A study of quasi-16-day ionospheric oscillations

J. Y. Liu

doi:10.1007/BF02275370

A study of quasi-16-day ionospheric oscillations

J. Y. Liu

Department of Space Science and Engineering

Research output: Contribution to journal › Article › peer-review

2 Scopus citations

Abstract

A quasi-16-day oscillation has been found in measurements of ionospheric parameters and geomagnetic field strength in winter 1988. Data obtained from numerous magnetometers show that this oscillation is a global event. The horizontal phase velocities in the E-and F-regions of the middle latitudes demonstrate that the oscillation is a westward-traveling wave. The downward phase velocity and upward group velocity indicate that the oscillation source is located in the lower atmosphere.

Original language	English
Pages (from-to)	155-165
Number of pages	11
Journal	Radiophysics and Quantum Electronics
Volume	39
Issue number	2
DOIs	https://doi.org/10.1007/BF02275370
State	Published - 1 Feb 1996

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10.1007/BF02275370

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abstract = "A quasi-16-day oscillation has been found in measurements of ionospheric parameters and geomagnetic field strength in winter 1988. Data obtained from numerous magnetometers show that this oscillation is a global event. The horizontal phase velocities in the E-and F-regions of the middle latitudes demonstrate that the oscillation is a westward-traveling wave. The downward phase velocity and upward group velocity indicate that the oscillation source is located in the lower atmosphere.",

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N2 - A quasi-16-day oscillation has been found in measurements of ionospheric parameters and geomagnetic field strength in winter 1988. Data obtained from numerous magnetometers show that this oscillation is a global event. The horizontal phase velocities in the E-and F-regions of the middle latitudes demonstrate that the oscillation is a westward-traveling wave. The downward phase velocity and upward group velocity indicate that the oscillation source is located in the lower atmosphere.

AB - A quasi-16-day oscillation has been found in measurements of ionospheric parameters and geomagnetic field strength in winter 1988. Data obtained from numerous magnetometers show that this oscillation is a global event. The horizontal phase velocities in the E-and F-regions of the middle latitudes demonstrate that the oscillation is a westward-traveling wave. The downward phase velocity and upward group velocity indicate that the oscillation source is located in the lower atmosphere.

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DO - 10.1007/BF02275370

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JO - Radiophysics and Quantum Electronics

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SN - 0033-8443

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A study of quasi-16-day ionospheric oscillations

Abstract

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