Sentence examples for evolution of the half from inspiring English sources
In Figure 15, we see that the best patch classification performance corresponds to an HTRR of 73.1% and a of 0.35 with the empirical modeling, and an HTTR of 76.3% for a of 0.2 and aspect model 2. This latter value of is chosen for all the MRF illustrations reported in Figures 16 and 17. Figure 15 The evolution of the half total recognition rate for different values for the MRF regularization.
Fig. 8 Daytime evolution of the half-hour mean evaporative fraction (EF) for both the wet and dry periods.
Fig. 7 Daytime evolution of the half-hour mean water use efficiency (WUE) (black continuous line) and vapour pressure deficit (VPD) (grey square) for both the wet and dry periods.
Experimentally, this calibration has been approached by previously studying the evolution of the mean half radius of δ′ by transmission electron microscopy (TEM).
It is controlled by the evolution of the asymmetric half-graben on the basal drag fault.
Conversely, however, the functional loss of a digit in syndactylous feet may have favoured the evolution of the bounding or half-bounding habit in both clades.
It takes the passing of a legend like Ravi Shankar, who died yesterday, at the age of ninety-two, to remind us that the permeability of genre is a modern invention, one that has driven the rapid musical evolutions of the past half-century.
It seems that the complete dehydration induces a drastic rearrangement of the environments of both central atoms related to the evolution of half molecule of cyanogen and one molecule of en from the formula unit of 1b, which is probably reflected on the DSC curve by the mentioned exo-effect at 208°C.
Tectonic history may be summarised as follows: (1) origin of the Quaternary fault-bounded Colfiorito and Cesi San Martino basins; (2) evolution of the basins with a half-graben style; (3) significant reduction of tectonic activity since the Middle Pleistocene.
In this way, the LSPR can be varied from 680 nm to 580 nm with a concomitant marked evolution of the full-width at half-maximum from 200 to 80 nm.
Here we analyse the longitudinal profile of rivers (n = 84) and the river basin topography (n = 72) with the aim of unravelling the evolution of the Amatlán de Cañas half-graben (ACHG), a Plio-Quaternary structure located in the northern sector of the Jalisco Block (west-central Mexico).
