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The phase velocity of IG waves observed in deep ocean environments is accurately explained by the gravity wave theory (e.g., Webb et al.1991).1991
Smith et al. (2011) showed that this change modifies gravity wave propagation into the mesosphere during late spring so that the mesospheric residual mean circulation is weakened by the gravity wave drag.
The ionospheric dynamo currents must be accompanied by the FACs, because the dynamo region caused by the gravity wave is limited in the horizontal scale and the dynamo currents need to divert along a highly conductive geomagnetic field, forming the FAC system.
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The mesospheric residual mean circulation could be intensified by changes in the gravity wave drag, thus causing a negative temperature trend in the summer polar mesosphere.
This could be due to the fact that the induced gravity wave generated in the ITCZ is blocked by the wind filtering effect around the mesospheric height in the upward propagation from the troposphere to the ionosphere (Mukherjee et al.2010) or by the polarization factor of the gravity wave that fails to trigger the irregularity occurrences (Tsunoda2010b).
(c) Sample of filtered TEC maps showing the gravity wave emitted by the rupture.
When the gravity wave passes by, it should expand and contract the aluminum or niobium bars.
Although initiation by a gravity wave seems likely, the gravity wave interaction cannot yield the large displacements observed without further amplification by the Rayleigh-Taylor instability, as suggested by Kelley et al. (1981 , 1986.
The modulation process of the neutral layer by gravity waves differs from that of ionized layers, and the propagation direction of the gravity wave is inferred using the difference between those mechanisms.
Indeed, if these structures were produced by a gravity wave moving slightly upstream (to account for the upstream migration of the crests), one should observe truncations on the lee sides, or the wavelength of the gravity wave should increase during building of the cross-stratification. Thus, neither the steep transverse, nor the lunate nor 2D DBs can be interpreted as antidunes.
Garcia et al. (1997) described QBO modulation of the SSAO due to filtering of the gravity waves by the QBO.
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