In July 2012, the ATLAS and CMS collaborations at the CERN Large Hadron Collider announced the observation of a Higgs boson at a mass of around 125 gigaelectronvolts. Ten years later, and with the data corresponding to the production of a 30-times larger number of Higgs bosons, we have ...
In July 2012, the ATLAS and CMS collaborations at the CERN Large Hadron Collider announced the observation of a Higgs boson at a mass of around 125 gigaelectronvolts. Ten years later, and with the data corresponding to the production of a 30-times larger number of Higgs bosons, we have...
Orbital and surface observations can shed light on the internal structure of Mars. NASA’s InSight mission allows mapping the shallow subsurface of Elysium Planitia using seismic data. In this work, we apply a classical seismological technique of inverting Rayleigh wave ellipticity curves extracted from...
We present a PDE-based approach for finding optimal paths for the Reeds–Shepp car. In our model we minimize a (data-driven) functional involving both
Relying on the results of the kinetic theory, Reynolds pointed out [1] that in the free molecular flow regime the pressure ratio between the cold and the hot reservoirs is proportional to the square root of the respective reservoir temperatures: 𝑝c𝑝h=(𝑇c𝑇h)1/2,pcph=TcTh1/2, ...
(C) The simplified (except ophiolite sequence units) geological map of the study area (Appendix A). The black rectangle is the main surveying area where UAV and geological mapping were performed. Although highly dismembered and tectonized, the Sabzevar ophiolites show a typical oceanic tectonic ...
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Take the mean of thesquareof differences (which makes everything positive) and then take thesquare root(which undoes the squaring). This is called theroot mean squared error(RMSE) orL2 norm. It’s OK to Have Forgotten Your Math In this book, we generally assume that you have completed hi...
Least-squares regression quantifies the scatter of data around the curve by reporting Sy.x, sometimes called Se, the standard error of the fit. It is computed by taking the square root of the ratio of the sum-of-squares divided by the number of degrees of freedom (N-K, where N is ...
Thus, a simple explanation for the relationship found in Figure 7 is that preservation potential is linearly proportional to deposit thickness and to the square root of the deposit area, resulting in the observed 3/2 exponent for volume and 1/2 for mass. Cumulative curves of the number of ...