The phrase "atmospheric tides" is correct and usable in written English.
It can be used in discussions related to meteorology, oceanography, or physics, particularly when referring to the periodic variations in atmospheric pressure and wind patterns caused by gravitational forces.
Example: "The study of atmospheric tides is essential for understanding weather patterns and their impact on climate change."
Alternatives: "air tides" or "meteorological tides".
By nudging wind and temperature to the reanalysis data in the troposphere and stratosphere, the eCMAM is able to produce the stratospheric QBO (not shown), thus allowing a more realistic interaction between the atmospheric tides and background atmosphere.
They quantified the effects from in-situ physical processes and atmospheric tides from the low atmosphere.
The agents which teleconnect the lower and upper atmosphere in these cases are atmospheric tides for the former two and CO2 infrared radiative cooling for the latter.
This complete dataset enables a comprehensive evaluation on the momentum and energy budget of the atmospheric tides and its relationship with natural variability in the atmosphere such as ENSO and QBO.
A major advantage of using data-assimilated middle atmosphere models such as eCMAM30 to study interannual variation of the atmospheric tides is to have many available variables (296 in the case of eCMAM30) that are self-consistently generated and regularly saved at even spatial and temporal grids.
Significant correlation of the ISO between the TCWV and MLT zonal wind as well as modulation of the tidal amplitudes in the ISO period band may suggest a contribution of the atmospheric tides to the existing ISO coupling of the lower and middle atmosphere.
The rotation period of Venus may represent an equilibrium state between tidal locking to the Sun's gravitation, which tends to slow rotation, and an atmospheric tide created by solar heating of the thick Venusian atmosphere.
Yes, the phenomenon is known as the lunar atmospheric tide.
Ingersoll and Dobrovolskis4 have reconsidered this suggestion, and attempted a quantitative calculation of the atmospheric tide.
The scope of the current article is to assess the data assimilation ionosphere model capabilities in representing the longitudinal effect in the night time ionosphere induced by the DE3 atmospheric tide.
The atmospheric oscillation tides could be periodic or chaotic.
