Warm Front Research Paper

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A warm front is the surface limit between a warm air mass and a frosty air mass it is overwhelming. The warm air moves into a zone of colder, drier air. The air masses don 't promptly blend; in this way the warm air rises gradually over the colder air in light of the fact that it is less thick. This produces mists and precipitation well in front of the drawing nearer warm front, subsequent to warm air in the southeastern US generally has higher water vapor content than cool air. Relentless precipitation for the most part endures along the limit of a warm front. This measure of precipitation, nonetheless, relies on upon the measure of dampness noticeable all around in front of the surface front. On the off chance that the warm air is generally dry and stable, precipitation would not be liable to happen. On the off chance that the air is wet and restrictively flimsy, overwhelming precipitation could happen over an expansive territory.

In the winter, a closer warm front is liable to achieve risky winter climate conditions. Along the warm front, close to the surface, where temperatures are
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The frosty air mass pushes under the warm air mass in view of its higher thickness, driving this warm air to rise. In the event that enough dampness exists in the climate right now, then mists and conceivably rainstorms could create. Icy fronts move much quicker than warm fronts. Cold fronts are spoken to as blue triangles on a climate guide and move in the heading that the "teeth" are indicating. Icy fronts are normally went with regions of low weight. Winds blow counter-clockwise around a territory of low weight in the Northern Hemisphere. In view of this, the wind heading before a frosty front passes would normally be out of the south or southwest with warm air temperatures. After the cool front passes, the winds would move to out of the west or northwest and the air temperature would relentlessly
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