SuperDARN observations show the migrating semidiurnal tide weakens immediately after SSW onset then strengthens anomalously 10-17 days later, with nonmigrating components varying differently and linked to background wind shifts.
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2 Pith papers cite this work. Polarity classification is still indexing.
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M-GITM simulations show gravity waves are critical for aphelion thermospheric polar warming but the model underestimates the observed polar-to-low-latitude temperature difference.
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SuperDARN Observations of Semidiurnal Tidal Variability in the MLT and the Response to Sudden Stratospheric Warming Events
SuperDARN observations show the migrating semidiurnal tide weakens immediately after SSW onset then strengthens anomalously 10-17 days later, with nonmigrating components varying differently and linked to background wind shifts.
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Mars Thermospheric Polar Warming at Aphelion: Dynamical Processes Studied Using M-GITM
M-GITM simulations show gravity waves are critical for aphelion thermospheric polar warming but the model underestimates the observed polar-to-low-latitude temperature difference.