Sentence examples for peak density for from inspiring English sources

The lower the altitude of the peak density for a given species, the longer it takes that species to escape and be sampled at 2.5Rt.

Then, using the TECgps input with the IRI-Plas code, we attribute the difference between the model and the measured TEC at altitudes from 65 km to 20,200 km (GPS orbit) as a source to update the F2-layer peak density for the GPS signal's travel through the oxygen-dominated plasma of the ionosphere and the tenuous hydrogen-dominated plasma of the plasmasphere.

Peak density for An.

The analyses that provided statistically significant values (p < 0.05) were peak density for lobular carcinomas, ductal carcinomas, and FN-FA-TA pathologies, and cepstrum slope for FN-FA-TA and benign pathologies.

The panels in Fig. 4 show a comparison of the ionosonde-derived and the GPS-reconstructed seasonal averaged NmF2 with the modeled (used here the IRI-2007 moutputstputs) F2-peak density for the three stations; SL (top panel), FZ (middle panel) and CP (bottom panel).

For example, comparing the RSFC-Snowballing aggregate peak density maps for a subject scanned on 2 separate sessions with 13 intervening days between the scans revealed a high degree of similarity (Fig.  11; mean spatial correlation between each subject's day 1 and day 2 RSFC-Snowballing aggregate peak density maps = 0.62, range of all subjects: r = 0.48 0.76).

It is worth highlighting that the IRI storm model option was implemented mostly to represent the mid-latitude F2 peak density variations for disturbed conditions.

However, there is no significant difference in peak density distributions for 1-, 2- and 3-fold rotated samples prepared in the same batch.

In the final step, an aggregate RSFC-Snowballing peak density map for the initialization location set was derived by summing all the starting location's peak density maps (Fig.  2 c).

From 2003 2012 dataset of the Irkutsk DPS-4 Digisonde (52.3°N, 104.3°E), we obtained the diurnal, seasonal and solar activity pattern of the F2 peak density (NmF2) variability for both high- and low-frequency parts of the variability.

The STORM-E model provides a dynamic storm-time correction factor to adjust a known nighttime quiescent E-region electron density peak concentration for geomagnetic enhancements due to auroral particle precipitation.