Mesospheric temperature trends derived from ground-based LF phase-height observations at mid-latitudes: comparison with model simulations

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Scientific paper

From indirect phase-height observations in the LF range at mid-latitudes, significant negative long-term trends of the ionospheric reflection height can be derived. The lowering of the reflection height at constant solar zenith angle can mainly be explained by a temperature decrease of the mesosphere due to increasing greenhouse gases (e.g. CO2) and a reduction of the atmospheric ozone content. Marked seasonal differences of the temperature trends could be found with a stronger cooling of the mesosphere in summer than in winter. A comparison of experimental trend results and model calculations with the three-dimensional global circulation model COMMA-IAP shows a reasonable agreement.

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