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Projekt Druckansicht

Die kurzzeitige Variabilität der äquatorialen Ionosphäre und ihre Verbindung zu planetaren atmosphärischen Wellen

Antragsteller Dr. Yosuke Yamazaki
Fachliche Zuordnung Physik des Erdkörpers
Förderung Förderung von 2019 bis 2025
Projektkennung Deutsche Forschungsgemeinschaft (DFG) - Projektnummer 416609110
 
Erstellungsjahr 2023

Zusammenfassung der Projektergebnisse

The primary goal of this project is to improve our understanding of the day-to-day variability, or “weather”, of the ionosphere, at altitudes of ca. 100−600 km. In particular, this project focuses on the ionospheric variability associated with globalscale atmospheric waves, such as planetary waves and atmospheric tides. Planetary waves have a period longer than a day and shorter than several weeks. Their ionospheric effects could make a contribution to the ionospheric day-to-day variability. We have found that there is often a “burst” of planetary-wave activity in the middle atmosphere (i.e., the neutral atmosphere just below the ionosphere, ca. 50−100 km) during sudden stratospheric warming (SSW) events. The “Fourier-wavelet” technique has been developed to enable to identify planetary-wave bursts during SSWs. We have also found evidence of the planetary-wave effect on the ionosphere during SSWs. In particular, during the Antarctic SSW event of September 2019, ionospheric oscillations with a period of ~6 days are detected in various parameters, including the equatorial electrojet, zonal electric field, and F- region plasma densities, along with a strong quasi-6-day wave in the middle atmosphere. Besides the quasi-6-day wave, the equatorial Kelvin wave with a period of ~3 days plays an important role for the ionospheric dayto-day variability at low latitudes. Atmospheric tides have a period of a solar day (24h) and its harmonics (12h, 8h, …). Thus, they do not make a direct contribution to the ionospheric day-to-day variability. Nevertheless, the interaction of tides with planetary waves can lead to “secondary waves”. For instance, the interaction between the semidiurnal tide (12h) and quasi-6- day wave results in a pair of global-scale waves; one with a period of 11h and the other with a period of 13h. These secondary waves were found to be important for the ionospheric day-to-day variability observed during the September 2019 SSW event. As briefly highlighted above, the ionosphere is subject to atmospheric forcing by various global-scale waves. This project was able to identify the importance of planetary waves and their interaction with tides for the ionospheric day-to-day variability.

Projektbezogene Publikationen (Auswahl)

 
 

Zusatzinformationen

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