Climatology of the Thermospheric Neutral Wind over Arecibo Observatory based on over three decades of Fabry Perot observations and an Associated Empirical Model

Physics

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[2419] Ionosphere / Ion Chemistry And Composition, [2447] Ionosphere / Modeling And Forecasting, [2481] Ionosphere / Topside Ionosphere, [2487] Ionosphere / Wave Propagation

Scientific paper

We present an empirical model of the thermospheric neutral wind (TNW) meridional and zonal components based on 630.0 nm nightglow Fabry-Perot Interferometer data over the Arecibo Observatory. We show and discuss the solar and geomagnetic dependencies of the TNW components and their variation over local time and season. A main result of this study is the detection of a substantial seasonal and local time dependence of the response of the TNW to solar and geomagnetic activity. In addition, we show that there is a long-term trend in the thermospheric neutral wind, which can be of a larger magnitude than the variation found in the seasonal, solar cycle and geomagnetic activity. A major signature of this trend over the last 30 years was an increase in the meridional northward component up to 1.4 m/s per year before midnight local time during the summer.

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