Sentence examples for mean winds in from inspiring English sources

Mean winds in the horizontal direction are ~1000 times faster than in the vertical direction, and are more organized, so that FA usually dominates over FT as long as Dt is not too large (say less than a day).

Data obtained by Wuhan (30.5°N, 114.4°E) MF radar and Yamagawa (31.2°N, 130.6°E) MF radar have been used to study the mean winds in the mesosphere and lower thermosphere (MLT) at about 30°N.

On Mars the first asymmetric eastward propagating mode with vertical wavelength of about 60 km is very efficiently induced by the asymmetric zonal mean winds in the middle atmosphere; this wave component propagates well into the thermosphere and accounts for much global asymmetry seen in the wave fields.

To verify the statistical confidence of nonzero differences in the mean winds in Fig. 1b, c, we can apply the statistical Student's t test (e.g., Rice 2006).

Positive and negative differences of the mean winds in Fig. 1b produce increases and decreases of ( {n}_m^2 ) in Fig. 6b.

The forcing (2) may approximate spectral components of convective and turbulent AGW sources transported by the mean winds in the atmosphere (Townsend 1965, 1966).

Supercells often propagate in a direction and with a speed other than indicated by the mean wind in the environment.

A TIME-GCM simulation by Liu and Roble (2002) revealed that the resonant SPW amplification prior to the peak warming causes a deceleration of the mean wind in the high latitude winter stratopause and mesosphere and reverses to westward with a critical layer near the zero wind line.

This study suggests that such conditions can last for a few hours, thus yielding an estimate of the lifetimes of the KH billow which is generated and deformed during 18 00 to 19 00 IST interval and can then be nearly 'frozen-in' and advected along with the mean wind in the absence of strong shears.

Therefore, we would expect DE3 and to some degree DE2 to take on a symmetric character in the upper thermosphere and for D0 to take on a more asymmetric character; however, factors such as ion drag and zonal-mean winds in the thermosphere can add further complications.

In the height range 80 100 km there is an increase in the annual mean winds and in the amplitudes of the annual and semiannual oscillations; also the semiannual oscillation is larger than the annual one.