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The largest positive and negative zonal wind differences between the westerly and easterly QBO phases in Fig. 1c occur in the stratosphere near the equator.
This is similar to the wind differences between the westerly and easterly QBO phases obtained from meteorological reanalysis data and simulated with tropospheric-stratospheric-mesospheric general circulation models by Yamashita et al. (2011) and Pogoreltsev et al. (2014).
Figure 1 also presents the altitude-latitude structures of the monthly mean differences of zonal mean velocities due to inclusion of OGW effects for the easterly QBO phase (Fig. 1b) and differences between the westerly and easterly QBO phases without OGW effects (Fig. 1c) in January.
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The currents in the Northern Hemisphere are weaker than those in the Southern Hemisphere due to the differences in strength between the Westerlies of each hemisphere.
Our simulated differences in the mean zonal winds between the westerly and easterly QBO phases at high latitudes of the northern hemisphere in Fig. 1c have different signs at different altitudes.
Positive and negative differences correspond to the westerly and easterly QBO phases.
There are fundamental differences between the two.
There are clear differences between the tests.
Describe the differences between the two.
The differences between the groups were remarkable.
Other differences between the sexes emerged.
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Justyna Jupowicz-Kozak
CEO of Professional Science Editing for Scientists @ prosciediting.com