Sentence examples for circulation of wind from inspiring English sources

Also, the vertical circulation of wind flow caused by the fire plume is well observed over the city.

"The trade off is that you also make it a little bit harder for some of those up-down motions to occur," he said, referring to the circulation of wind inside a storm cloud.

This anticyclone (circulation of winds around a central region of high atmospheric pressure) leads to southeast trade winds on its north side, since the rotation of wind around the high-pressure area is opposite to that in the Northern Hemisphere because of the Coriolis force (the effect caused by Earth's rotation).

Water exchange between the Ría and the adjacent shelf was mainly controlled by the upwelling/downwelling cycle, and tidal (both semidiurnal and spring–neap) variability appeared as a modulation of the response of the Ría circulation to wind variability.

Anticyclones that interrupt the normal circulation of the westerly wind in this way are called blocking anticyclones, or blocking highs.

The first and most important of them are the subtropical high-pressure air masses over the South Atlantic and South Pacific oceans and their seasonal shifts in position, which determine both large-scale patterns of wind circulation and the location of the rain-bearing intertropical convergence zone (ITCZ).

However, the depression continued to organize as deep convection continued to develop near the circulation despite moderate amounts of wind shear, and the system intensified into Tropical Storm Chris six hours after developing.

Second, upwelling occurs behind a typhoon because of the cyclonic circulation of the surface winds (Price 1981; Wada 2002).

Several new studies link the pause with changes in the Pacific and in the trade winds that influence the circulation of water within it.Trade winds blow east-west at tropical latitudes.

Orientation may control air for circulation and reduce the disadvantages of wind, rain, and snow, since in most climates the prevailing currents can be foreseen.

Over elevated surfaces, heating of the ground exceeds the heating of the surrounding air at the same altitude above sea level, creating an associated thermal low over the terrain and enhancing any thermal lows that would have otherwise existed, and changing the wind circulation of the region.