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Sirocco
Sirocco ( ) or scirocco 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: * * * or ''marin'' * * * * or * * , or romanized: sirókos * or * ( sr-Cyrl, југо), in Croatia rarely ''širok'' (широк) * * or * Libyan Arabic: , romanized: , which means "coming from the Qibla" * , which means "fifty" ("fifty-day wind") * , probably from with the same meaning as ; or * , pronounced širguī The Roman poet Horace refers to the sirocco at Trevico in Apulia as "Atabulus" (a Messapic word) in his account of his journey to Brundisium in 37 BC. Development Siroccos arise from warm, dry, tropical air masses that are pulled northward by low-pressure cells moving eastward across the Med ...
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Adriatic Sea
The Adriatic Sea () is a body of water separating the Italian Peninsula from the Balkans, Balkan Peninsula. The Adriatic is the northernmost arm of the Mediterranean Sea, extending from the Strait of Otranto (where it connects to the Ionian Sea) to the northwest and the Po Valley. The countries with coasts on the Adriatic are Albania, Bosnia and Herzegovina, Croatia, Italy, Montenegro, and Slovenia. The Adriatic contains more than 1,300 islands, mostly located along its eastern coast. It is divided into three basins, the northern being the shallowest and the southern being the deepest, with a maximum depth of . The prevailing currents flow counterclockwise from the Strait of Otranto. Tidal movements in the Adriatic are slight, although acqua alta, larger amplitudes occur occasionally. The Adriatic's salinity is lower than the Mediterranean's because it collects a third of the fresh water flowing into the Mediterranean, acting as a dilution basin. The surface water temperatures ...
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Acqua Alta
An (, ; ) is an exceptional tide peak that occurs periodically in the northern Adriatic Sea. The term is applied to such tides in the Italian region of Veneto. The peaks reach their maximum in the Venetian Lagoon, where they cause partial flooding of Venice and Chioggia; flooding also occurs elsewhere around the northern Adriatic, for instance at Grado and Trieste, but much less often and to a lesser degree. The phenomenon occurs mainly between autumn and spring, when the astronomical tides are reinforced by the prevailing seasonal winds that hamper the usual reflux. The main winds involved are the sirocco, which blows northbound along the Adriatic Sea, and the bora, which has a specific local effect due to the shape and location of the Venetian Lagoon. Causes Precise scientific parameters define the phenomenon called ''acqua alta'', the most significant of which (i.e., the deviation in amplitude from a base measurement of "standard" tides) is measured by the hydrographi ...
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Notus
In Greek mythology and religion, Notus () is the god of the south wind and one of the Anemoi (wind-gods), sons of the dawn goddess Eos and the star-god Astraeus. A desiccating wind of heat, Notus was associated with the storms of late summer and early autumn, wetness, mist, and was seen as a rain-bringer. Unlike his two more notable brothers, Boreas (the god of the north wind) and Zephyrus (the god of the west wind), Notus has little to no unique mythology of his own. His Roman equivalent is the god Auster. Etymology The Greek noun refers both to the south cardinal direction and the south wind that blows from it. Its ultimate etymology remains unknown, although a pre-Greek origin seems to be the most likely origin. Family Notus, like most of the wind gods, the Anemoi was said to be the son of Eos, the goddess of the dawn, by her husband Astraeus, a minor god related to the stars. Thus, he is brother to the five star-gods and the justice goddess Astraea, and half-brother t ...
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Khamsin
Khamsin, chamsin or hamsin ( , meaning "fifty"), more commonly known in Egypt, Israel and Palestine as khamaseen ( , ), is a dry, hot, sandy local wind affecting Egypt and the Levant; similar winds, blowing in other parts of North Africa, the Arabian Peninsula and the entire Mediterranean basin, have different local names, such as '' bad-i-sad-o-bist roz'' in Iran and Afghanistan, ''haboob'' in the Sudan, ''aajej'' in southern Morocco, ''ghibli'' in Tunis, ''harmattan'' in the western Maghreb, ''africo'' in Italy, sirocco (derived from the Arabic , "eastern") which blows in winter over much of the Middle East,Philologos ''Fifty Days and Fifty Nights'' in The Forward, 4 April 2003. Accessed 18 May 2018 and '' simoom''. From the Arabic word for "fifty", these dry, sand-filled windstorms blow sporadically in Egypt typically after fifty days from the start of spring, hence the name. The term is also used in the southern Levant (Jordan, Israel, Palestine), where the phenomenon ...
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Messapic Language
Messapic (; also known as Messapian; or as Iapygian) is an extinct Indo-European Paleo-Balkanic language of the southeastern Italian Peninsula, once spoken in Salento by the Iapygian peoples of the region: the Calabri and Salentini (known collectively as the Messapians), the Peucetians and the Daunians. Messapic was the pre- Roman, non- Italic language of Apulia. It has been preserved in about 600 inscriptions written in an alphabet derived from a Western Greek model and dating from the mid-6th to at least the 2nd century BC, when it went extinct following the Roman conquest of the region. Name The term 'Messapic' or 'Messapian' is traditionally used to refer to a group of languages spoken by the Iapygians, a "relatively homogeneous linguistic community" of non- Italic-speaking tribes ( Messapians, Peucetians and Daunians) dwelling in the region of Apulia before the Roman conquest. However, some scholars have argued that the term ' Iapygian languages' should be prefer ...
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Sahara Dust Vitrolles
The Sahara (, ) is a desert spanning across North Africa. With an area of , it is the largest hot desert in the world and the third-largest desert overall, smaller only than the deserts of Antarctica and the northern Arctic. The name "Sahara" is derived from , a broken plural form of ( ), meaning "desert". The desert covers much of North Africa, excluding the fertile region on the Mediterranean Sea coast, the Atlas Mountains of the Maghreb, and the Nile Valley in Egypt and the Sudan. It stretches from the Red Sea in the east and the Mediterranean in the north to the Atlantic Ocean in the west, where the landscape gradually changes from desert to coastal plains. To the south it is bounded by the Sahel, a belt of semi-arid tropical savanna around the Niger River valley and the Sudan region of sub-Saharan Africa. The Sahara can be divided into several regions, including the western Sahara, the central Ahaggar Mountains, the Tibesti Mountains, the Aïr Mountains, the Ténéré ...
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Sahara
The Sahara (, ) is a desert spanning across North Africa. With an area of , it is the largest hot desert in the world and the list of deserts by area, third-largest desert overall, smaller only than the deserts of Antarctica and the northern Arctic. The name "Sahara" is derived from , a broken plural form of ( ), meaning "desert". The desert covers much of North Africa, excluding the fertile region on the Mediterranean Sea coast, the Atlas Mountains of the Maghreb, and the Nile, Nile Valley in Egypt and the Sudan. It stretches from the Red Sea in the east and the Mediterranean in the north to the Atlantic Ocean in the west, where the landscape gradually changes from desert to coastal plains. To the south it is bounded by the Sahel, a belt of Tropical and subtropical grasslands, savannas, and shrublands, semi-arid tropical savanna around the Niger River valley and the Sudan (region), Sudan region of sub-Saharan Africa. The Sahara can be divided into several regions, including ...
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Foehn Wind
A Foehn, or Föhn (, , , ), is a type of dry, relatively warm downslope wind in the lee of a mountain range. It is a rain shadow wind that results from the subsequent adiabatic warming of air that has dropped most of its moisture on windward slopes (see orographic lift). As a consequence of the different adiabatic lapse rates of moist and dry air, the air on the leeward slopes becomes warmer than equivalent elevations on the windward slopes. Foehn winds can raise temperatures by as much as in just a matter of hours. Switzerland, southern Germany, and Austria have a warmer climate due to the Foehn, as moist winds off the Mediterranean Sea blow over the Alps. Etymology The name ''Foehn'' (, ) arose in the Alpine region. Originating from Latin , a mild west wind of which Favonius was the Roman personification and probably transmitted by or just , the term was adopted as . In the Southern Alps, the phenomenon is known as but also and in Serbo-Croatian and Slovene. Th ...
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Hurricane
A tropical cyclone is a rapidly rotating storm system with a low-pressure area, a closed low-level atmospheric circulation, strong winds, and a spiral arrangement of thunderstorms that produce heavy rain and squalls. Depending on its location and strength, a tropical cyclone is called a hurricane (), typhoon (), tropical storm, cyclonic storm, tropical depression, or simply cyclone. A hurricane is a strong tropical cyclone that occurs in the Atlantic Ocean or northeastern Pacific Ocean. A typhoon is the same thing which occurs in the northwestern Pacific Ocean. In the Indian Ocean and South Pacific, comparable storms are referred to as "tropical cyclones". In modern times, on average around 80 to 90 named tropical cyclones form each year around the world, over half of which develop hurricane-force winds of or more. Tropical cyclones typically form over large bodies of relatively warm water. They derive their energy through the evaporation of water from the ocean ...
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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, the Montenegrin Littoral, the Sloven ...
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