| Themes > Science > Astronomy > The Solar System > The Solar System > The Earth > Consequences of Rotation for Weather | ||||
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Coriolis ForcesThe following diagram illustrates the effect of Coriolis forces in the Northern and Southern hemispheres.
Since winds are just molecules of air, they
are also subject to Coriolis forces. Winds are basically driven by Solar
heating. As the adjacent (highly idealized) image indicates, Solar heating
on the Earth has the effect of producing three major convection zones in
each hemisphere.
If solar heating were the only thing influencing the weather, we would then expect the prevailing winds along the Earth's surface to either be from the North or the South, depending on the latitude. However, the Coriolis force deflects these wind flows to the right in the Northern hemisphere and to the left in the Southern hemisphere. This produces the prevailing surface winds illustrated in the adjacent figure. For example, between 30 degrees and 60 degrees
North latitude the solar convection pattern would produce a prevailing
surface wind from the South. However, the Coriolis force deflects this
flow to the right and the prevailing winds at these latitudes are more
from the West and Southwest. They are called the prevailing Westerlies.
In these composite images red indicates visible light (reflected sunlight), green indicates the 11 micron IR channel (thermal emission), and blue indicates the 3.9 micron channel (thermal + sunlight). At night the images are blue and green. The three periods of daylight in this 72 hour sequence are clearly visible as red-orange regions moving from East to West (right to left). In the IR channels, the natural intensity pattern has been inverted: warmer is darker, so that cool cloudtops stand out brightly. One can see clearly the pronounced cloud flows associated with the strong westerlies at mid-latitudes in each hemisphere. (This is taken in Northern hemisphere Winter, so the heavier cloud cover in that hemisphere is not surprising.) Less obvious are the easterly trade winds and the polar easterlies, though one can see vestiges of each if one looks carefully. Also apparent are the swirling motions associated with frontal systems. These are particularly pronounced at the boundaries between the mid-latitude westerly and polar wind flows in each hemisphere. Cyclones & AnticyclonesThe swirling motions evident in the preceding animations are consequences of frontal systems anchored to high and low pressure systems, which are also called anticyclones and cyclones, respectively. The wind flow around high pressure (anticyclonic) systems is clockwise in the Northern hemisphere and counterclockwise in the Southern hemisphere. The corresponding flow around low pressure (cyclonic) systems is counterclockwise in the Northern hemisphere and clockwise in the Southern hemisphere. This is a consequence of the Coriolis force, as illustrated for the Northern hemisphere in the following figure.
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