Adding identity to device-free localization systems

Energy releases are observed in numerous dynamic phenomena (e.g. solar flares, coronal mass ejections, solar energetic particle events) where mea- surements provide signatures of

For the TrOCA method we identified low inventory estimates in the South Atlantic (Fig. 3b) due to the relatively large amount of negative C ant estimates in deep waters (Fig. The

Variational data assimilation, soil water movement, quasilinear parabolic problem, solvability, numerical analysis.. 1 LMC-IMAG, 38041 Grenoble Cedex

L’archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des

Bacteria in organic and mineral horizons generally declined with warming treatment, and those that increased in response to warming tended to be dominant in control soils, thus

Figure 6. The upper panel is the time series of the Helmert translation parame- ters in X, Y, Z and terrestrial scale of the combined solution with respect to IGb08. The lower panel

We expected that anticipation of tennis shot direction would be made possible when simulations contained dynamic differences in shot direction (Huys et al., 2008),

Although this method to employ type II sums on questions about prime number asymptotics is somewhat easier than those already in the literature, it seems harder to incorporate