Sentence examples for latitude ground from inspiring English sources

Initial results of subionospheric very low frequency (VLF) perturbations observed on NWC (19.8 kHz) and NPM (21.4 kHz) transmitter signals at low latitude ground station Varanasi, India, during the period January June 2010, are presented.

Villante et al. (2006) have presented a case in which power enhancements (at 1.4, 2.5, and 4.2 mHz) simultaneously occurred in the H component on the low latitude ground as well as in the radial component of the SW speed and IMF, while the SW density showed minor enhancements at different frequencies.

The shock impact was quite intense to produce a SSC magnitude of ∼80 nT in the low latitude ground magnetic records followed by sharp and deep main phase (Dst ∼−300 nT) in the first stage, following the density (Np) enhancement.

The distributed high latitude ground-based observations are now being interpreted within the context of in-situ data being provided by a variety of ISTP-era spacecraft.

The study relies on UV-visible observations at several mid- and high latitude ground-based stations in both hemispheres, complemented by balloon-borne solar occultation profile measurements and 3D chemical transport model simulations.

With a preliminary analytical method, electric field in F2-region before Wenchuan earthquake was derived from the five lower latitude ground-based ionosondes: Lhasa (29.63°N, 91.17°E), Chongqing (29.50°N, 106.40°E), Kunming (25.00°N, 102.70°E), Guangzhou (23.15°N, 113.35°E) and Haikou (23.15°N, 110.35°E).

It is suggested that low-latitude ground magnetic data may serve as a proxy for the interplanetary conditions in the solar wind.

In addition, our result suggests that a combination of equatorial and low-latitude ground magnetograms may be used to monitor the solar wind dynamic pressure variation not only in the northward IMF, but also in the southward IMF.

3.4 Observations at high-latitude ground stations.

We used the magnetic data from the geosynchronous ETS-VIII satellite and the low-latitude ground observatories.

Using data from the geosynchronous ATS-6 satellite and mid-latitude ground stations, (Sakurai and McPherron1983) found that Pi 2 onsets were almost simultaneous (within 1 min).