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60-507: The Jadro flows through the town of Solin and has a length of approximately four kilometres' moreover, the river provides water to the cities of Split , Kaštela and Trogir as well as of municipalities Podstrana , Klis , Seget and Okrug . Incompliances with the regulations related to water for consumption occasionally appear due to turbidity caused by abundant precipitation. People from Solin also call it Solinska rika (Croatian for "Solin's river"). Salmo obtusirostris salonitana

120-424: A 40 mm (1.6 in) level. The third letter indicates the degree of summer heat: " a " represents an average temperature in the warmest month above 22 °C (72 °F), while " b " indicates the average temperature in the warmest month below 22 °C (72 °F). There is a "c" with 3 or less months' average temperature above 10 °C (50 °F), but this climate is rare and is very isolated. Under

180-891: A Csb climate because of its location inside the Alborz mountains . Winters in this zone are rainy and can be mild to chilly. Some locales in this zone experience some amount of snowfall, while others do not. Csb climates are found in northwestern Iberian Peninsula (namely Galicia and the Norte region and west coast of Portugal ), in coastal Northern California , in the Pacific Northwest (namely western Washington , western Oregon and southern portions of Vancouver Island in British Columbia ), in central Chile , in parts of southern Australia and in sections of southwestern South Africa . A few locations close to

240-456: A Mediterranean climate are near large bodies of water, temperatures are generally moderate, with a comparatively small range of temperatures between the winter low and summer high unlike (the relatively rare) dry-summer humid continental climates (although the daily diurnal range of temperature during the summer is large due to dry and clear conditions, except along the immediate coastlines). Temperatures during winter only occasionally fall below

300-613: A century of intensive agriculture. Much of the Overberg in the southern Cape of South Africa , was once covered with renosterveld , but has likewise been largely converted to agriculture, mainly for wheat . In hillside and mountainous areas, away from the urban sprawls , ecosystems and habitats of native vegetation are more sustained and undisturbed. The fynbos vegetation in the South-western Cape in South Africa

360-668: A few kilometres inland. Occasionally also termed the "cool-summer Mediterranean climate", this subtype of the Mediterranean climate ( Csb ) is less common and experience warm (but not hot) and dry summers, with no average monthly temperatures above 22 °C (72 °F) during its warmest month and as usual an average in the coldest month between 18 and −3 °C (64 and 27 °F) or, in some applications, between 18 and 0 °C (64 and 32 °F). Also, at least four months must average above 10 °C (50 °F). Cool ocean currents, upwelling and higher latitudes are often

420-556: A mean temperature below 0 °C (32 °F) (or −3 °C [27 °F]), depending on the isotherm used). Regions in the Americas with this climate are influenced by the dry-summer trend (though briefly) that extends considerably poleward along the west coast, as well as the moderating influences of high altitude and relative proximity to the Pacific Ocean. These conditions maintain an unusually narrow temperature range through

480-550: A season earlier than at the Dead Sea . In the Holy Land no rain at all falls in summer but early rains may come in autumn. The majority of the regions with Mediterranean climates have relatively mild winters and very warm summers. However, winter and summer temperatures can vary greatly between different regions with a Mediterranean climate. For instance, in the case of winters, Funchal experiences mild to warm temperatures in

540-545: A short time, is probable. That city, located on the Adriatic coast, with excellent sea connections with Italy and the Middle East , attracted Christian messengers of faith. Salona had a well-organized Christian community with a bishop as leader ever since the middle of the 3rd century (bishop martyr Venantius lived at that time). Since the fourth century, Salona honored in its large basilicas its glorious martyrs from

600-523: A suburb of Split. Today, with its independent municipal status, Solin is part of the Split conurbation , well connected with other towns. Lately, besides industry, tourism is being developed based on numerous archaeological sites and Solin's distinctive image that comes from many urban parks along the Jadro. Solin is situated north of the Split peninsula, in a basin surrounded by mountains Kozjak (779 m) to

660-597: A yearly cycle in which abiotic (environmental) controls of stream populations and community structure dominate during floods, biotic components (e.g. competition and predation) controls become increasingly important as the flood discharge declines, and environmental controls regain dominance as environmental conditions become very harsh (i.e. hot and dry); as a result, these communities are well suited to recover from droughts , floods , and fires . Aquatic organisms in these regions show distinct long-term patterns in their structure and function, and are also highly sensitive to

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720-413: Is Mediterranean , with mild winters and hot summers. During the winter, a strong north-eastern wind Bura occurs frequently. The administrative area of the city of Solin includes the following settlements: In the vernacular, Solin is divided into eight neighbourhoods: Centar, Priko vode, Srednja strana, Sveti Kajo, Rupotina, Vranjic, Mravince and Kučine. In the late ancient times, Salona's importance

780-576: Is a town and a suburb of Split , in Split-Dalmatia county, Croatia . It is situated right northeast of Split , on the Adriatic Sea and the river Jadro . Solin developed on the location of ancient city of Salona , which was the capital of the Roman province of Dalmatia and the birthplace of Emperor Diocletian . After the arrival of Avars and Croats in the 7th-century, the town

840-646: Is adequate rainfall year-round. The Köppen Climate Classification subtype for this climate is " Csa " ( Mediterranean climate ). Mediterranean climate A Mediterranean climate ( / ˌ m ɛ d ɪ t ə ˈ r eɪ n i ən / MED -ih-tə- RAY -nee-ən ), also called a dry summer climate , described by Köppen as Cs , is a temperate climate type that occurs in the lower mid-latitudes (normally 30 to 44 north and south latitude). Such climates typically have dry summers and wet winters, with summer conditions being hot and winter conditions typically being mild. These weather conditions are typically experienced in

900-485: Is an endemic trout species living in this river, which is currently endangered by the rainbow trout . This Split-Dalmatia County geography article is a stub . You can help Misplaced Pages by expanding it . This article related to a river in Croatia is a stub . You can help Misplaced Pages by expanding it . Solin, Croatia Solin ( Latin and Italian : Salona ; Ancient Greek : Σαλώνα Salóna )

960-424: Is closely associated with Mediterranean climate zones, as are unique freshwater communities, though vegetation native to the Mediterranean climate zone can also be found in the approximate nearby climate zones, which usually tend to be the humid subtropical , oceanic and/or semi-arid zones, depending on the region and location. Particularly distinctive of the climate are sclerophyll shrublands, called maquis in

1020-576: Is famed for its high floral diversity , and includes such plant types as members of the Restionaceae , Ericas (Heaths) and Proteas . Representatives of the Proteaceae also grow in Australia, such as Banksias . The palette of California native plants is also renowned for its species and cultivar diversity. This subtype of the Mediterranean climate ( Csa ) is the most common form of

1080-406: Is higher, steppe climates tend to prevail, but still follow the basic pattern of the Mediterranean climates. Irregularity of the rainfall, which can vary considerably from year to year, accentuates the droughts of the Mediterranean climate. Rain does not fall evenly, nor does the rain arrive at the same time or within the same intervals. In Gibraltar , for instance, rain starts falling nearly half

1140-539: Is organized by several bus lines operated by the Promet Split company, which provides public transport for the Split conurbation. These routes are: Local bus lines from Split to Kaštela , Trogir , Klis and Sinj also stop in Solin centre. As of 2021, Solin has 24,862 inhabitants , 49.01% of them being male and 50.09% being female . Solin's climate has mild differences between highs and lows, and there

1200-583: The Avars retreated from those regions, to a settlement "Spalatum", today's ( Split ), at the location of Diocletian's Palace (probably around the middle 7th century AD ). Christianity in Salona probably originated during the time of the apostles . The Apostle Paul mentions that his pupil Apostle Titus traveled to Dalmatia so the assumption that he worked in Dalmatia's capital city of Salona, at least for

1260-590: The Cathedral of Saint Domnius . In the 9th century, Duke Trpimir I of Croatia built a Benedictine monastery between Klis and Solin. Inscriptions dated to 852 from there are first known written record of the name of Croats in modern-day Croatian territory. In the 10th century, Queen Helen (Jelena) had built two churches by the Jadro: the Church of St. Stephen and the Church of St. Mary. The Church of St. Stephen

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1320-603: The Köppen climate classification , "hot dry-summer" climates (classified as Csa ) and "cool dry-summer" climates (classified as Csb ) are often referred to as just "Mediterranean". Under the Köppen climate system, the first letter indicates the climate group (in this case temperate climates). Temperate climates or " C " zones average temperature above 0 °C (32 °F) (or −3 °C (27 °F)), but below 18 °C (64 °F), in their coolest months. The second letter indicates

1380-738: The garrigue or maquis in the European Mediterranean Basin, the chaparral in California, the fynbos in South Africa , the mallee in Australia, and the matorral in Chile. Areas with this climate are also where the so-called "Mediterranean trinity" of major agricultural crops have traditionally been successfully grown ( wheat , grapes and olives ). As a result, these regions are notable for their high-quality wines, grapeseed/olive oils, and bread products. Under

1440-415: The subtropical ridge migrates towards the equator and leaves the area, making rainfall much more likely. As a result, areas with this climate receive almost all of their precipitation during their winter and spring seasons, and may go anywhere from four to six months during the summer and early fall without having any significant precipitation . In the lower latitudes, precipitation usually decreases in both

1500-604: The Andes in Northern Ecuador , Peru , Colombia , and Western Venezuela . The cold-summer subtype of the Mediterranean climate ( Csc ) is rare and predominantly found at scattered high-altitude locations along the west coasts of North and South America having a similar climate. This type is characterized by cool, dry summers, with less than four months with a mean temperature at or above 10 °C (50 °F), as well as with cool, wet winters, with no winter month having

1560-631: The Atlantic portions of Iberia and Northwest Africa, the Pacific portions of the United States and Chile, extreme west areas of Argentina, around Cape Town in South Africa, parts of Southwest and South Australia , and parts of Central Asia . They tend to be found in proximity (both poleward and near the coast) of desert and semi-arid climates , and equatorward of oceanic climates . Mediterranean climate zones are typically located along

1620-399: The Köppen classification, dry-summer climates ( Csa , Csb ) usually occur on the western sides of continents. Csb zones in the Köppen system include areas normally not associated with Mediterranean climates but with Oceanic climates, such as much of the Pacific Northwest , much of southern Chile , parts of west-central Argentina , and parts of New Zealand . Additional highland areas in

1680-671: The Mediterranean Basin, chaparral in California, matorral in Chile, fynbos in South Africa, and mallee and kwongan shrublands in Australia. Mediterranean vegetation shows a number of adaptations to drought , grazing , and frequent fire regimes. The small sclerophyllous leaves that characterize many of the perennial shrubs of this biome, help conserve water and prevent nutrient loss. The soils generally are of low fertility , and many plants have mutualistic relationships with nitrogen-fixing bacteria . Aquatic communities in Mediterranean climate regions are adapted to

1740-514: The Mediterranean climate typically experience hot, sometimes very hot and dry summers. Winters can be mild, cool or chilly, and some cities in this region receive somewhat regular snowfall (e.g. Kermanshah ), while others do not receive any (e.g. Casablanca ). Csa climates are mainly found around the Mediterranean Sea , southern Australia, southwestern South Africa , sections of Central Asia , northern sections of Iran and Iraq ,

1800-448: The Mediterranean climate, therefore it is also known as a "typical Mediterranean climate". As stated earlier, regions with this form of a Mediterranean climate experience average monthly temperatures in excess of 22.0 °C (71.6 °F) during its warmest month and an average in the coldest month between 18 and −3 °C (64 and 27 °F) or, in some applications, between 18 and 0 °C (64 and 32 °F). Regions with this form of

1860-431: The average annual precipitation must not exceed 900 mm (35 in), as well as satisfying Köppen's precipitation requirements. [Chile] has four months of winter, no more, and in them, except when there is a quarter moon, when it rains one or two days, all the other days have such a beautiful sunshine that is not necessary to resort to fire. The summer is so temperate, with delicious airs, that man can go all day under

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1920-407: The chapel. Search for relics for Rome was probably the incentive for Salona residents who inhabited the new city of Split, located only a few kilometers from the abandoned Salona. At the very least, they wanted to bring to Split the bones of their most important protectors: St. Domnius and St. Anastasius . They placed them in what was once Diocletian's mausoleum, which was subsequently converted into

1980-428: The city are located in the middle part of the river's flow, and on the gentle slopes that make the Solin basin. Industrial areas occupy a small valley of the upper basin of the Jadro, as well as large areas to the west of the center, on the easternmost tip of the bay of Kaštela where industrial and service port is situated. The ruins of the ancient Salona are located in the middle, to the west of today center. The climate

2040-524: The city territory. Although there is a train station in Solin (2 km (1 mi) to the west of the city centre), only regional trains stop here. Regional rail transport is to be intensified because of the Split Suburban Railway project. Split Airport (SPU) in Kaštela is situated 15 km (9 mi) to the west of Solin, well-connected by roads and local transport. Public transport

2100-434: The cold current has a stabilizing effect on the surrounding air, further reducing the chances for rain, but often causing thick layers of marine fog that usually evaporates by mid-day. Similar to desert climates, in many Mediterranean climates there is a strong diurnal character to daily temperatures in the warm summer months due to strong solar heating during the day from sunlight and rapid cooling at night. In winter,

2160-562: The fall of Salona and the whole region under the Avarian rule (first quarter of 7th century), worship of Salona's martyrs was moved to Rome. Namely, Pope John IV ordered transportation of parts of their relics, which he placed in a dedicated chapel close to the Lateran baptistry. The images of those saints, which had been created in mosaic by the Pope's wish, can be found today in the apside of

2220-557: The freezing point and snow is generally seldom seen. Summer temperatures can be cool to very hot, depending on the distance from a large body of water, elevation, and latitude, among other factors. Strong winds from inland desert regions can sometimes boost summer temperatures up, quickly increasing the risk of wildfires . Notable exceptions to the usual proximity from bodies of water, thus featuring extremely high summer temperatures and cooler winters, include south-eastern Turkey and northern Iraq ( Urfa , Erbil ), surrounded by hot deserts to

2280-706: The interior of northern California west of the Sierra Nevada , along the Wasatch Front in Utah , and inland areas of southern Oregon west of the Cascade Mountains . Southern California's coasts also experience hot summers due to the shielding effect of the Channel Islands . However, unshielded areas of that coastline can have warm-summer Mediterranean climates with hot-summer areas just

2340-432: The lowland areas, temperatures which can sometimes prohibit the growth of typical cold-sensitive Mediterranean plants. Some Spanish authors opt to use the term 'continental Mediterranean climate' ( Clima Mediterráneo Continentalizado ) for some regions with lower temperatures in winter than the coastal areas, but Köppen's Cs zones show no distinction as long as winter temperature means stay above freezing. Additionally,

2400-489: The majority of Mediterranean-climate regions and countries, but remain highly dependent on proximity to the ocean, altitude and geographical location. The dry summer climate is found throughout the warmer middle latitudes , affecting almost exclusively the western portions of continents in relative proximity to the coast. The climate type's name is in reference to the coastal regions of the Mediterranean Sea , which mostly share this type of climate, but it can also be found in

2460-573: The north and Mosor (1339 m) to the east. The ancient city of Salona developed near the estuary of Jadro, and the later medieval settlement was formed on one of the several islands formed by the river, which is where today's center is also situated. The city covers an area of 18 km (7 sq mi), situated in the central part of the Split conurbation , 8 km (5 mi) north of Split, 6 km (4 mi) east of Kaštela , 22 km (14 mi) east of Trogir and 4 km (2 mi) south of Klis . Residential and business parts of

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2520-580: The precipitation pattern (" s " represents dry summers). Köppen has defined a dry summer month as a month with less than 30 mm (1.2 in) of precipitation and as a month within the high-sun months of April to September, in the case of the Northern Hemisphere and October to March, in the case of the Southern Hemisphere, and it also must contain exactly or less than one-third that of the wettest winter month. Some, however, use

2580-530: The reason for this cooler type of Mediterranean climate. The other main reason for this cooler type is the altitude . For instance, Menton on the French coast has a Csa climate while Castellar, Alpes-Maritimes , the adjacent town just north of Menton, with an altitude between 100 and 1,382 m (328 and 4,534 ft), has a Csb climate instead. The village of Siah Bisheh in Northern Iran also has

2640-650: The recent effects of climate change . The native vegetation of Mediterranean climate lands must be adapted to survive long, hot summer droughts in summer and prolonged wet periods in winter. Mediterranean vegetation examples include the following: Many native vegetations in Mediterranean climate area valleys have been cleared for agriculture and farming. In places such as the Sacramento Valley and Oxnard Plain in California , draining marshes and estuaries combined with supplemental irrigation has led to

2700-419: The south and mountains to the north. Those places routinely experience summer daily means of over 30 °C (86 °F) and daily highs above 40 °C (104 °F), while receiving enough rainfall in winter not to fall into arid or semi-arid classifications. As in every climatologic domain, the highland locations of the Mediterranean domain can present cooler temperatures in the summer and winter than

2760-546: The south coast of England such as Weymouth and Portland just scrape into this climate classification due to very low rainfall in July. A trend towards slightly drier summers during the 1971–2000 climate average period, meant that this classification previously extended slightly further to include a few other weather stations in southern England, such as Bognor Regis and Teignmouth . Rarer instances of this climate can be found in relatively small and isolated high altitude areas of

2820-743: The subtropics also meet Cs requirements, though they, too, are not normally associated with Mediterranean climates. The same goes for a number of oceanic islands such as Madeira , the Juan Fernández Islands , the western part of the Canary Islands , and the eastern part of the Azores . Under Trewartha 's modified Köppen climate classification, the two major requirements for a Cs climate are revised. Under Trewartha's system, at least eight months must have average temperatures of 10 °C (50 °F) or higher ( subtropical ), and

2880-537: The sun. Poleward extension and expansion of the subtropical anticyclone over the oceans bring subsiding air to the region in summer, with clear skies and high temperatures. When the anticyclone moves Equator-ward in winter, it is replaced by traveling, frontal cyclones with their attendant precipitation. During summer, regions of the Mediterranean climate are strongly influenced by the subtropical ridge which keeps atmospheric conditions very dry with minimal cloud coverage. In some areas, such as coastal California ,

2940-461: The temperature and rainfall pattern for a Csa or even a Csb climate can exist as a microclimate in some high-altitude locations adjacent to a rare tropical As ( tropical savanna climate with dry summers, typically in a rainshadow region, as in Hawaii). These have a favourable climate, with mild wet winters and fairly warm, dry summers. The Mediterranean forests, woodlands, and scrub biome

3000-472: The times of Diocletian's persecution: St Domnius (Latin: Domnius ; Croatian: Duje ; Italian: Domnio ), craftsman Anastasius the Fuller , deacon Septimia, priest Asteria, and others. In the fifth Century, Salona's bishops started exercising more metropolitan duties (archbishop Hezihius), and in the sixth century they carried the archbishop title as well (arhiepiscopus), and fulfilled the duties associated with

3060-514: The title. (archbishops Stephen , Honorius and others). That means that at that time they held primary positions in western Illyria. Siscia's bishop from the region Pannonia joined the Dalmatian bishops on the synods held in Salona in the years 530 and 533 as a member with full rights. At the time of Diocletian, Salona had a population of 60,000. In 639 Salona was destroyed by the Slavs. After

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3120-702: The tropics, on Haleakalā Summit in Hawaii. In South America, Csc regions can be found along the Andes in Chile and Argentina. The town of Balmaceda, Chile is one of the few towns confirmed to have this climate. Small areas with a Csc climate can be found at high elevations in Corsica . In Norway, the small fishing village of Røstlandet , in Røst Municipality , above the Arctic Circle has

3180-452: The western coasts of landmasses, between roughly 30 and 45 degrees north or south of the equator . The main cause of Mediterranean, or dry summer, climate is the subtropical ridge , which extends towards the pole of the hemisphere in question during the summer and migrates towards the equator during the winter. This is due to the seasonal poleward-equatorward variations of temperatures. The resulting vegetation of Mediterranean climates are

3240-541: The winter and summer due to higher evapotranspiration . Toward the polar latitudes, total moisture usually increases; for instance, the Mediterranean climate in Southern Europe has more rain. The rainfall also tends to be more evenly distributed throughout the year in Southern Europe, while in places such as Southern California , the summer is nearly or completely dry. In places where evapotranspiration

3300-410: The winter, with frost and snowfall almost unknown, whereas Tashkent has cold winters with annual frosts and snowfall; or, to consider summer, Seville experiences rather high temperatures in that season. In contrast, San Francisco has cool summers with daily highs around 21 °C (70 °F) due to the continuous upwelling of cold subsurface waters along the coast. Because most regions with

3360-554: The year for climate zones at such distances from coasts. In North America, areas with Csc climate can be found in the Olympic , Cascade , Klamath , and Sierra Nevada ranges in Washington, Oregon and California. These locations are found at high altitude nearby lower altitude regions characterized by a warm-summer Mediterranean climate ( Csb ) or hot-summer Mediterranean climate ( Csa ). A rare instance of this climate occurs in

3420-570: Was the burial place of a number of Croatian kings along with other nobility, It was destroyed by the Ottoman Turks in the 16th century. The nearby Church of Saint Mary was the burial site of Mihajlo Krešimir II and his wife Jelena, the benefactress. In the 11th century, the Church of Saint Peter and Moses (known today as "hollow church") was built north of Solin, near the two churches of Saint Mary and Stephen, in which Demetrius Zvonimir

3480-622: Was crowned as king of Dalmatia and Croatia. Solin is situated on the D8 ( E65 ) Adriatic road ("Jadranska magistrala"), that becomes a 4-lane "Split bypass road" here and continues south towards Split and further down the Adriatic coast. A big roundabout south of the city centre is a major intersection with a D1 ( E59 ) road that connects the area of Split conurbation with the A1 Zagreb-Split highway. The Zagreb-Split railway passes through

3540-604: Was destroyed, and its refugees moved to the settlement in and around Diocletian's palace, "Spalatum" ( Split ), turning it into a fortified town. In the Early Middle Ages , Solin was part of Croatian territory and played an important role in the Medieval Croatian state , being one of the political centres. In the 20th century, the intensive industrialisation process of the Split basin made Solin no more than

3600-495: Was great both politically and religiously. It was the birthplace of Emperor Diocletian , who ruled the Roman Empire from 284 to 305 AD . He was born around 244, and served as a soldier and then a Roman army officer as a young man. Salona was an early Roman settlement, which became overshadowed when Diocletian constructed the nearby Diocletian's Palace in about the year 300 AD. Surviving local residents of Salona, after

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