Information for the model LPJ-GUESS is provided for the simulation rounds shown in the tabs below. Click on the appropriate tab to get the information for the simulation round you are interested in.
The model is the crop-enabled version of LPJ-GUESS, described in Lindeskog et al. (2013). It is loosely based on LPJmL as described in Bondeau et al. (2007), but differs in several important aspects, including not being calibrated to observed country-level yields, a new phenology scheme, and a dynamic calculation of the potential heat units (PHU) required for a crop to achieve maturity. Sowing dates are calculated dynamically following Waha et al. (2012). The PHU sum needed for full development of a crop in a particular grid cell is calculated using a 10-year running mean of heat unit sums accumulated from the sowing date to the end of a sampling period (ranging from 190 to 245 days) derived from default sowing and harvest limit dates (Lindeskog et al., 2013). Crops are harvested upon full development. This dynamic variation of PHU to climate effectively assumes a perfect adaptation of crop cultivar to the prevailing climate. N limitation is not explicitly accounted for in this version of the model.
Bondeau, A. et al. Modelling the role of agriculture for the 20th century global terrestrial carbon balance. Glob. Change Biol. 13, 679-706, doi:10.1111/j.1365-2486.2006.01305.x (2007).
Lindeskog, M. et al. Implications of accounting for land use in simulations of carbon cycling in Africa. Earth System Dynamics 4, 385-407, doi:10.5194/esd-4-385-2013 (2013).
Waha, K., et al. Climate-driven simulation of global crop sowing dates. Global Ecology and Biogeography 21, 247-259 (2012).
Information for the model LPJ-GUESS is provided for the simulation rounds shown in the tabs below. Click on the appropriate tab to get the information for the simulation round you are interested in.