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1 Introduction The Earth's thermosphere, stretching from the mesopause to the exobase ( ∼ ${\sim} $ 85–500 km), is a critical region of the upper atmosphere that plays a pivotal role in space weather and satellite operations. These altitudes include both the ionosphere and the Low Earth Orbit (LEO) region, and its state is influenced by a variety of photochemical and dynamical processes.
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