|
Climate Of Kosovo
Kosovo is a relatively small country. Because of the climatic position and complicated structure of the relief it has a variety of climate systems. Kosovo lies in the south part of the middle geographical latitude of the northern hemisphere and it is affected by the Mediterranean Mild Climate and European Continental Climate. Important factors that affect Kosovo's climate are: its position towards Eurasia and Africa, hydrographic masses (Atlantic Ocean and Mediterranean sea), atmospheric masses ( tropic, arctic and continental) and others. Minor factors are: relief, hydrography, plain and vegetation. Areas The climatic area of the Ibar valley is influenced by continental air masses. For this reason, in this part of the region, the winters are colder with medium temperatures above , but sometimes down to . The summers are very hot with average temperatures of , sometimes up to . This area is characterized by a dry climate and a total annual precipitation of 600 mm per y ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precipitation Kosovo
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Precipitation (meteorology)
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 condense ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Gjilan
Gjilan, or Gnjilane ( sr-cyr, Гњилане) is the eighth largest city in Kosovo and seat of Gjilan Municipality and Gjilan District. Name Ottoman chronicler Evliya Çelebi mentions ''Morava'' as a settlement of the Sanjak of Vučitrn. Çelebi writes that: "The seventeen day journey from Constantinople (Istanbul) to pass through Vranje, Novo Brdo, Kriva Reka (Egridere) and Morava (Gjilan). The etymology of Gjilan is disputed. Albanian sources claim that the town (initially a village) obtained its name from Bahti Beg Gjinolli of Gjinaj clan that ruled the region of Vushtrri ( Llap and Drenica), and populated this area in the 18th century (around 1750). History In 1342, a place called Morava was visited by Serbian King Stefan Dušan (later Emperor, r. 1331–1355).Kostić 1922, p. 126 A fort was built nearby in the 14th century. Gornja Morava ("Upper Morava") was known as simply Morava under Ottoman rule, and it extended west of the Upper Žegra–Budriga–Cern ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Istok, Kosovo
Istog or Istok ( sq-definite, Istog, Istogu, sr, Исток, ''Istok'') or Burim is a town and municipality located in the District of Peja of western Kosovo. According to the 2011 census, the city of Istog has 5,115 inhabitants, while the municipality has 39,289 inhabitants. Based on the population estimates from the Kosovo Agency of Statistics in 2016, the municipality has 39,982 inhabitants. Name The name of the town comes from the version of the Serbian word ''istok'' (variant ''istek''), meaning "well, water source" referring to the springs of the Istočka river (, literally "spring river"), a tributary to the White Drin river. The name of the nearby village of Vrela, one of the largest settlements in the municipality, also means "springs", as does the newly proposed Albanian name of the town, ''Burimi''. History The Ottoman ''defter'' (tax registry; census) of 1582 registered the Ipek nahiyah as having 235 villages, of which Suho Grlo (Suvo Grlo) was located within moder ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Podujevo
Podujevo ( sr-Cyrl, Подујево), Podujeva, or Besiana ( sq-definite, Podujevë or ''Besianë''), is a city and municipality in Kosovo's Pristina District. According to the 2011 census, the city of Podujeva has 23,453 inhabitants, while the municipality has 88,499 inhabitants.Kosovo Agency for StatisticsThe population of the municipality of Podujeva according to settlement, gender and ethnicity 2011 The population of the city may be higher, as these figures include only the population of the cadastral zone of Podujeva, but not some urban neighborhoods of the city that are outside the cadastral zone. Podujeva is located along a regional motorway and has railroad passing through it, which links the area to surrounding regions. Pristina, the capital of Kosovo, is located some to the south. History Middle Ages The region includes many Medieval Serbian monuments. In 1355, Emperor Stefan Dušan gave the village of Braina to Mount Athos. In 1381, Prince Lazar gave Orlane ( ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Prizren
) , settlement_type = Municipality and city , image_skyline = Prizren Collage.jpg , imagesize = 290px , image_caption = View of Prizren , image_alt = View of Prizren , image_flag = , flag_alt = Flag of Prizren , image_seal = , seal_alt = Seal of Prizren , pushpin_map = Kosovo , pushpin_map_alt = Location of Prizren in Kosovo and Europe , pushpin_mapsize = 290 , pushpin_relief = 1 , pushpin_label = Prizren , coordinates = , subdivision_type = Country , subdivision_name = , subdivision_type2 = District , subdivision_name2 = Prizren , established_title = , established_date = , government_type = Mayor–council , leader_party = PDK , leader_title = Mayor , leader_name = Shaqir Tot ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Topography
Topography is the study of the forms and features of land surfaces. The topography of an area may refer to the land forms and features themselves, or a description or depiction in maps. Topography is a field of geoscience and planetary science and is concerned with local detail in general, including not only relief, but also natural, artificial, and cultural features such as roads, land boundaries, and buildings. In the United States, topography often means specifically ''relief'', even though the USGS topographic maps record not just elevation contours, but also roads, populated places, structures, land boundaries, and so on. Topography in a narrow sense involves the recording of relief or terrain, the three-dimensional quality of the surface, and the identification of specific landforms; this is also known as geomorphometry. In modern usage, this involves generation of elevation data in digital form (DEM). It is often considered to include the graphic representation of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Airflow
Airflow, or air flow, is the movement of air. The primary cause of airflow is the existence of air. Air behaves in a fluid manner, meaning particles naturally flow from areas of higher pressure to those where the pressure is lower. Atmospheric air pressure is directly related to altitude, temperature, and composition. In engineering, airflow is a measurement of the amount of air per unit of time that flows through a particular device. It can be described as a volumetric flow rate (volume of air per unit time) or a mass flow rate (mass of air per unit time). What relates both forms of description is the air density, which is a function of pressure and temperature through the ideal gas law. The flow of air can be induced through mechanical means (such as by operating an electric or manual fan) or can take place passively, as a function of pressure differentials present in the environment. Types of airflow Like any fluid, air may exhibit both laminar and turbulent flow patterns. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountain
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited Summit (topography), summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are Monadnock, isolated summits, but most occur in mountain ranges. Mountain formation, Mountains are formed through Tectonic plate, tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through Slump (geology), slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce Alpine climate, colder climates than at sea level at similar latitude. These colder climates strongly affect the Montane ecosystems, ecosys ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
.jpg "Click for more on -> Summer")
