Which type of precipitation is more oceanic or Mediterranean?

The oceanic climate has a lot of precipitation, and the rainfall is abundant and evenly distributed throughout the year, taking London precipitation as an example (1 December, unit: mm).

Take the number of rainy days in London as an example (1 December, unit: days):

Comparison between the two: warm in winter and cool in summer, small annual temperature difference: the closer to the ocean in the oceanic climate zone, the stronger the oceanic climate.

Especially in winter, because there is a warm current along the coast, the westerly wind blows from the warm current and the sea, and the air flow is warm and humid, so the winter temperature is much warmer than that of the center of the continent and the east coast of the continent at the same latitude. The average temperature of the coldest month is above 0. In summer, the warm water temperature is still lower than that of the mainland, and the sea is much cooler than the land, and the average temperature of the hottest month here is below 22 due to the westerly wind.

Due to the warm winters and cool summers, the annual temperature difference is much smaller than in other regions at the same latitude. Rain throughout the year, more rain in winter: This area is on the path of extratropical cyclone activity, and cyclone rainfall is abundant, especially in winter, when extratropical cyclones are more active, with many rainy days, but the intensity of precipitation is not large.

Winter precipitation accounts for a slightly larger proportion of the year, and there is no dry season throughout the year.

Mediterranean climate, controlled by the subtropical high pressure zone in summer, the water temperature of the Mediterranean Sea is lower than that of the land to form high pressure, which increases the influence of the subtropical high pressure zone, and the water temperature of the Mediterranean Sea is relatively high in winter, forming a low pressure, attracting the west wind, and greatly strengthening the power of the west wind The climate is characterized by hot and dry summer, high temperature and little rain, and mild and rainy winter. The temperature is 5 10 in winter and 21 27 in summer. The annual precipitation is about 350 900 mm, concentrated in winter, and the precipitation in the second half of the year accounts for only 20 40 per cent of the annual precipitation, and the maximum monthly precipitation is more than three times that of the minimum monthly precipitation.

The oceanic climate is more prevalent, because both regions are affected by the westerly wind belt in winter and have abundant precipitation, while the Mediterranean climate is affected by the subtropical high in summer, and the precipitation is less than that of the temperate oceanic climate, which is still affected by the westerly wind belt in summer.

Tropical oceans? Temperate oceans? The landlord should ask about the temperate marine and Mediterranean climate. Let's give an example:

The annual Roman precipitation in the central Apennine Peninsula is:

The annual rainfall in Caramé on the Peloponnese Peninsula in the southern Balkans is 840 mm, and cyclone activity is frequent and precipitation is high in Western Europe, with annual precipitation above 1000 mm in the western British Isles and 2000 mm or more off the western coast of Scotland. In other areas, it is mostly 600-1000mm.

Overall, there is more precipitation in temperate oceanic climates.

Mediterranean climate: hot and dry summers with high temperatures and little rainfall, mild and humid winters.

Temperate oceanic climate: no severe cold in winter, no scorching heat in summer, and the annual and diurnal temperature differences are small. There is precipitation throughout the year, with more in autumn and winter.

So in contrast, it should be an oceanic climate with more precipitation.

The Mediterranean climate is characterized by hot, dry summers and mild and rainy winters. It is located on the west coast of the continent at subtropical latitudes, between latitude and about 30° 40°, and includes the Mediterranean coast, the coast of California in the United States, the central coast of Chile in South America, the southern tip of South Africa, and the southern tip of Australia.

It is located in a transitional zone between a tropical semi-arid climate and a temperate oceanic climate. These areas are significantly affected by the seasonal displacement of the pressure zone, and in summer, they are controlled by the subtropical high pressure, and the airflow sinks, so except for the western coast of the mainland affected by the cold current, the summer temperature is very hot, and the sinking airflow is not conducive to clouds and rain, so the climate is dry. Winters are influenced by westerly winds, and are mild and humid. Rainfall is moderate throughout the year, with annual precipitation ranging from 300 to 1,000 mm, mainly concentrated in winter.

Temperate oceanic climate: characterized by mild and rainy year-round.

It is located on the west coast of the mainland, at 40° 60° north latitude. It is in the westerly wind belt all the year round, deeply affected by the ocean air mass, and there is a warm current passing through the coast, there is no severe cold in winter, there is no scorching heat in summer, the average temperature of the coldest month is above 0, the hottest month is below 22, and the annual and daily temperature range is small. There is precipitation throughout the year, more in autumn and winter, with annual precipitation of more than 1,000 mm, and in the windward slopes of the mountains it can reach more than 2,000 to 3,000 mm.

This climate is most typical in Western Europe and has the largest distribution, and is also found in the corresponding latitudes on the west coast of the South and North American continents, as well as in Tasmania and New Zealand in Oceania.

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Analysis: The distribution of the Mediterranean climate is located on the west coast of the continent between 30 and 40 degrees north and south latitudes. The Mediterranean climate is most pronounced along the Mediterranean coast.

Other regions include the coast of California in North America, central Chile in South America, the Cape of Good Hope region at the southern tip of Africa, and the southwest coast of Australia.

The Mediterranean climate is characterized by a mild climate controlled by westerly winds in winter, with an average temperature of 4 10 in the coldest month and abundant precipitation. In summer, under the control of the subtropical high pressure, the air flow sinks, and the climate is hot and dry, with few clouds and abundant sunshine.

The annual precipitation is 300 1000 mm, accounting for about 60 70 in the winter half year and only 30 40 in the summer half of the year. Climatic characteristics of winter rain and summer dryness.

It has a temperate oceanic climate, located on the west coast of the continent, at 40° and 60° north latitudes. It is in the westerly wind belt all the year round, deeply affected by the ocean air mass, and there is a warm current along the coast, there is no severe cold in winter, there is no scorching heat in summer, the average temperature of the coldest month is above 0, the hottest month is below 22, and the temperature is small every year and day. Precipitation occurs throughout the year, with more precipitation in autumn and winter, with annual precipitation of more than 1,000 mm.

This climate is most typical in Western Europe and has the largest distribution area, and is also found in the corresponding latitudes on the west coast of the South and North American continents, as well as in Tasmania and New Zealand in Oceania.

The main differences between a Mediterranean climate and a temperate oceanic climate are distribution, genesis, precipitation and temperature variations.

1.The distribution is different: the Mediterranean climate is distributed on the west coast of the continent at latitudes 30° to 40°N, and the temperate oceanic climate is distributed on the west coast of the continent at 40° to 60°N.

2.The reasons for its formation are different: the Mediterranean climate is formed by the alternating control of the subtropical high pressure zone and the westerly wind belt, with hot and dry summers and mild and rainy winters; The temperate oceanic climate is controlled by the westerly wind belt throughout the year, and under the influence of the marine air mass, Zheng Sulxian is warm and humid all year round, and there are many rainy days.

3.The characteristics of precipitation are different: the Mediterranean climate is a winter rain type, with hot and dry summers and mild and rainy winters; The temperate oceanic climate is of the annual rain type, with mild and rainy throughout the year.

4.The temperature changes differently: the Mediterranean climate is hot and dry in summer under the control of the subtropical high pressure belt, and mild and humid in winter under the influence of the westerly wind belt; The temperate oceanic climate is controlled by westerly winds throughout the year and is mild and rainy.

In summary, the main differences between the Mediterranean climate and the temperate oceanic climate are distribution, genesis, precipitation and temperature changes.