| Bildiri Türü | Tebliğ/Bildiri |
| Bildiri Alt Türü | Tam Metin Olarak Yayınlanan Tebliğ (Uluslararası Kongre/Sempozyum) |
| Bildiri Niteliği | Alanında Hakemli Uluslararası Kongre/Sempozyum |
| Bildiri Dili | İngilizce |
| Kongre Adı | FIG Working Week 2017 |
| Kongre Tarihi | 29-05-2017 / 02-06-2017 |
| Basıldığı Ülke | Finlandiya |
| Basıldığı Şehir | Helsinki |
| Bildiri Linki | http://www.fig.net/resources/proceedings/fig_proceedings/fig2017/papers/ts07c/TS07C_basciftci_inal_et_al_8940.pdf |
| Özet |
| The atmosphere surrounding the earth as a cover is divided into different layers depending on its characteristics such as density, heat and height. A part of the atmosphere containing free electrons and ions is called the ionosphere. The ionosphere is a natural plasma environment located at an altitude of 70 km to 1000 km of the atmosphere and shaped by radiation from the Sun. The radiation from the sun forms positively charged ions and free electrons by ionizing the atoms and molecules in the ionosphere. The ionosphere is an important layer affecting GNSS (Global Navigation Satellite System) measurements. The quality of the GNSS measures is directly related to the changes in the ionosphere. Total Electron Content (TEC) is one of the important parameters expressed to character of the ionosphere which has great importance for satellite based positioning, shortwave and satellite communication systems … |
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