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Therefore, we propose here a 3D parallel inversion procedure with different numbers of rings and different Lp norms, with 1<p⩽2, applied to the model regularization of the misfit function to increase the resolution of the models after inversion.
Under the idealized conditions of perfect models and precipitation input, one may expect that spatiotemporal specificity and accuracy of the model output improve as the resolution of the models and precipitation input increases.
Figure 1 shows the attributes diagram for evaluating the reliability and resolution of the models.
The reviewer has already expressed his reservations regarding the resolution of the models.
First, to assess whether additional time points of HRV and BP data would improve the resolution of the models, we modeled the mean change in outcome across five measurements taken every 30 min during the 2-hr exposure.
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The spatial resolution of the model is limited by the computer resources available.
To assess the vertical resolution of the model, we performed spike tests (Fig. 6a d).
(c) What is an optimal resolution of the model to account properly for the ocean effect?
The resolution of the model is chosen to be 1° × 1°.
The resolution of the model is indicated by the degree to which the introduced velocity perturbation is reproduced.
The spatial resolution of the model is set sufficiently high to reproduce the variations in the Kuroshio Current.
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Since I tried Ludwig back in 2017, I have been constantly using it in both editing and translation. Ever since, I suggest it to my translators at ProSciEditing.

Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com