Air current
Concentrated areas of wind due to atmospheric pressure or temperature gradients / From Wikipedia, the free encyclopedia
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In meteorology, air currents are concentrated areas of winds. They are mainly due to differences in atmospheric pressure or temperature. They are divided into horizontal and vertical currents; both are present at mesoscale while horizontal ones dominate at synoptic scale. Air currents are not only found in the troposphere, but extend to the stratosphere and mesosphere.