Impact of the lower thermospheric winter-to-summer residual circulation on thermospheric composition
This study suggests the significance of “residual thermospheric circulation,” a process acting like a “lower thermospheric spoon,” that was long neglected but could be responsible for the seasonal gradients in the thermosphere and ionosphere and account for a long-standing deficiency in models for circulation in the upper atmosphere. Through a set of simulations, the authors investigate the significance of the process of residual thermospheric circulation, and conclude that it is important in representing seasonal gradients in the thermosphere and ionosphere.
- Article Category
- Research Letters
- Space Sciences
Impact of the lower thermospheric winter‐to‐summer residual circulation on thermospheric composition
- First Published:
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Eos.org: Earth & Space Science News
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