Akhfennir
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Akhfennir
Akhfennir is a small town in Tarfaya Province, in the Laâyoune-Sakia El Hamra region of Morocco. The area is noted for Khenifiss National Park and Tarfaya-Akhfenir Wind Farm. Climate and Weather Condition in Akhfennir In Akhfennir, the Summer, summer seasons are warm, Humidity, muggy, and arid; the Winter, winter seasons are short, cool, and dry; and it is windy and mostly clear year round. Over the year, the temperature typically changes from 55 °F to 81 °F and is rarely below 51 °F or above 89 °F. Rainfall The rainy period starts from November 18 to March 1, and lasts for 3.5 months of the year, with a sliding 31-day rainfall of at least 0.5 inches. The month with the highest rain in Akhfennir is February, with an average rainfall of 0.6 inches. The rainless period of the year lasts for 8.6 months, from March 1 to November 18. The month with the least rain in Akhfennir is June, with an average rainfall of 0.0 inches. Average temperature The warm se ...
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Regions Of Morocco
Regions are currently the highest administrative divisions in Morocco. Since 2015, Morocco officially administers 12 regions, including one (Dakhla-Oued Ed-Dahab) that lies completely within the disputed territory of Western Sahara and two (Laâyoune-Sakia El Hamra and Guelmim-Oued Noun) that lie partially within it. The regions are subdivided into a total of 75 second-level administrative divisions, which are Prefectures and provinces of Morocco, prefectures and provinces. A region is governed by a directly elections in Morocco, elected regional council. The president of the council is responsible for carrying out the council's decisions. Prior to the 2011 Moroccan constitutional referendum, 2011 constitutional reforms, this was the responsibility of the Wali, the representative of the central government appointed by the King, who now plays a supporting role in the administration of the region. Regions since 2015 On 3 January 2010, the Moroccan government established the Con ...
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Humidity
Humidity is the concentration of water vapor present in the air. Water vapor, the gaseous state of water, is generally invisible to the human eye. Humidity indicates the likelihood for precipitation, dew, or fog to be present. Humidity depends on the temperature and pressure of the system of interest. The same amount of water vapor results in higher relative humidity in cool air than warm air. A related parameter is the dew point. The amount of water vapor needed to achieve saturation increases as the temperature increases. As the temperature of a parcel of air decreases it will eventually reach the saturation point without adding or losing water mass. The amount of water vapor contained within a parcel of air can vary significantly. For example, a parcel of air near saturation may contain 28 g of water per cubic metre of air at , but only 8 g of water per cubic metre of air at . Three primary measurements of humidity are widely employed: absolute, relative, and specific. Ab ...
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Precipitation
In meteorology, precipitation is any product of the condensation of atmospheric water vapor that falls under gravitational pull from clouds. The main forms of precipitation include drizzle, rain, sleet, snow, ice pellets, graupel and hail. Precipitation occurs when a portion of the atmosphere becomes saturated with water vapor (reaching 100% relative humidity), so that the water condenses and "precipitates" or falls. Thus, fog and mist are not precipitation but colloids, because the water vapor does not condense sufficiently to precipitate. Two processes, possibly 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 that is lifted or otherwise forced to rise over a layer of sub-freezing air at the surface may be condensed into ...
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Snow
Snow comprises individual ice crystals that grow while suspended in the atmosphere—usually within clouds—and then fall, accumulating on the ground where they undergo further changes. It consists of frozen crystalline water throughout its life cycle, starting when, under suitable conditions, the ice crystals form in the atmosphere, increase to millimeter size, precipitate and accumulate on surfaces, then metamorphose in place, and ultimately melt, slide or sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes nucleate around particles in the atmosphere by attracting supercooled water droplets, which freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns and rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow metamorphoses, by sintering, sublimation and freeze-thaw. Where the climate is co ...
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Rain
Rain is water droplets that have condensed from atmospheric water vapor and then fall under gravity. Rain is a major component of the water cycle and is responsible for depositing most of the fresh water on the Earth. It provides water for hydroelectric power plants, crop irrigation, and suitable conditions for many types of ecosystems. The major cause of rain production is moisture moving along three-dimensional zones of temperature and moisture contrasts known as weather fronts. If enough moisture and upward motion is present, precipitation falls from convective clouds (those with strong upward vertical motion) such as cumulonimbus (thunder clouds) which can organize into narrow rainbands. In mountainous areas, heavy precipitation is possible where upslope flow is maximized within windward sides of the terrain at elevation which forces moist air to condense and fall out as rainfall along the sides of mountains. On the leeward side of mountains, desert climates can exi ...
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Temperature
Temperature is a physical quantity that expresses quantitatively the perceptions of hotness and coldness. Temperature is measured with a thermometer. Thermometers are calibrated in various temperature scales that historically have relied on various reference points and thermometric substances for definition. The most common scales are the Celsius scale with the unit symbol °C (formerly called ''centigrade''), the Fahrenheit scale (°F), and the Kelvin scale (K), the latter being used predominantly for scientific purposes. The kelvin is one of the seven base units in the International System of Units (SI). Absolute zero, i.e., zero kelvin or −273.15 °C, is the lowest point in the thermodynamic temperature scale. Experimentally, it can be approached very closely but not actually reached, as recognized in the third law of thermodynamics. It would be impossible to extract energy as heat from a body at that temperature. Temperature is important in all fields of natur ...
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Winter
Winter is the coldest season of the year in polar and temperate climates. It occurs after autumn and before spring. The tilt of Earth's axis causes seasons; winter occurs when a hemisphere is oriented away from the Sun. Different cultures define different dates as the start of winter, and some use a definition based on weather. When it is winter in the Northern Hemisphere, it is summer in the Southern Hemisphere, and vice versa. In many regions, winter brings snow and freezing temperatures. The moment of winter solstice is when the Sun's elevation with respect to the North or South Pole is at its most negative value; that is, the Sun is at its farthest below the horizon as measured from the pole. The day on which this occurs has the shortest day and the longest night, with day length increasing and night length decreasing as the season progresses after the solstice. The earliest sunset and latest sunrise dates outside the polar regions differ from the date of the winte ...
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Arid
A region is arid when it severely lacks available water, to the extent of hindering or preventing the growth and development of plant and animal life. Regions with arid climates tend to lack vegetation and are called xeric or desertic. Most arid climates straddle the Equator; these regions include parts of Africa, Asia, South America, North America, and Australia. Change over time The distribution of aridity at any time is largely the result of the general circulation of the atmosphere. The latter does change significantly over time through climate change. For example, temperature increase by 1.5–2.1 percent across the Nile Basin over the next 30–40 years could change the region from semi-arid to arid, significantly reducing the land usable for agriculture. In addition, changes in land use can increase demands on soil water and thereby increase aridity. See also * Arid Forest Research Institute * Aridity index * Desert climate * Desiccation tolerance * Drought * Hu ...
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Summer
Summer is the hottest of the four temperate seasons, occurring after spring and before autumn. At or centred on the summer solstice, the earliest sunrise and latest sunset occurs, daylight hours are longest and dark hours are shortest, with day length decreasing as the season progresses after the solstice. The date of the beginning of summer varies according to climate, tradition, and culture. When it is summer in the Northern Hemisphere, it is winter in the Southern Hemisphere, and vice versa. Timing From an astronomical view, the equinoxes and solstices would be the middle of the respective seasons, but sometimes astronomical summer is defined as starting at the solstice, the time of maximal insolation, often identified with the 21st day of June or December. By solar reckoning, summer instead starts on May Day and the summer solstice is Midsummer. A variable seasonal lag means that the meteorological centre of the season, which is based on average temperature pattern ...
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Laâyoune-Sakia El Hamra
Laâyoune-Sakia El Hamra ( ar, العيون - الساقية الحمراء, al-ʿuyūn as-sāqiya l-ḥamrāʾ; ber, ⵍⵄⵢⵓⵏ ⵜⴰⵔⴳⴰ ⵜⴰⵣⴳⴳⵯⴰⵖⵜ, lɛyun targa tazggʷaɣt) is one of the twelve regions of Morocco. It is mainly located in the disputed territory of Western Sahara: the western part of the region is administered by Morocco and the eastern part by the Sahrawi Arab Democratic Republic. The region as claimed by Morocco covers an area of and had a population of 367,758 as of the 2014 Moroccan census. The capital of the region is Laâyoune. Geography Laâyoune-Sakia El Hamra borders the region of Guelmim-Oued Noun to the north and Dakhla-Oued Ed-Dahab to the south. It shares its eastern border with Mauritania's Tiris Zemmour Region, and to its west is the Atlantic Ocean. The towns of Tarfaya, El Marsa and Boujdour are located on the Atlantic coast, and the Canary Islands are located offshore. The regional capital Laâyoune is located i ...
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Tarfaya-Akhfenir Wind Farm
Tarfaya Wind Farm is a wind farm in Morocco, located in 20 km from Tarfaya. It was developed by Tarec (Trarfaya Energy Company), a 50/50 joint venture of Nareva Holding and International Power Ltd. Tarfaya Wind Farm is owned and operated by a 50:50 joint venture between the GDF SUEZ and Nareva Holding and it is Africa's 2nd largest capacity wind farm after Lake Turkana Wind Project, with 131 wind turbines, each generating 2.5 Megawatts of power, and a total installed capacity of 301 MW. It was on the list of ten “Most Outstanding African Projects in 2015”, a ranking by Jeune Afrique magazine. The park was commissioned in December 2014 after two years of work and investment of 5 billion dirhams. Its constructor and operator is Tarec, which sells the power generated to the National Electricity Office. See also * List of wind farms in Morocco As of 2020, Morocco had an installed wind power capacity of 1400 MW. As of 2013, there was an installed capacity of 947 MW ...
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Khenifiss National Park
Khenifiss National Park (french: Le Parc National Khenifiss ) is a national park in the southwest of Morocco, located near Akhfenir on the Atlantic coast in the region of Laâyoune-Sakia El Hamra. It was established in 2006. The area of the park is . The national park was created to protect desert, wetlands, and coastal dunes. The park was first created as a natural reserve in 1960, and in 1980, it was classified as a wetland of international importance. In 1983, the natural reserve was transformed into a Permanent Biological Reserve, and on September 26, 2006, the national park was created. The park is located at the coast of Atlantic Ocean, north of the border with Western Sahara, between the towns of Tan-Tan (north) and Tarfaya (south). The National Route 1, which runs along the Atlantic coast of Morocco, passes through the park. The park includes a coastal portion, the Khenfiss lagoon, the biggest lagoon at the Moroccan coast, and the inland portion, located on desert ...
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