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However, as the difference between irregularities of the right and left rails increases, the results obtained from 2D and 3D models are considerably different.
However, for the climatological study of correlation between irregularities and gravity waves, using a well-defined threshold to assure for the gravity wave occurrences in the OLRs will result in a clear conclusion.
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There was no interaction between irregularity and interval order (F 5,80) =0.6, NS).
For the other five sectors, no correlations are found in the m/l distributions between the irregularities and OLRs.
For the plots in the second and the fourth rows, linear regression of the monthly occurrences between the irregularities and OLRs in a longitude sector is shown.
The frequency response function between track irregularities and the vibration response of the vehicle track vertical coupled system can be obtained from Eq. (12).
On the other hand, no correlation exists between the irregularities and OLRs during the June solstice in the Central Pacific sector where the magnetic declination is positive.
For the other five longitude sectors, the monthly occurrence distributions between the irregularities and OLRs do not correlate with each other topographically or in the linear regression analysis.
Thus, in the seven longitude sectors, similar m/l distributions between the irregularities and OLRs are noticed only in the South American sector.
Similarly, no correlation is concluded for the Indian, West Pacific, and Central Pacific sectors, because the correlations are negative between the irregularities and OLRs and the OLRs are more abundant than the irregularities.
The linear regression analyses indicate that the African, South American, and Atlantic sectors have positive correlations between the irregularities and OLRs, while the Indian, West Pacific, Central Pacific, and East Pacific sectors have a negative correlation.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com