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.
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).
Monitoring strategy and extent of source data verification (SDV) are described in a trial specific monitoring manual.
MEG localizations slightly under-estimated the spatial extent of the sources and also showed few distant spurious sources.
Nonetheless, deeper magnetic sources affect long crustal magnetic field and that the estimation of the depth to the bottom of magnetic sources requires magnetic data that cover broader areas with dimensions that are longer than ten times the depth extent of magnetic sources to provide accurate estimates (Ravat et al. 2007; Bouligand et al. 2009).
The extent of these sources of exposure is unclear, as noted above, but is likely to present a minimal increase in exposure and hence risk in comparison to dietary intake.
Semantic profiling of a user's field of specialization or interest is necessary functionality in any medical domain information retrieval system; this is because the (structural and semantic) extent of information sources is massive and individual users are only likely to be interested in specific parts of the overall knowledge documents on the basis of their area of specialization.
Similarly to our previous findings in (Grova et al. 2006) and (Chowdhury et al. 2013), MNE was less sensitive than cMEM to the spatial extent of the sources, showing overall lower AUC values.
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.
