4.7 Article

Multivariable evaluation of land surface processes in forced and coupled modes reveals new error sources to the simulated water cycle in the IPSL (Institute Pierre Simon Laplace) climate model

Journal

HYDROLOGY AND EARTH SYSTEM SCIENCES
Volume 25, Issue 4, Pages 2199-2221

Publisher

COPERNICUS GESELLSCHAFT MBH
DOI: 10.5194/hess-25-2199-2021

Keywords

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Funding

  1. Japan Society for the Promotion of Science (JSPS KAKENHI) [16J00783]
  2. Centre national d'etudes spatiales (CNES
  3. under the program Terre Ocean Surfaces Continentales et Atmosphere)
  4. CNRS, Sorbonne Universite, Ecole Polytechnique
  5. CNES
  6. CMIP6 project at IPSL by GENCI (Grand equipement national de calcul intensif) [2016-A0030107732, 2017-R0040110492, 2018-R0040110492]
  7. Grants-in-Aid for Scientific Research [16J00783] Funding Source: KAKEN

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This study evaluates land surface models using different simulations to understand the errors and uncertainties within the models. Results show that the model performs well in representing spatiotemporal patterns, but there are uncertainties related to landscape and meteorological factors, especially in coupled mode simulations. The biases are amplified in the coupled mode, indicating a strong link between irrigation-precipitation and complex link between precipitation-evapotranspiration.
Evaluating land surface models (LSMs) using available observations is important for understanding the potential and limitations of current Earth system models in simulating water- and carbon-related variables. To reveal the error sources of a LSM, five essential climate variables have been evaluated in this paper (i.e., surface soil moisture, evapotranspiration, leaf area index, surface albedo, and precipitation) via simulations with the IPSL (Institute Pierre Simon Laplace) LSM ORCHIDEE (Organizing Carbon and Hydrology in Dynamic Ecosystems) model, particularly focusing on the difference between (i) forced simulations with atmospheric forcing data (WATCH Forcing Data ERA-Interim - WFDEI) and (ii) coupled simulations with the IPSL atmospheric general circulation model. Results from statistical evaluation, using satellite- and ground-based reference data, show that ORCHIDEE is well equipped to represent spatiotemporal patterns of all variables in general. However, further analysis against various landscape and mete-orological factors (e.g., plant functional type, slope, precipitation, and irrigation) suggests potential uncertainty relating to freezing and/or snowmelt, temperate plant phenology, irrigation, and contrasted responses between forced and coupled mode simulations. The biases in the simulated variables are amplified in the coupled mode via surfaceatmosphere interactions, indicating a strong link between irrigation-precipitation and a relatively complex link between precipitation-evapotranspiration that reflects the hydrometeorological regime of the region (energy limited or water limited) and snow albedo feedback in mountainous and boreal regions. The different results between forced and coupled modes imply the importance of model evaluation under both modes to isolate potential sources of uncertainty in the model.

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