Sentence examples for distribution of the topside from inspiring English sources

Our results demonstrate a high degree of similarities in the occurrence pattern of the seasonal and longitudinal distribution of the topside ionospheric irregularities.

FedSat's GPS above-the-horizon data can be used by itself to obtain the electron density distribution of the topside ionosphere and plasmasphere using tomographic reconstruction technique.

The obtained results demonstrate a high degree of similarities in the occurrence pattern of the seasonal and longitudinal distribution of the topside ionospheric irregularities derived from both types of the satellite observations.

The integral function (Eq. (3)) has a unique solution under the assumption, as was made above, that the electron density distribution in the topside ionosphere of Mars has a monotonic profile.

Here we study the global distribution of the plasma density irregularities in the topside ionosphere by using the concurrent GPS and Langmuir probe measurements onboard the Swarm satellites.

The switch altitude between overestimation and underestimation and the latitude-local time distribution of the model deviation depend on the topside option.

Therefore, potentially we can obtain additional information on the global distribution of the plasma density irregularities in the topside ionosphere using GPS measurements from LEO missions without LP instrument, like GRACE, MetOP, TerraSAR-X, etc.; however, additional cross-validation analysis on the same database is needed.

This is highlighted during ionospheric disturbances (e.g. during geomagnetic storms), when the shape of the topside electron density distribution might be better described by an Epstein profiler rather than a Chapman profiler.

COSMIC RO measurements have several perspective advantages in comparison with the traditional ground-based measurements— global distribution of the occultation events and probing of the topside part of the ionosphere.

In this paper we consider an idea of the troposphere tide influence on the character of the longitudinal variations in the distribution of the equatorial plasma bubbles (EPBs) observed in the topside ionosphere.

We analyze the differences in the spatial distribution of ionospheric irregularities detected by the ground-based permanent GPS network with that of the topside GPS measurements onboard the Swarm constellation, using a case study of the 2015 St . Patricks Day storm.