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In general, the error existing between observations and simulation is reduced substantially by proper calibration of the vegetation/soil parameters.
In addition, the lack of representative thermodynamic and rate expression data contributed to the discrepancies between observations and simulation results, thus further research into the applicability of laboratory-derived thermodynamic and rate expression data to field conditions could minimize these discrepancies.
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A reasonable agreement between observations and simulations of trends in mesospheric temperatures and PMC albedo levels has also been achieved.
A reasonable agreement between observations and simulations of trends in mesospheric temperatures and PMC albedo has been reached.
b Horizontal residuals between observations and simulations Fig. 6 Simulated coseismic deformation field and residuals for InSAR.
We also compare the spatial distribution of first-motion polarizations between observations and simulations using our MT results.
Large discrepancies are found between observations and simulations in the SR region (Fig. 4d f), ACtrans region (Fig. 4g i) and AC region (Fig. 4j l).
Both are well reproduced in terms of frequency, but the simultaneity of occurrence of exceedance days between observations and simulations is not well captured.
Due to subgrid variability and differences between the simulation and observation scale (the Digital Elevation Model pixel versus the point measurement), the point-to-point comparison between observations and simulations shows a poor correlation.
Between observations and simulations for various types of experiments, such as a hold under a constant shear stress (left column), reloading after the hold (middle column), steady-state sliding at different velocities, and transience between them (right column) from Figure Sixteen of Nagata et al. (2012).
To check the estimation error of the focal mechanism of our MT results, we evaluated the variance reductions of F-net displacement waveforms between observations and simulations of a double-couple point source with a fixed seismic moment and centroid depth but changing strike, dip, and rake angles (Fig. 9).
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