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Tramuntana

The north wind is strong cold wind coming from the north , polar origin, using the north of the Pyrenees and southwest of Massif French Central as acceleration zone. Its speed has reached 200 km / h. When the wind blows the pure blue sky is usually presented.

As can be seen?: manifests itself in relation to an input stream of cold dry air, the Polar Continental origin. Circumstance or feature that explains their greater frequency / prevalence in the winter months, when anticyclones of Siberia extends to Central Europe promoting the arrival of this cold air current. The current after invaded the Po Valley, about the obstacle force representing the Apennines and bursts violently into the Gulf of Genoa and the Tyrrhenian.

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mistral wind

The mistral or I look is wind from the northwest.

The name comes from Latin Magistrale, "masterful" since it is a dry wind and violent feared by farmers and sailors.

the Catalan Countries occur when the mistral winds from the Atlantic anticyclone dominates the east of the Iberian Peninsula and its northern flank is crossed by a disturbed stream, which crosses the Pyrenees and produces strong winds and cold the valley of the Ebro, which affect the land near the river ports Beseit, delta, Tarragona and center of Aragon.

the Rhone delta (a French river) the mistral wind is Cantabrian northwest blowing when the high pressures of Europe attracted by the low of the Mediterranean narrow channel through the valley of the river winds over the region.

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MIGJORN

The Migjorn (wind from the south or Noon), is the union of a storm centered in Portugal and an anticyclone over Italy, more or less symmetrical. The name refers to Noon the sun's altitude above the horizon when the sun in its daily movement reaches its highest elevation at noon. It is a wind from the African continent, and brings warm, dry air, a characteristic that is displayed particularly in summer, causing a great sensation embarrassment. Rarely reaches force 6. As a general rule appears in combination with its neighbors and Llebeig Xaloc.

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Wind Wind Wind Gregal

Wind Gregal

The gregarious Mediterranean is called the wind from the northeast. This wind is called by the name of gregarious, that comes from Greece, thus justifying the use of that word.

In the gregarious Western Mediterranean in the eastern part of Spain, with rainfall results that differ according to the relief of the country. An example is the stretch of the Alicante coast, around Cape Nao: northeast Denia, the incidence of storms northeast are abundant and time intensive, takes center stage and the two observatories located rainy Valencia. In contrast, modification of coastal path, which is NW-SE direction in the Marina, is home of the gregarious and northeast storms, to the extent that, in less than 50 km, the average annual rainfall of 644 mm falls Denia to Benidorm 345, falling by almost half.

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LEVANTE

The east wind is the name which usually refers to wind from the east on the Mediterranean coast of Spain and, in general, throughout the western Mediterranean.

The wind rises in the central Mediterranean and in the vicinity of the Balearic Islands and reaches its highest speed to cross the Gibraltar Strait. The wind brings clouds and rain to the east side of the Rock of Gibraltar but causes dry weather in the western side of the Strait, especially on the Atlantic coast of Andalusia. This peculiarity makes them well known to local people that they associate it with hot or windy weather. However, in Gibraltar generates particular cloud formations on the Rock. Levante winds may occur at any time of year but are most common from May to October. Its intensity can be very variable but can be very high, precluding Vessels in the exit port of Algeciras.

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southwest wind or llebeig

The Llebeig or Garbi is the name of the southwest wind. At Valencia called llebeig except in Alicante which is known as garbinet , while further north it is called Garbi. By origin, carries much sand and fine dust in suspension from the Sahara Desert .

The llebeig occurs as a result of storms moving the Mediterranean south from west to east, this movement causes the movement of tropical air masses, warm, dry and Sahara dust cover until southeast of the Iberian Peninsula .

llebeig is usually anticipated by the haze (warm mist) that appears on the horizon to the south. The characteristic color of the haze is caused by the large amount of African dust carried.

The appearance of this wind heralds the arrival of the depression that often originates and comes with heavy rains.

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east wind

The Levant is the cardinal point east, and the compass s' also called the east wind that comes from this cardinal point. In the area of \u200b\u200bthe Catalan Countries , the east wind is a moist, since it comes from the sea.

According to Greek mythology , Euro was the personification of the east wind.

Etymologically lift comes from the Latin adjournment, 'that rises. According to another version, would be to remove as it is where does the Sun in equinoxes.

Description
The wind was born in the central Mediterranean and in the vicinity of the Balearic Islands and reached its greatest speed crossing the Gibraltar Strait. The wind brings clouds and rain to the eastern side of the Rock of Gibraltar but dry weather is on the western side of the Strait, especially on the Atlantic coast of Andalusia. This peculiarity makes them well known by the inhabitants of the place that you associate yourself mps hot or windy. However Gibraltar generates individual cloud formations in the rock. Levante winds can occur anytime of year but are most common from May to October. Its intensity can be highly variable but can be very high, thus preventing the departure of ships port of Algeciras.

Weather Source
During the summer, the home shops sunshine often generate a low temperature (B) on the northwest of Africa, just over the ridge of the Atlas. This low pressure between 1005 and 1010 millibar comes into conflict with the anticyclone of the Azores, the more strengthened in summer periods, and located north of the archipelago. This combination creates winds clockwise against the Low Pressure (east wind at its north) on m editerrània western. Alongside the pressure source, adding the local effect of the Strait of Gibraltar, which magnifies his strength and speed just in this area.

dryness in western Andalusia is due to the Foehn effect produced by the foothills of the western Betic mountains.