What is the marine climate?
The sea climate, also known as the ocean climate, the naval climate or the climate of the sea west coast, is a slight climate that exists on the west coast of continents. These climate usually occur between geographical widths of 45 ° and 55 °, although in Western Europe it extends further north. They are characterized by slight weather, even the level of precipitation and a narrow annual temperature range. The conditions in these regions vary depending on location and topography. These areas show a narrower deviation of the annual temperature than the areas that receive winds coming on the ground. The alleviating effect of large water bodies on temperatures is due to high specific water heat: increased temperature of a certain amount of water requires more energy than the equivalent of air or soil. Therefore, temperatures above the oceans do not roll wide.
In some cases, warm ocean currents have mitigating the effect on the temperature of nearby soil, which helps to create a marine climate. An example of this effect can be seen in the Gulf stream, the mainstream in the Atlantic Ocean, which carries hot water north along the coast of North America and to Western Europe. Meteorologists believe that the climate of Western Europe is warmer than it would otherwise be caused by the effects of the Persian Gulf.
Theocean Air carries moisture, so that the marine climatic areas have constant precipitation during the year, along with a heavy clouds and high humidity. Snowfall is also common in these areas in winter. Although the marine climate does not have a fully dry period, some show a trend in the summer.
Mountain Ranges have a major impact on how the sea climate is scattered on the ground. In North and South America, mountain zones often take place from north to south, which effectively blocks Westerlies and Ocean air. This causes the marine climate region to spread in narrow bands up and down the coast. In Europe, on the other side, mountain zones running from the educationalThe west feast allow the ocean air to penetrate inland and create a large marine climate on most of the continent.
In addition to the slight climate found in the middle latitudes, there are other varieties in higher and lower latitudes. Some areas in the subpolar regions show characteristics of the marine climate, which makes them subpolar ocean climate. The term subtropical highlands is used to indicate regions that have a marine climate due to the cooling effects of high height, but are located in lower latitudes, in the tropics.