interactions between the atmosphere of warmth and sun is a never-ending and is always a constant. Every part of the atmosphere is not heated equivalent at the same time. This is equivalent to the large mass of air to move, like an automatic response of the atmosphere around him. The many types of weather are a direct consequence of this mass movement of air.
The existing air mass in a region may occur, which are already there, if another air mass moves customs front, the border between these two air masses. Cold front, when the cold air replaces the warm air and cold front will be replaced if it is known as a warm front.
A cold air mass, when a warm front, colder air pushing under the warm front. Condensed water vapor in clouds changes when the warm front rises and cools. Appearance of the clouds follows the mid-high cirrus clouds. Mid-level cloud, followed by thick stratus clouds. Precipitation and wind come on.
Weather cold fronts often produce larger fluctuations of nature. The mass of warm air move upwards when it is combined with a cold front. Convection and instability results because of this strong uptrend. On the front towers and trigger the formation of large cumulus clouds. An area of strong winds and low pressure zone is created due to the rapid rise in the air. The real front is accompanied by strong winds and heavy rain. After frontal passage, the persistent showers.
In times of a cold front moving slowly overtaken generally warm front. The warm up is pressed against the cold, if that happens. An occluded front is the line that in-between the two fronts, as they continue to move together. Light stratus clouds and precipitation generally accompany the occluded fronts.
A stagnation is formed when two air masses, but not strong enough to replace and the other meet. Precipitation over a long period due to cloud cover through this stagnant situation. This stagnation can be as warm front or cold front begin to move, or after a few days in May dispel. In summer, the chances of the occurrence of such stagnant fronts are higher.
More than 70% of the earth's surface is protected by the oceans. Country is not cool or heat up as fast as the water surface and thus heat efficiently in seawater. Due to this characteristic cold or warm water to the various parts of the world by ocean currents. The temperature of the currents under the influence of temperatures on the surface. Changes in the temperature of the ocean climate change. It concerns more effectively, the climate of the coastal region.
In the few weeks around the summer and winter solstice, the maximum and minimum temperatures sea legs because of the slow heating and cooling nature of water. The weather is determined by the variation in maritime and land transport elevated temperatures, is due to this delay. As a result, large parts of the surface water can fog and the weather in the coastal region could be cooler.
In the air will be condensed water vapor cloud, which eventually falls as precipitation on the surface. The whole process starts all again, because most of it goes back to the oceans after a small part of the snow and rain. So next time you rent a car from Murcia airport and it starts to rain, you know, the whole natural process, the weather pattern.
His special interest in Moraira, Eric Slarkowski handled many detailed text in this field. You can see his articles on Murcia airport car rental at many different sources for Murcia airport car rental news.
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