Geomatik Uygulama ve Araştırma Merkezi, (GEOMER) / Geomatics Application and Research Center

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Browsing Geomatik Uygulama ve Araştırma Merkezi, (GEOMER) / Geomatics Application and Research Center by Author "Can, Zehra"

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    Observation of Kinetic Alfven Waves and Mirror Mode Structure by THEMIS in Central Plasma Sheet
    (2015-06-16) Guyer, Sinan; Can, Zehra; 2759
    Substorms are effective indicator for many physical phenomena in magnetosphere. The central plasma sheet is the main research area in this study which is located in the nightside of the magnetosphere. Since plasma structure shows variability during the substorm, examination of the plasma changes can be observed. This variability contains low frequency structure and instability. The goal of the study is observation of this low frequency, namely kinetic Alfven wave structure and the mirror-mode structure which can be found in high beta plasma condition during substorm time. Charged particles can be accelarated by the KAWs because of their parallel electric field. The energization and acceleration mechanism can be driven by KAWs in central plasma sheet. Both these low frequency structures are important to understand of plasma responds during the substorm. Observations are made with THEMIS-E probe in tail-science, stage 23 of mission which provides a good opportunity for the researchers in order to investigate substorms.
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    The Ionospheric Refractivity Effects on the GPS Signals
    (IEEE, 345 E 47Th St, New York, Ny 10017 Usa, 2013) Ünver, Onur; Guyer, Sinan; Uzel, Turgut; Can, Zehra; 9308; 2759
    The communication between the global navigation satellites and ground observation stations is provided by the electromagnetic waves that emits from the satellites. When the satellite signals pass through the Ionosphere, they are refracted by the different Ionospheric layers. The precise determination of the Ionospheric refractivity index is crucial for the evaluation of the Ionospheric delay that depends on the refraction ratio. The electromagnetic waves that passes through the Magnetoionic medium interacts with the medium depending upon the free electron content and plasma frequency. As a consequence of that interaction the medium shows the dispersive and refractive effects on the waves. The phase and group velocity of an electromagnetic wave in the vacuum are equal and advances with the speed of light, on the other hand in the plasma medium there is a relativistic difference between the phase and group velocities, and this difference depends on the refractivity index of the medium. The refractivity shows varieties depending upon the free electron content of the medium, external magnetic field, gyrofrequency of electrons and plasma frequency. In the earth's atmosphere the layer that locates the altitude 501000 km and contains free electrons and positive ions as a result of the effects of the solar radiation and solar energetic particles is called as Ionosphere. In the Ionosphere, the thermal effects on the electrons are low level so this region is termed "cold plasma". In the Ionospheric researches, due to mass of the positive ions higher than mass of the electrons, ion motions are neglected. In terms of quality and quantity, Ionosphere shows the Magnetoionic medium effects on the electromagnetic waves. In this study, the variations of the Ionospheric refractivity index on the GPS signals due to different Ionospheric conditions is examined and made a comparison with the results of the literature.