Sentence examples for extent of source from inspiring English sources

Tsunami observations can provide good timing constraints on the location of seafloor motions, potentially constraining slip at shallow depths, but the long wavelengths involved do require accounting for the full spatial extent of source motions (Lay et al., 2011b).

Our objectives here were to show how measurements of the distribution of contaminant mass flux and the overall mass discharge emanating from the source under undisturbed groundwater conditions could be related to the processes and extent of source mass depletion.

Monitoring strategy and extent of source data verification (SDV) are described in a trial specific monitoring manual.

Such studies can, in turn, provide important insights concerning the identity and extent of sources of variability that may arise in the source-to-outcome continuum for a given chemical class, physiologic state, or adverse response.

However, instantaneous measurement of the longitudinal distribution of waves and particles is essential to provide quantitative understanding, because, for example, statistical analysis of long-term single satellite data can lead to misinterpreting a moving localized wave source as a wide spatial extent of the source region.

This detection accuracy index (between 0 and 1) integrates sensitivity and specificity of the source localization methods to reconstruct the spatial extent of the source against the Ground Truth, by varying a detection threshold between 0 and the maximum of reconstructed current density.

This indicates that MEEG localizations presented less spatial spread of the solution around the true extent of the source or less spurious activities distant from the true source than EEG or MEG localizations.

The spatial extent of each source was obtained by region growing around the seed following the cortical surface using spatial neighborhood order s e  = 3 (≈4 cm) and s e  = 4 (≈12 cm).

The aftershock distribution of large earthquakes is essential for estimating the extent of a source fault.

Thus, we neglect the finite extent of the source zone in this study.

The aftershock distribution and geodetic observations suggest that a spatial extent of the source fault is controlled by this boundary.