Bompas is a commune in the Pyrénées-Orientales department in southern France. Bompas is located in the arrondissement of Perpignan. Communes of the Pyrénées-Orientales department INSEE commune file
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravity. The main forms of precipitation include drizzle, sleet, snow and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor, so that the water condenses and "precipitates", thus and mist are not precipitation but suspensions, because the water vapor does not condense sufficiently to precipitate. Two processes acting together, can lead to air becoming saturated: cooling the air or adding water vapor to the air. Precipitation forms as smaller droplets coalesce via collision with other rain drops or ice crystals within a cloud. Short, intense periods of rain in scattered locations are called "showers."Moisture, lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into clouds and rain. This process is active when freezing rain occurs. A stationary front is present near the area of freezing rain and serves as the foci for forcing and rising air.
Provided necessary and sufficient atmospheric moisture content, the moisture within the rising air will condense into clouds, namely stratus and cumulonimbus. The cloud droplets will grow large enough to form raindrops and descend toward the Earth where they will freeze on contact with exposed objects. Where warm water bodies are present, for example due to water evaporation from lakes, lake-effect snowfall becomes a concern downwind of the warm lakes within the cold cyclonic flow around the backside of extratropical cyclones. Lake-effect snowfall can be locally heavy. Thundersnow is possible within lake effect precipitation bands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation. On the leeward side of mountains, desert climates can exist due to the dry air caused by compressional heating. Most precipitation is caused by convection; the movement of the monsoon trough, or intertropical convergence zone, brings rainy seasons to savannah climes.
Precipitation is a major component of the water cycle, is responsible for depositing the fresh water on the planet. 505,000 cubic kilometres of water falls as precipitation each year. Given the Earth's surface area, that means the globally averaged annual precipitation is 990 millimetres, but over land it is only 715 millimetres. Climate classification systems such as the Köppen climate classification system use average annual rainfall to help differentiate between differing climate regimes. Precipitation may occur on other celestial bodies, e.g. when it gets cold, Mars has precipitation which most takes the form of frost, rather than rain or snow. Precipitation is a major component of the water cycle, is responsible for depositing most of the fresh water on the planet. 505,000 km3 of water falls as precipitation each year, 398,000 km3 of it over the oceans. Given the Earth's surface area, that means the globally averaged annual precipitation is 990 millimetres. Mechanisms of producing precipitation include convective and orographic rainfall.
Convective processes involve strong vertical motions that can cause the overturning of the atmosphere in that location within an hour and cause heavy precipitation, while stratiform processes involve weaker upward motions and less intense precipitation. Precipitation can be divided into three categories, based on whether it falls as liquid water, liquid water that freezes on contact with the surface, or ice. Mixtures of different types of precipitation, including types in different categories, can fall simultaneously. Liquid forms of precipitation include drizzle. Rain or drizzle that freezes on contact within a subfreezing air mass is called "freezing rain" or "freezing drizzle". Frozen forms of precipitation include snow, ice needles, ice pellets and graupel; the dew point is the temperature to which a parcel must be cooled in order to become saturated, condenses to water. Water vapor begins to condense on condensation nuclei such as dust and salt in order to form clouds. An elevated portion of a frontal zone forces broad areas of lift, which form clouds decks such as altostratus or cirrostratus.
Stratus is a stable cloud deck which tends to form when a cool, stable air mass is trapped underneath a warm air mass. It can form due to the lifting of advection fog during breezy conditions. There are four main mechanisms for cooling the air to its dew point: adiabatic cooling, conductive cooling, radiational cooling, evaporative cooling. Adiabatic cooling occurs when air expands; the air can rise due to convection, large-scale atmospheric motions, or a physical barrier such as a mountain. Conductive cooling occurs when the air comes into contact with a colder surface by being blown from one surface to another, for example from a liquid water surface to colder land. Radiational cooling occurs due to the emission of infrared radiation, either by the air or by the surface underneath. Evaporative cooling occurs when moisture is added to the air through evaporation, which forces the air temperature to cool to its wet-bulb temperature, or until it reaches saturation; the main ways water vapor is added to the air are: wind convergence into areas of upward motion, precipitation or virga falling from above, daytime heating evaporating water from the surface of oceans, water bodies or wet lan
La Cabanasse is a commune in the Pyrénées-Orientales department in southern France. La Cabanasse is located in the arrondissement of Prades. Communes of the Pyrénées-Orientales department INSEE
Departments of France
In the administrative divisions of France, the department is one of the three levels of government below the national level, between the administrative regions and the commune. Ninety-six departments are in metropolitan France, five are overseas departments, which are classified as regions. Departments are further subdivided into 334 arrondissements, themselves divided into cantons; each department is administered by an elected body called a departmental council. From 1800 to April 2015, these were called general councils; each council has a president. Their main areas of responsibility include the management of a number of social and welfare allowances, of junior high school buildings and technical staff, local roads and school and rural buses, a contribution to municipal infrastructures. Local services of the state administration are traditionally organised at departmental level, where the prefect represents the government; the departments were created in 1790 as a rational replacement of Ancien Régime provinces with a view to strengthen national unity.
All of them were named after physical geographical features, rather than after historical or cultural territories which could have their own loyalties. The division of France into departments was a project identified with the French revolutionary leader the Abbé Sieyès, although it had been discussed and written about by many politicians and thinkers; the earliest known suggestion of it is from 1764 in the writings of d'Argenson. They have inspired similar divisions in some of them former French colonies. Most French departments are assigned a two-digit number, the "Official Geographical Code", allocated by the Institut national de la statistique et des études économiques. Overseas departments have a three-digit number; the number is used, for example, in the postal code, was until used for all vehicle registration plates. While residents use the numbers to refer to their own department or a neighbouring one, more distant departments are referred to by their names, as few people know the numbers of all the departments.
For example, inhabitants of Loiret might refer to their department as "the 45". In 2014, President François Hollande proposed to abolish departmental councils by 2020, which would have maintained the departments as administrative divisions, to transfer their powers to other levels of governance; this reform project has since been abandoned. The first French territorial departments were proposed in 1665 by Marc-René d'Argenson to serve as administrative areas purely for the Ponts et Chaussées infrastructure administration. Before the French Revolution, France gained territory through the annexation of a mosaic of independent entities. By the close of the Ancien Régime, it was organised into provinces. During the period of the Revolution, these were dissolved in order to weaken old loyalties; the modern departments, as all-purpose units of the government, were created on 4 March 1790 by the National Constituent Assembly to replace the provinces with what the Assembly deemed a more rational structure.
Their boundaries served two purposes: Boundaries were chosen to break up France's historical regions in an attempt to erase cultural differences and build a more homogeneous nation. Boundaries were set so that every settlement in the country was within a day's ride of the capital of a department; this was a security measure, intended to keep the entire national territory under close control. This measure was directly inspired by the Great Terror, during which the government had lost control of many rural areas far from any centre of government; the old nomenclature was avoided in naming the new departments. Most were named after other physical features. Paris was in the department of Seine. Savoy became the department of Mont-Blanc; the number of departments 83, had been increased to 130 by 1809 with the territorial gains of the Republic and of the First French Empire. Following Napoleon's defeats in 1814–1815, the Congress of Vienna returned France to its pre-war size and the number of departments was reduced to 86.
In 1860, France acquired the County of Nice and Savoy, which led to the creation of three new departments. Two were added from the new Savoyard territory, while the department of Alpes-Maritimes was created from Nice and a portion of the Var department; the 89 departments were given numbers based on the alphabetical order of their names. The department of Bas-Rhin and parts of Meurthe, Moselle and Haut-Rhin were ceded to the German Empire in 1871, following France's defeat in the Franco-Prussian War. A small part of Haut-Rhin became known as the Territoire de Belfort; when France regained the ceded departments after World War I, the Territoire de Belfort was not re-integrated into Haut-Rhin. In 1922, it became France's 90th department; the Lorraine departments were not changed back to their original boundaries, a new Moselle department was created in the regaine
Bages is a commune in the Pyrénées-Orientales department in southern France. Bages is located in the arrondissement of Perpignan. Communes of the Pyrénées-Orientales department INSEE
Bourg-Madame is a commune in the Pyrénées-Orientales department in southern France. Bourg-Madame is located in the arrondissement of Prades, it lies right on the border with Spain. It abuts directly onto the Spanish town of Puigcerdà, is near the Spanish exclave of Llívia; the town used to be known in French as Les Guinguettes, until 1815 when it was renamed Bourg-Madame in honour of the wife of the Duke of Angoulême. The Catalan name for the town is still the traditional one; the following major roads lead to Bourg-Madame: N-20 from Ur to the north. Bourg-Madame is located at a key point of intersection for railways that link Toulouse and Valencia; the railway station is located in the Arena district. The commune is twinned with: Vespella de Gaià, Spain Communes of the Pyrénées-Orientales department INSEE commune file
Banyuls-dels-Aspres is a commune in the Pyrénées-Orientales department in southern France. Banyuls-dels-Aspres is located in the arrondissement of Céret; the inhabitants are called Banyulencs. Saint-Andrew church, first mentioned in 1091 but rebuilt in the 15th century. Henri Ey: psychiatrist and philosopher born in Banyuls-dels-Aspres. Communes of the Pyrénées-Orientales department INSEE statistics INSEE commune file