundra site
1000 Autor/in
  1. Dutch, Victoria R. |
  2. Rutter, Nick |
  3. Wake, Leanne |
  4. Sonnentag, Oliver |
  5. Hould Gosselin, Gabriel |
  6. Sandells, Melody |
  7. Derksen, Chris |
  8. Walker, Branden |
  9. Meyer, Gesa |
  10. Essery, Richard |
  11. Kelly, Richard |
  12. Marsh, Phillip |
  13. Boike, Julia |
  14. Detto, Matteo |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-02-15
1000 Erschienen in
1000 Quellenangabe
  • 21(3):825-841
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/bg-21-825-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Estimates of winter (snow-covered non-growing season) CO2 fluxes across the Arctic region vary by a factor of 3.5, with considerable variation between measured and simulated fluxes. Measurements of snow properties, soil temperatures, and net ecosystem exchange (NEE) at Trail Valley Creek, NWT, Canada, allowed for the evaluation of simulated winter NEE in a tundra environment with the Community Land Model (CLM5.0). Default CLM5.0 parameterisations did not adequately simulate winter NEE in this tundra environment, with near-zero NEE (&lt; 0.01 gCm-2d-1) simulated between November and mid-May. In contrast, measured NEE was broadly positive (indicating net CO2 release) from snow-cover onset until late April. Changes to the parameterisation of snow thermal conductivity, required to correct for a cold soil temperature bias, reduced the duration for which no NEE was simulated. Parameter sensitivity analysis revealed the critical role of the minimum soil moisture threshold of decomposition (Ψmin) in regulating winter soil respiration. The default value of this parameter (Ψmin) was too high, preventing simulation of soil respiration for the vast majority of the snow-covered season. In addition, the default rate of change of soil respiration with temperature (Q10) was too low, further contributing to poor model performance during winter. As Ψmin and Q10 had opposing effects on the magnitude of simulated winter soil respiration, larger negative values of Ψmin and larger positive values of Q10 are required to simulate wintertime NEE more adequately. </jats:p>
1000 Liste der Beteiligten
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1000 Förderer
  1. Natural Environment Research Council |
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1000 Dateien
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    1000 Förderer Natural Environment Research Council |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 @id frl:6482109.rdf
1000 Erstellt am 2024-05-24T02:57:41.251+0200
1000 Erstellt von 322
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1000 Zuletzt bearbeitet Mon May 27 10:56:16 CEST 2024
1000 Objekt bearb. Mon May 27 10:56:16 CEST 2024
1000 Vgl. frl:6482109
1000 Oai Id
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