Sentence examples for modeled temperature was from inspiring English sources

The modeled temperature was in relatively good agreement.

For both plots modeled temperature was underestimated as compared to field data with RMSE of 1.0 1.5 °C, but the pattern of temperature spatial differentiation was similar to that observed in the field.

For the tectonic tremor region near the central part (or northern edge of southern part) of the North Island (Figure 2a), the modeled temperatures are very high (at least 500°C even for the highest corresponding λ parameter) for the scenarios set to a convergence rate of 2 and 4 cm/year.

To the best of our knowledge, the effect of temperature was modeled relatively accurately for the first time in this type of model.

Accuracy in terms of mean absolute error between modeled and observed temperatures was 1.63°C for minimum and 3.57°C for maximum temperatures (Table 4).

Accuracy in terms of mean absolute error between modeled and observed temperatures was generally better for minimum than maximum temperatures, likely due to greater fine-scale variability in maximum temperature lapse rates.

In the primary analyses, ambient and apparent temperature were modeled as continuous linear functions.

The modeled creep compliances at every temperature were converted into the relaxation moduli according to the constitutive relations of the generalized Kelvin model.

For validation, the modeled external surface temperatures are compared with experimental results obtained while changing the inlet temperatures of the nitrogen working fluid.

To explore the uncertainties in the resulting modeled temperature distribution, the numerical modeling is carried out three times; each one is based on the original, maximum, and minimum value of formation thermal conductivity and basal heat flow density.

The phenomenon demonstrated by the temperature-at-depth maps (Fig. 10; "Modeled temperature fields" section) can be explained by examining the characteristic of the subsurface geology, i.e., in terms of the depths where the lateral distribution of lithology starts to change significantly.