User Manual Privacy Policy Disclaimer Contact us
  Advanced SearchBrowse




Journal Article

A multi-layer land surface energy budget model for implicit coupling with global atmospheric simulations


Naudts,  Kim
Laboratoire des Sciences du Climat et de l'Environnement, LSCE/IPSL;
Emmy Noether Junior Research Group Forest Management in the Earth System, The Land in the Earth System, MPI for Meteorology, Max Planck Society;

There are no locators available
Fulltext (public)

(Publisher version), 2MB

Supplementary Material (public)

(Supplementary material), 2MB


Ryder, J., Polcher, J., Peylin, P., Ottle, C., Chen, Y., van Gorsel, E., et al. (2016). A multi-layer land surface energy budget model for implicit coupling with global atmospheric simulations. Geoscientific Model Development, 9, 223-245. doi:10.5194/gmd-9-223-2016.

Cite as: http://hdl.handle.net/21.11116/0000-0000-6170-4
In Earth system modelling, a description of the energy budget of the vegetated surface layer is fundamental as it determines the meteorological conditions in the planetary boundary layer and as such contributes to the atmospheric conditions and its circulation. The energy budget in most Earth system models has been based on a big-leaf approach, with averaging schemes that represent in-canopy processes. Furthermore, to be stable, that is to say, over large time steps and without large iterations, a surface layer model should be capable of implicit coupling to the atmospheric model. Surface models with large time steps, however, have difficulties in reproducing consistently the energy balance in field observations. Here we outline a newly developed numerical model for energy budget simulation, as a component of the land surface model ORCHIDEE-CAN (Organising Carbon and Hydrology In Dynamic Ecosystems - CANopy). This new model implements techniques from single-site canopy models in a practical way. It includes representation of in-canopy transport, a multi-layer long-wave radiation budget, height-specific calculation of aerodynamic and stomatal conductance, and interaction with the bare-soil flux within the canopy space. Significantly, it avoids iterations over the height of the canopy and so maintains implicit coupling to the atmospheric model LMDz (Laboratoire de Meteorologie Dynamique Zoomed model). As a first test, the model is evaluated against data from both an intensive measurement campaign and longer-term eddy-covariance measurements for the intensively studied Eucalyptus stand at Tumbarumba, Australia. The model performs well in replicating both diurnal and annual cycles of energy and water fluxes, as well as the vertical gradients of temperature and of sensible heat fluxes.