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The modeling was initialized and validated by FNL data.
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In this case, the model was initialized with a minimal SOC content, with 3% of the initial SOC considered to be protected microbial biomass and the remaining 97% stable humus.
By default, the mixture model was initialized with 20 components.
The LOEM model was initialized once and run continuously through the simulation period.
Thus, the 3D model was initialized with the proper deformed shape and the current post-riveting stress strain state.
The model was initialized for each location soil type using a 20-year spin-up period to reach stable SOC fractions.
Consequently, the calculation of STOIP improved drastically when the dynamic model was initialized with the newly derived FWL and saturation height equations (modeled from the capillary pressure dataset).
The model was initialized with an axisymmetric cyclonic vortex that had a maximum azimuthal wind of 12 m s−1 as formulated by Rotunno and Emanuel ([1987]).
The model was initialized and calibrated based on landcover maps derived from Landsat-5 Thematic Mapper data acquired in 1986 and 1999 coupled with plant biomass measurements collected in the field during 2000.
The fact that the soil carbon pool of the forest model was initialized with a soil pool in a steady state might lead to an overestimation of ecosystem respiration at Tharandt.
The model was initialized with the first measurement from the data, and expected values were generated from user-defined initial parameter values.
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