It's only a small one, so don't be surprised if our easterlies bring in some black dust.

The easterlies winds cause rainfall in the eastern coastal region.

Strong low level easterlies and rapid westward movement led to slower development thereafter.

After the weekend of easterlies waxwings continued to arrive.

Strong upper level easterlies halted development due to vertical wind shear.

The region 30 degrees on either side of the equator is characterized by easterlies (the trade winds).

Cold heavy air flows south from the north pole and is bent west, forming the polar easterlies.

For nearly two thousand miles they ran before the easterlies, covering most days more than a hundred and fifty miles.

The winter had Easterlies (from Siberia) as its dominant feature.

This flow of air is altered by the Earth's rotation and deflected east, hence the name easterlies.

This cuts off the source of cool subsiding air, and therefore the surface Easterlies cease.

From pole to equator they are the polar easterlies, the westerlies and the trade winds.

The southern polar easterlies are mostly over Antarctica.

Downward motion of the easterlies is usually more irregular than that of the westerlies.

Unlike the westerlies in the middle latitudes, the polar easterlies are often weak and irregular.

The winds over Antarctica are called the polar easterlies where winds blow from the east to the west.

Air flows outwards from the poles to create the polar easterlies in the arctic and antarctic areas.

All of this unequal heat, rushing air and spinning Earth combine to form global currents such as the polar easterlies.

A trough or cyclonic curvature maximum in the trade-wind easterlies.

Embedded within the deep easterlies, the depression tracked westnorthwestward at .

The initial forecast was for an increase in strength and motion into the easterlies at a pace of 11 mph (17 km/h).

Westerly winds are most frequent in the mid-latitudes while easterlies dominate the tropics.

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.

With the prevailing easterlies, Brysta was hot and damp, but seldom had much rain until late summer.

In September the dry north easterlies begin to strengthen and to push south and by the end of December they cover the entire country.

It's only a small one, so don't be surprised if our easterlies bring in some black dust.

The easterlies winds cause rainfall in the eastern coastal region.

Strong low level easterlies and rapid westward movement led to slower development thereafter.

After the weekend of easterlies waxwings continued to arrive.

Strong upper level easterlies halted development due to vertical wind shear.

The region 30 degrees on either side of the equator is characterized by easterlies (the trade winds).

Cold heavy air flows south from the north pole and is bent west, forming the polar easterlies.

For nearly two thousand miles they ran before the easterlies, covering most days more than a hundred and fifty miles.

The winter had Easterlies (from Siberia) as its dominant feature.

This flow of air is altered by the Earth's rotation and deflected east, hence the name easterlies.

This cuts off the source of cool subsiding air, and therefore the surface Easterlies cease.

From pole to equator they are the polar easterlies, the westerlies and the trade winds.

The southern polar easterlies are mostly over Antarctica.

Downward motion of the easterlies is usually more irregular than that of the westerlies.

Unlike the westerlies in the middle latitudes, the polar easterlies are often weak and irregular.

The winds over Antarctica are called the polar easterlies where winds blow from the east to the west.

Air flows outwards from the poles to create the polar easterlies in the arctic and antarctic areas.

All of this unequal heat, rushing air and spinning Earth combine to form global currents such as the polar easterlies.

A trough or cyclonic curvature maximum in the trade-wind easterlies.

Embedded within the deep easterlies, the depression tracked westnorthwestward at .

The initial forecast was for an increase in strength and motion into the easterlies at a pace of 11 mph (17 km/h).

Westerly winds are most frequent in the mid-latitudes while easterlies dominate the tropics.

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.

With the prevailing easterlies, Brysta was hot and damp, but seldom had much rain until late summer.

In September the dry north easterlies begin to strengthen and to push south and by the end of December they cover the entire country.