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In support of this model, the KM of substrate binding and the disassociation constant (Kd) of dimerization are unchanged as well.
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To reduce the atmospheric delay noise, we used a method for calculating the atmospheric delay based on the JMA results for a Meso-Scale Model, the 10-km-mesh numerical weather model (Ozawa and Shimizu 2010).
The LB model is less wavelength-dependent than the KM model, but the agreement with the thicknesses measurements made with OCT is worse than the KM model.
Fig. 12 When calculating the thickness of a thick and thin coating layer for different wavelengths, this calculated thickness differs by a maximum of 23.3 μm for the LB model and 40.6 μm for the KM model for different wavelengths.
Table 2 compares the accuracy of the KM model (the kinetic model described here) relative to other popular models described in the literature.
Previous studies have identified North Atlantic TC frequency and intensity as a key low bias in HadGEM2-ES, which has been attributed to the coarse spatial resolution of the model (~200 km at the equator 12,23.
The total horizontal size of the model was 356 km (times) 356 km.
The lateral dimensions of the regional model are 10,000 km × 10,000 km, and the horizontal mesh in the central area that includes the array is 50 km × 50 km.
For both models, this is probably because there is very high absorption in this region; the exponential function will turn reflectances tending to zero into LB model coefficients going to infinity and the solutions when solving for the K and S coefficients of the KM model will not be stable.
The checkerboard test showed good recovery beneath the Bonin ridge for the final modification of the model for line SPr2, but the eastern edge of the model (520 570 km) was not resolved at depths greater than 10 km.
In the KM model, the shortening effect is included in the velocity vector and the corresponding kinetic energy.
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