Terdiurnal tidelike variability in sporadic E layers

Details Terdiurnal tidelike variability in sporadic E layers Terdiurnal tidelike variability in sporadic E layers

Jul 2006

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2006jgra..11107303h&link_type=abstract

Journal of Geophysical Research, Volume 111, Issue A7, CiteID A07303

Physics

5

Ionosphere: Ionosphere/Atmosphere Interactions (0335), Ionosphere: Midlatitude Ionosphere, Atmospheric Processes: Acoustic-Gravity Waves, Ionosphere: Ionospheric Dynamics

Scientific paper

Time series analysis was performed on a large database of ionosonde recordings taken over 12 years, for the 6-month period from the beginning of May to the end of October when sporadic E layer occurrence is frequent. The results show that in addition to the well known 24- and 12-hour tidal variations, there is also a weaker but regular 8-hour periodicity in midlatitude sporadic E layers (Es). Statistically, this terdiurnal periodicity is significant and occurs in both the sporadic E layer critical frequency (foEs) and the layer virtual height (h'Es), becoming strongest around summer solstice and later in October after a minimum in September. At times a weak 6-hour periodicity can also be present in Es but its effects are much less significant than those of the 8-hour oscillation. The 8-hour periodicity in Es is attributed to the terdiurnal tide, presumably acting through its vertical wind shear forcing of the metallic ions in the lower thermosphere. The relation to the terdiurnal tide was inferred from simultaneous ionosonde recordings from three widely spaced stations in the same midlatitude zone, showing the 8-hour oscillation to be present simultaneously in all ionosonde stations and have phases which are consistent with a westward propagating terdiurnal wave of zonal wave number 3. The present study establishes the regular occurrence of a terdiurnal tidelike oscillation in Es which needs to be incorporated into the physics and modeling of sporadic E layer formation and dynamics.

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