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A weak inverted wave in the easterlies is generally found beneath it, and it may also be associated with broad areas of high-level clouds.
Winds are frequent and salt-laden being moderate easterlies in the summer and fresh to strong westerlies in the winter.
Air flows outwards from the poles to create the polar easterlies in the arctic and antarctic areas.
Unlike the westerlies in the middle latitudes, the polar easterlies are often weak and irregular.
Embedded within the deep easterlies, the depression tracked west-northwestward at 20 mph.
The initial forecast was for an increase in strength and motion into the easterlies at a pace of 11 mph (17 km/h).
Strong upper level easterlies halted development due to vertical wind shear.
A weak inverted wave in the easterlies is generally found underneath them, and they may also be associated with broad areas of high-level clouds.
Westerly winds are most frequent in the mid-latitudes while easterlies dominate the tropics.
The polar easterlies are one of the five primary wind zones, known as wind belts, that make up our atmosphere's circulatory system.
Downward motion of the easterlies is usually more irregular than that of the westerlies.
Embedded within the deep easterlies, the depression tracked west-northwestward at 20mph km/h.
From pole to equator they are the polar easterlies, the westerlies and the trade winds.
Most of them are detectable in the low tropospheric temperature field as cold troughs in the easterlies.
Figure 2 illustrates the steady southerly and easterly spread of the epizootic between the early cases in the third quarter of 2001 and the final quarter of 2002.
