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Dramalj
Dramalj is a village in Croatia. It is part of the town of Crikvenica, extending from the neighborhood Crni mol to the tourist complex Kačjak. Dramalj has 1,485 inhabitants, most of whom are empolyed in the tourism and catering industries. More intensive development of the village started back in the 19th century, following the tourism boom in the nearby Crikvenica area, as well as the rest of the Croatian Littoral. The village has several restaurants offering local specialties, as well as a post office and a clinic providing medical assistance to tourists. It is also home to the Dramalj Culture Hall, where traditional carnival feasts are held during the winter. History Dramalj was first mentioned in the 18th century, when it was named Zagorje - Dramalj. In the beginning, it was a fishing port with olive groves, most of which were owned by the inhabitants of Tribalj valley. There are ruins of an ancient Liburnian hill fort enclosed with a dry-stone dyke above Dramalj. Ampho ...
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Crikvenica
Crikvenica () is a city in Croatia, located on the Adriatic in the Primorje-Gorski Kotar County. Names The names of the town in various languages include: * la, Ad Turres * it, Cirquenizza * hu, Cirkvenica, Cirkvenicza, Czirkvenicza, Czirkwenicza * german: Cirknenz Geography Crikvenica is located southeast of Rijeka and is the largest settlement on the coast of the Vinodol coastal area. Towns near Crikvenica include Kraljevica, Selce and Novi Vinodolski. In the last twenty years, due to urban expansion of Crikvenica itself and expansion of the nearby town of Selce, the two were merged into a mini-conglomerate. Population In the 2011 census, Crikvenica had a total municipal population of 11,122, in the following settlements: * Crikvenica, population 6,860 * Dramalj, population 1,485 * Jadranovo, population 1,224 * Selce, population 1,553 History Crikvenica was developed on the site of a Roman era settlement and military base called Ad Turres. Old Crikvenica was o ...
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List Of Regions Of Croatia
The Republic of Croatia is administratively organised into twenty counties, and is also traditionally divided into four historical and cultural regions: Croatia Proper, Dalmatia, Istria, and Slavonia. These are further divided into other, smaller regions. Historical regions Smaller regions * Banovina (or Banija) is a region in central Croatia, situated between the rivers Sava, Una and Kupa. * Baranja forms a small enclave between the region of Slavonia and the Republic of Hungary, it lies in the north east of Croatia. The rest of the region known as Baranja is located in Hungary. *Croatian Littoral (''Hrvatsko primorje'') the maritime region of Croatia proper * Gorski kotar the region occupies the area between the major cities of Karlovac and Rijeka (a.k.a. ''Fiume''). The regions main city is Delnice. The river Kupa separates the region from the Republic of Slovenia in the north. *Konavle forms a small subregion of Dalmatia in the very south of Croatia and stretche ...
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Austria-Hungary
Austria-Hungary, often referred to as the Austro-Hungarian Empire,, the Dual Monarchy, or Austria, was a constitutional monarchy and great power in Central Europe between 1867 and 1918. It was formed with the Austro-Hungarian Compromise of 1867 in the aftermath of the Austro-Prussian War and was dissolved shortly after its defeat in the First World War. Austria-Hungary was ruled by the House of Habsburg and constituted the last phase in the constitutional evolution of the Habsburg monarchy. It was a multinational state and one of Europe's major powers at the time. Austria-Hungary was geographically the second-largest country in Europe after the Russian Empire, at and the third-most populous (after Russia and the German Empire). The Empire built up the fourth-largest machine building industry in the world, after the United States, Germany and the United Kingdom. Austria-Hungary also became the world's third-largest manufacturer and exporter of electric home appliances, ...
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Levant (wind)
The levant ( ca, Llevant, it, Levante, mt, Lvant, el, Λεβάντες, es, Levante) is an easterly wind that blows in the western Mediterranean Sea and southern France, an example of mountain-gap wind. In Roussillon it is called "llevant" and in Corsica "levante". In the western Mediterranean, particularly when the wind blows through the Strait of Gibraltar, it is called the Viento de Levante or the Levanter. It is also known as the Solano. When blowing moderately or strongly, the levant causes heavy swells on the Mediterranean. Usually gentle and damp, the levant frequently brings clouds and rain. When it brings good weather, it is known as the "''levant blanc''",Meteo-France website (in French) on "Vents regionaux and vents locaux" or "''levante calma''" in Gibraltar. The origin of the name is the same as the origin of the Levant, the region of the eastern Mediterranean: it is the Latin word "levante", the participle of levare "to raise" – as in sol levante "risi ...
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Maestral
The mistral ( ca, Mestral, el, Μαΐστρος, it, Maestrale, mt, Majjistral, Corsican: ''Maestrale'') is a strong, cold, northwesterly wind that blows from southern France into the Gulf of Lion in the northern Mediterranean. It produces sustained winds often exceeding , sometimes reaching . It is most common in the winter and spring, and strongest in the transition between the two seasons. Periods of the wind exceeding for more than sixty-five hours have been reported. In France, it refers to a violent, cold, north or northwest wind that accelerates when it passes through the valleys of the Rhône and the Durance Rivers to the coast of the Mediterranean around the Camargue region. It affects the northeast of the plain of Languedoc and Provence to the east of Toulon, where it is felt as a strong west wind. It has a major influence all along the Mediterranean coast of France, and often causes sudden storms in the Mediterranean between Corsica and the Balearic Islands. The ...
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Ostro
Ostro ( ca, Migjorn, hr, Oštro, el, Όστρια), or Austro, is a southerly wind in the Mediterranean Sea, especially the Adriatic Sea, Adriatic. Its name is Italian, derived from the Latin name ''Anemoi#Auster, Auster'', which also meant a southerly wind. It is a warm and humid wind that often carries rain, but it is also sometimes identified with the Libeccio and sirocco, Scirocco. External links List of wind names (in German)
Italian words and phrases Winds Climate of Malta {{Climate-stub ...
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Jugo
Sirocco ( ), scirocco, or, rarely, siroc (see below) is a Mediterranean wind that comes from the Sahara and can reach hurricane speeds in North Africa and Southern Europe, especially during the summer season. Names ''Sirocco'' derives from '' šurūq'' (), verbal noun of '' šaraqa'', related to the East, ''aš-šarq''. Various names for this wind in other languages include: * it, scirocco * scn, sciroccu * es, siroco * ca, xaloc * mt, xlokk * oc, siròc or * el, σορόκος, sorókos, or romanized: sirókos * sq, Jugu (south) * hr, jugo, lit=southern, or rarely ''širok'' * lij, sciöco or * Libyan Arabic: , romanized: , which means 'coming from the Qibla' * arz, خمسين, Ḫamsīn, which means 'fifty' ('fifty-day wind') * aeb, شلوق, šlūq, probably from with the same meaning as ; or * ary, شرقي, lit=eastern, šarquiyy, pronounced širguī Development Siroccos arise from warm, dry, tropical air masses that are pulled northward by low- ...
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Bora (wind)
The bora is a northerly to north-easterly katabatic wind in areas near the Adriatic Sea. Similar nomenclature is used for north-eastern winds in other littoral areas of eastern Mediterranean and Black Sea basins. Name It is known in Greek as (''mpóra'', pronounced ''bora'') and Italian as . In English, the name ''bora'' is used. The Serbo-Croatian name and Slovene are not etymologically related to ''bora''; they derive from Common Slavic ''burja'' 'storm' (from the verb ''*burĭti''), and the meaning 'bora' developed later. The same root as ''bora'' is found in the name of the Greek mythological figure of Boreas (Βορέας), and the Modern Greek word for the north wind . Historical linguists speculate that the name may derive from a Proto-Indo-European root *''gworhx-'' 'mountain', which gave rise to Slavic ''gora'' and Sanskrit ''giri-'', both 'mountain'. Features The changeable bora can often be felt all over Adriatic Croatia, Montenegrin Littoral, the Slovenian ...
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Relative 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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Cloud Cover
Cloud cover (also known as cloudiness, cloudage, or cloud amount) refers to the fraction of the sky obscured by clouds on average when observed from a particular location. Okta is the usual unit for measurement of the cloud cover. The cloud cover is correlated to the sunshine duration as the least cloudy locales are the sunniest ones while the cloudiest areas are the least sunny places, as clouds can block sunlight, especially on sunrise and sunset where sunlight is already limited. The global cloud cover averages around 0.68 when analyzing clouds with optical depth larger than 0.1. This value is lower (0.56) when considering clouds with an optical depth larger than 2, and higher when counting subvisible cirrus clouds. Particularly over the oceans cloud cover is persistent with an average 72% of cloud cover. Role in the climate system Clouds play multiple critical roles in the climate system and diurnal cycle. In particular, being bright objects in the visible part o ...
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Continental Climate
Continental climates often have a significant annual variation in temperature (warm summers and cold winters). They tend to occur in the middle latitudes (40 to 55 north), within large landmasses where prevailing winds blow overland bringing some precipitation, and temperatures are not moderated by oceans. Continental climates occur mostly in the Northern Hemisphere due to the large landmasses found there. Most of northern and northeastern China, eastern and southeastern Europe, Western and north western Iran, central and southeastern Canada, and the central and northeastern United States have this type of climate. Continentality is a measure of the degree to which a region experiences this type of climate. In continental climates, precipitation tends to be moderate in amount, concentrated mostly in the warmer months. Only a few areas—in the mountains of the Pacific Northwest of North America and in Iran, northern Iraq, adjacent Turkey, Afghanistan, Pakistan, and Central Asia ...
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Mediterranean Climate
A Mediterranean climate (also called a dry summer temperate climate ''Cs'') is a temperate climate sub-type, generally characterized by warm, dry summers and mild, fairly wet winters; these weather conditions are typically experienced in the majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. This climate type's name is in reference to the coastal regions of the Mediterranean Sea within the Mediterranean Basin, where this climate type is most prevalent. The "original" Mediterranean zone is a massive area, its western region beginning with the Iberian Peninsula in southwestern Europe and coastal regions of northern Morocco, extending eastwards across southern Europe, the Balkans, and coastal Northern Africa, before reaching a dead-end at the Levant region's coastline. Mediterranean climate zones are typically located along the western coasts of landmasses, between roughly 30 and 45 ...
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