Parameter interactions and sensitivity analysis for modelling carbon heat and water fluxes in a natural peatland, using CoupModel v5

被引:17
作者
Metzger, Christine [1 ,3 ]
Nilsson, Mats B. [2 ]
Peichl, Matthias [2 ]
Jansson, Per-Erik [1 ]
机构
[1] Royal Inst Technol, Dept Land & Water Resources Engn, S-10044 Stockholm, Sweden
[2] Swedish Univ Agr Sci, Dept Forest Ecol & Management, S-90183 Umea, Sweden
[3] Karlsruhe Inst Technol, Inst Meteorol & Climate Res Atmospher Environm Re, D-82467 Garmisch Partenkirchen, Germany
基金
瑞典研究理事会;
关键词
BIOME-BGC MODEL; ECOSYSTEM RESPIRATION; ERIOPHORUM-VAGINATUM; NORTHERN PEATLAND; METHANE EMISSIONS; PLANT BIOMASS; MONTE-CARLO; CO2; FLUXES; LIFE-SPAN; UNCERTAINTY;
D O I
10.5194/gmd-9-4313-2016
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In contrast to previous peatland carbon dioxide (CO2) model sensitivity analyses, which usually focussed on only one or a few processes, this study investigates interactions between various biotic and abiotic processes and their parameters by comparing CoupModel v5 results with multiple observation variables. Many interactions were found not only within but also between various process categories simulating plant growth, decomposition, radiation interception, soil temperature, aerodynamic resistance, transpiration, soil hydrology and snow. Each measurement variable was sensitive to up to 10 (out of 54) parameters, from up to 7 different process categories. The constrained parameter ranges varied, depending on the variable and performance index chosen as criteria, and on other calibrated parameters (equifinalities). Therefore, transferring parameter ranges between models needs to be done with caution, especially if such ranges were achieved by only considering a few processes. The identified interactions and constrained parameters will be of great interest to use for comparisons with model results and data from similar ecosystems. All of the available measurement variables (net ecosystem exchange, leaf area index, sensible and latent heat fluxes, net radiation, soil temperatures, water table depth and snow depth) improved the model constraint. If hydraulic properties or water content were measured, further parameters could be constrained, resolving several equifinalities and reducing model uncertainty. The presented results highlight the importance of considering biotic and abiotic processes together and can help modellers and experimentalists to design and calibrate models as well as to direct experimental set-ups in peatland ecosystems towards modelling needs.
引用
收藏
页码:4313 / 4338
页数:26
相关论文
共 129 条
  • [1] Simulation of CO2 and Attribution Analysis at Six European Peatland Sites Using the ECOSSE Model
    Abdalla, M.
    Hastings, A.
    Bell, M. J.
    Smith, J. U.
    Richards, M.
    Nilsson, M. B.
    Peichl, M.
    Lofvenius, M. O.
    Lund, M.
    Helfter, C.
    Nemitz, E.
    Sutton, M. A.
    Aurela, M.
    Lohila, A.
    Laurila, T.
    Dolman, A. J.
    Belelli-Marchesini, L.
    Pogson, M.
    Jones, E.
    Drewer, J.
    Drosler, M.
    Smith, P.
    [J]. WATER AIR AND SOIL POLLUTION, 2014, 225 (11)
  • [2] Alexandersson H., 1991, 81 SMHI
  • [3] [Anonymous], 1981, WATER MOVEMENT MIREL
  • [4] [Anonymous], 1964, HYDROLOGY PAPERS COL
  • [5] Aubinet M, 2000, ADV ECOL RES, V30, P113, DOI 10.1016/S0065-2504(08)60018-5
  • [6] The timing of snow melt controls the annual CO2 balance in a subarctic fen -: art. no. L16119
    Aurela, M
    Laurila, T
    Tuovinen, JP
    [J]. GEOPHYSICAL RESEARCH LETTERS, 2004, 31 (16) : L161191 - 4
  • [7] The DigiBog peatland development model 1: rationale, conceptual model, and hydrological basis
    Baird, Andy J.
    Morris, Paul J.
    Belyea, Lisa R.
    [J]. ECOHYDROLOGY, 2012, 5 (03) : 242 - 255
  • [8] Bazin M. J., 1988, CRC SERIES MATH MODE, V2
  • [9] Modelling forest management within a global vegetation model Part 1: Model structure and general behaviour
    Bellassen, V.
    Le Maire, G.
    Dhote, J. F.
    Ciais, P.
    Viovy, N.
    [J]. ECOLOGICAL MODELLING, 2010, 221 (20) : 2458 - 2474
  • [10] Belyea LR, 2009, GEOPHYS MONOGR SER, V184, P5, DOI 10.1029/2008GM000829