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The Mistral in France is a fresh or cold, often violent, and usually dry wind, blowing throughout the year but is most frequent in winter and spring. A santon is a small hand-painted figurine cast in Terracotta or a similar material that is used for building Nativity scenes Santons are a traditional product This article is about the country For a topic outline on this subject see List of basic France topics. Wind is the flow of Air or other Gases that compose an Atmosphere (including but not limited to the Earth's) It blows from the northwest or north of Europe through the valley of the Rhône River to the Mediterranean. The Rhone, or the Rhône is one of the major Rivers of Europe, running through Switzerland and France. [1] It also affects the whole of Sardinia in Italy. Sardinia (sɑrˈdɪnɪə Sardegna Sardigna or Sardinnya is the second-largest island in the Mediterranean Sea (after Sicily) Italy (Italia officially the Italian Republic, (Repubblica Italiana is located on the Italian Peninsula in Southern Europe, and on the two largest
In the south of France the name comes from the Languedoc dialect of the provençal language and means "masterly. Languedoc ( in French Lengadòc in Occitan) is a former Province of France, now continued in the modern-day ''régions'' of Languedoc-Roussillon Provençal ( Provençau) is one of several dialects of Occitan spoken by a minority of people mostly in Provence (in southern France " The same wind is called mistrau in the occitan language, mestral in Catalan and maestrale in Italian and Corsican. Occitan ( IPA BrE: /ˈɒksɪtn/ AmE: /ˈɑksəˌtɑn/ known also as Lenga d'òc or Langue d'oc (native name occitan Italian ( or lingua italiana) is a Romance language spoken by about 63 million people as a First language, primarily in Italy. Corsican ( Corsu or Lingua Corsa) is a Romance language spoken and written on the islands of Corsica ( France) and northern Sardinia
The mistral is usually accompanied by clear and sunny weather, and it plays an important role in creating the climate of Provence. It can reach speeds of more than ninety kilometers an hour, particularly in the Rhone Valley.
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The mistral is an example of a katabatic wind, which is created by the difference in pressure between the cold air of a high pressure system over the Atlantic or northwest Europe and a low pressure system over the Gulf of Lion or the Gulf of Genoa in the Mediterranean. A katabatic wind, from the Greek word katabatikos meaning "going downhill" is the technical name for a drainage Wind, a wind A high pressure area (also called a high or high-pressure is a region where the Atmospheric pressure is greater than surrounding areas A low pressure area, or " low " is a region where the Atmospheric pressure is lower in relation to the surrounding area The Gulf of Lion (French Golfe du Lion is a wide Embayment of the Mediterranean coastline of Languedoc-Roussillon and Provence in The Gulf of Genoa ( Golfo di Genova) is the northernmost part of the Ligurian Sea. The high-pressure air flows south through the Rhone Valley, gathering speed as it is funneled between the Alps and the Massif Central. The Massif Central ( Occitan: Massís Central / Massís Centrau) is an elevated region in south-central France, consisting of Mountains and
In France, the mistral particularly affects Provence, Languedoc east of Montpellier, and the department of the Var to the west of Frejus, as well as all of the Rhone Valley from Lyon to Marseille as far as Corsica and Sardinia. Provence ( Provençal Occitan: Provença in classical norm or Prouvènço in Mistralian norm is a region of southeastern France Languedoc ( in French Lengadòc in Occitan) is a former Province of France, now continued in the modern-day ''régions'' of Languedoc-Roussillon Montpellier ( Occitan Montpelhièr) is a City in the south of France. Fréjus can also refer to the Fréjus Road Tunnel and the Fréjus Rail Tunnel in the Alps ||-||} Lyon, also known as Lyons in English is a city in east-central France. Marseille, ( English alt Marseilles mɑrˈseɪ — French: maʁsɛj locally — Provençal Occitan: Marselha maʀˈsijɔ The mistral usually blows from northwest or north, but in certain pre-alpine valleys and along the Cote d'Azur, the wind is channelled by the mountains so that it blows from east to west. The French Riviera (Côte d'Azur Occitan: Còsta Azzura) is one of the most famous resort areas in the world extending along the Mediterranean Sea west Sometimes it also blows from the north-north-east toward the east of Languedoc as far as Cap Béar. Frequently the mistral will affect only one part of the region, particularly when it is not caused by a flow of air from the northwest.
The mistral and the similar north wind in France, the tramontane, usually originate with a flow of air from the northwest. Tramontane ( Tramuntana, Tramontana) is a classical name for a northern wind A cold front associated with a low pressure area over northern Europe moves toward the east. The flow shifts to the northwest, bringing with it cold maritime air. The cool wind from the northeast dries the air and rapidly disperses the clouds. The acceleration of the wind is caused by the creation of a depression, or low-pressure area, in the Gulf of Genoa under the wind from the Alps. In this case the mistral affects the entire Rhone Valley, the inland territory of Provence and the Cote d'Azur, where the wind comes from the east.
In the Languedoc area, where the tramontane is the strongest wind, the mistral and the tramontane blow together onto the Gulf of Lion and the northwest of the western Mediterranean, and can be felt to the east of the Balearic Islands, in Sardinia, and sometimes as far as the coast of Africa. The Balearic Islands ( Catalan and official Illes Balears; Spanish: Islas Baleares) are an Archipelago in the western Mediterranean Sardinia (sɑrˈdɪnɪə Sardegna Sardigna or Sardinnya is the second-largest island in the Mediterranean Sea (after Sicily)
When the mistral originates from the west, the mass of air is not so cold and the wind only affects the plain of the Rhone delta and the Cote d'Azur. The good weather is confined to the coast of the Mediterranean, while it can rain in the interior. The Cote d'Azur generally has a clear sky and warmer temperatures, the classic effect of this type of Foehn Wind. A foehn wind or föhn wind is a type of dry downslope wind which occurs in the lee of a mountain range This type of mistral usually blows for no more than one to three days.
The mistral originating from the northeast has a very different character; it is felt only in the west of Provence and as far as Montpellier, with the wind coming from either a northerly or north-northeasterly direction. In the winter this is by far the coldest form of the mistral, when it carries chill air from Central Europe and from Russia. It is caused by the presence of a high pressure area over northern Europe. The wind can blow for more than a week, until the high pressure area has moved east and the wind changes direction. This kind of mistral is often connected with a low pressure area in the Gulf of Genoa, and it can bring unstable weather to the Cote d'Azur and the east of Provence, sometimes bringing heavy snow to low altitudes in winter.
When the flow of air comes from the northeast due to a widespread low pressure area over the Atlantic and atmospheric disturbances over France, the air is even colder at both high altitudes and ground level, and the mistral is even stronger, and the weather worse, with the creation of cumulus clouds bringing weak storms. This kind of mistral is weaker in the east of of Provence and the Cote d'Azur.
The mistral is not always synonymous with clear skies. When a low pressure front over the Mediterranan approaches the coast from the southeast, the weather can change quickly for the worse, and the mistral and its clear sky changes rapidly to an east wind bringing humid air and threatening clouds. The position of the low-pressure front creates a flow of air from the northwest or the northeast. chanelled through the Rhone Valley. If this low-pressure area moves back toward the southeast, the mistral will quickly clear the air and the good weather will return; but if the cold-weather front continues to approach the land, bad weather will continue for several days in the entire Mediterranean basin, sometimes transforming into what French meteorologists call an épisode cévenol, a succession of torrential rains and floods, particularly in the areas west of the Rhone Valley: the Ardèche, the Gard, Herault and Lozère. Ardèche ( Occitan and Arpitan: Ardecha) is a department in south-central France named after the Ardèche River. Gard ( Occitan: Gard) is a département located in southern France in the Languedoc-Roussillon region Hérault ( Occitan: Erau) is a department in the southwest of France named after the Hérault river. Lozère (in Occitan Losera) is a department in southeast France near the Massif Central.
The summer mistral, unlike the others, is created by purely local conditions. It usually happens in July, and only in the valley of the Rhone and on the coast of Provence. It is caused by a thermal depression over the interior of Provence (The Var and Alpes de Haute-Provence), created when the land is overheated. This creates a flow of air from the north toward the east of Provence. This wind is frequently cancelled out close to the coast by the breezes from the sea. It does not blow for more than a single day, but it is feared in Provence, because it dries the vegetation and it can spread forest fires
The mistral is a dry wind, and its arrival almost always clears the skies and dries the air. The Mistral helps explain the unusually sunny climate (2700 to 2900 hours of sunshine a year) and clarity of the air of Provence. When other parts of France have clouds and storms, Provence is rarely affected for long, since the mistral quickly clears the sky. In less than two hours, the sky can change from completely covered to completely clear. The mistral also blows away the dust, and makes the air particularly clear, so that during the mistral it is possible to see mountains 150 kilometers and farther away.
The mistral has the reputation of bringing good health, since the dry air dries stagnant water and the mud, giving the mistral the local name mange-fange (eng. "mud-eater. ") It also blows away pollution from the skies over the large cities and industrial areas.
The sunshine and dryness brought by the mistral have an important effect on the local vegetation. The vegetation in Provence, which is already dry because of the small amount of rainfall, is made even drier by the wind, which makes it particularly susceptible to fires, which the wind spreads very rapidly, sometimes devastating vast expanses of mountainside before being extinguished. During the summer, thousands of hectares can burn when the mistral is blowing.
In the Rhone Valley and on the plain of la Crau, the regularity and force of the mistral causes the trees to grow leaning to the south. Once the forest has been razed by fire, the strong wind makes it difficult for new trees to grow. The farmers of the Rhone Valley have long planted rows of cypress trees to shelter their crops from the dry force of the mistral. The mistral can also have beneficial effects- the moving air can save crops from the spring frost, which can last until the end of April.
As summer visitors to the beach in Provence learn, the summer mistral can quickly lower the temperature of the sea, as the wind pushes the warm water near the surface out to sea and it is replaced by colder water from greater depths.
The mistral can effect the weather in North Africa, Sicily and Malta or throughout the Mediterranean, particularly when low pressure areas form in the Gulf of Genoa. North Africa or Northern Africa is the Northernmost Region of the African Continent, separated by the Sahara from Sub-Saharan Sicily ( Italian and Sicilian: Sicilia) is an autonomous region of Italy. Malta, officially the Republic of Malta (Repubblika ta' Malta is a European Microstate, comprising an Archipelago of three islands A low pressure area, or " low " is a region where the Atmospheric pressure is lower in relation to the surrounding area The Gulf of Genoa ( Golfo di Genova) is the northernmost part of the Ligurian Sea.
The same name is used for the cool North/North-West wind in the Adriatic Sea. This is also a katabatic wind and has similar causes as its French namesake - air cooled over the Dinaric Alps flows down into the Adriatic sea, where it is known as Maestro or Maestral. The Dinaric Alps or Dinarides ( Croatian and Bosnian: Dinarsko gorje or Dinaridi, Alpet Dinaride Maestro or maestral is a northwesterly wind which blows in summer in the Adriatic when pressure is low over the Balkan peninsula
In south-western Crete it is known as Maestro and it is considered the most beneficial wind, which is said to blow only during the daytime.
The Mistral plays an important part in the life and culture of Provence, The Mas (Provencal Farmhouse) traditionally faces south, with its back to the Mistral. A Mas (pronounced 'mah' is a traditional farmhouse in the Provence region of France. The bell towers of villages in Provence are often open iron frameworks, which allow the wind to pass through. The traditional Provençal Christmas crib often has a figure of a shepherd holding his hat, with his cloak blowing in the Mistral. A nativity scene may be used to describe any depiction of the Nativity of Jesus in art, but in the sense covered here also called a crib or manger in the