Sentence examples for compared electron density from inspiring English sources

By using these data sets, we compared electron density profiles as well as Pedersen and Hall height-integrated conductivities in order to evaluate the photometric method using two emission lines at 427.8 and 630.0 nm.

Robinson et al. (1992) compared electron density measurements from the Søndre Strømfjord (67°N, 51°W) IS radar with electron densities inferred from OI (135.6 nm) and N2 + (391.4 nm) emissions observed by the auroral ionospheric remote sensor (AIRS) onboard the Polar Bear satellite and found a good agreement between the measured and inferred profiles.

To do this, we compared electron density maps for crystals of RPo soaked with ATP and CMPcPP to electron density maps for crystals of RPo first soaked with GE and then soaked with ATP and CMPcPP.

We compare electron density predictions of the International Reference Ionosphere IRI-20077) model with in situ measurements of the satellites CHAMP and GRACE for the years from 2005 to 2010 over the subauroral regions.

In that way COSMIC RO profiles derived on October 11, 2008 (Disturbed day) were compared with electron density profiles derived from the measurements of the nearest ionosonde.

Lei et al. (2007) compared the electron density profile from constellation observing system for meteorology, ionosphere, and climate (COSMIC) radio occultation (RO) measurements with those observed by incoherent scatter radar (ISR) at Millstone Hill and Jicamarca for a limited number of overhead passes.

This contributes to the decrease of hydrogen storage capacity for LaNi4Al, which is illustrated by comparing the electron density distribution of LaNi4AlH7 with LaNi5H7.

We further compare the electron density with U (white arrows) and the longitudinal maximum W (W M, white circle-dots in each of plots) at 300-km altitude at 75° S during the 4 months.

The water content of the films swelled at different humidity conditions was calculated comparing the electron density of the dry and the swelled films.

This study compares the electron density and temperature observed by the CHAMP satellite and those predicted by the International Reference Ionosphere (IRI) model.

Results of the 3-D model are shown by comparing the electron density profiles given by the model with the ones measured at two testing ionospheric stations: Roquetes (40.8°N, 0.5°E), Spain, and San Vito (40.6°N, 17.8°E), Italy.