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Karaburun-Sazan Marine Park

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Karaburun-Sazan Marine Park ( Albanian : Parku Detar Karaburun-Sazan ) is a marine park in the Vlorë County of southwestern Albania . The marine park encompasses over 125.70 km (48.53 sq mi) and comprises the boundaries of both the Peninsula of Karaburun and the Island of Sazan . It is home to a vast array of landforms , including mountains , caves , islands , depressions , bays , cliffs , canyons and rocky coasts , all contributing to an exceptionally considerable biological diversity . The marine park has been identified as an Important Bird and Plant Area , because it supports immense bird and plant species. Containing ecosystems and habitats that are specific to the Mediterranean Basin , the convention of Barcelona has classified the marine park as a Specially Protected Areas of Mediterranean Importance .

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66-567: The Karaburun Peninsula is mostly hilly and a geological continuation of the Ceraunian Mountains , a mountain range rising immediately along the Ionian Sea . Its crests combine a northwest–southeast line with a series of distinct peaks along its irregular structure that are broken apart by steep and irregular slopes. The coastal landscape is marked by a rough relief and calcareous limestone cliffs , that dips vertically into

132-891: 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

198-456: 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

264-613: 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

330-555: A dominance of lentisk , kermes oak and Phoenicean juniper . The western coasts of are incised by caves and canyons and characterized by high vertical cliffs that appear underwater at great depths. The cliffs are mostly dotted by sea fennel , statice and caper bush . Moreover, Mediterranean tapeweed hosts macrofauna such as sponges , cnidarias , bryozoas , molluscas and many countless others. Karaburun Peninsula, Albania The Karaburun Peninsula ( Albanian : Gadishulli i Karaburunit ), also known as Cape Linguetta ,

396-668: 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

462-556: 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

528-544: 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 a 40 mm (1.6 in) level. The third letter indicates

594-491: A narrow natural channel , separates the peninsula from the island. Sazan is the largest island in the country, having a length of 4.8 km (3.0 mi) and a width of 2.7 km (1.7 mi), with a surface area of 5.7 km (2.2 sq mi). It is surrounded by the Adriatic Sea in the north and the Ionian Sea in the south. The peninsula was shaped into its current form over several geological eras with

660-606: 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

726-528: A number of mountains that rises to an elevation of 800 metres (2,600 ft) above the Adriatic . In the west, the mountains in the peninsula falls steeply into the Ionian Sea . The most elevated natural points are Maja e Shendelliut at 1,499.5 metres (4,920 ft), Maja Ali Hila at 1,318 metres (4,324 ft), Maja e Ilqes at 733 metres (2,405 ft), Maja e Flamurit at 826 metres (2,710 ft) and Maja Çadëri at 839 metres (2,753 ft). The Mesokanali,

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792-550: 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

858-409: A vast array of habitats which in turn are home to a diverse wildlife. The fauna is represented by several threatened and endangered species such as the loggerhead and green sea turtle but also the mediterranean monk seal , the rarest seal species in the world. The landmass of the peninsula is designated as nature reserve , while the shoreline and its surrounding sea waters are part of

924-447: A vast array of invertebrates represented with 167 species. The diverse landscapes of the park, with an exceptionally considerable marine and terrestrial life free of any marks of human disturbance, maintain a particular appeal. The park is home to an incredible array of mammal species whose numbers are more than 70. The most common are the golden jackal , wildcat , chamois , roe deer , wild boar , badger and otter . A few of

990-597: 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

1056-744: Is a peninsula of the Mediterranean Sea located in Southern and Southeastern Europe , which is almost completely surrounded by both the Adriatic Sea to the north and the Ionian Sea to the south. It is located in Southwestern Albania along the Albanian Ionian Sea Coast , whereas the Strait of Otranto separates it from Italy . The Strait of Mezokanal separates the peninsula from Sazan Island , while in

1122-424: 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

1188-658: Is essentially composed of limestone rocks, that has been formed during the Burdigalian age . The optimal conditions, in terms of geology and hydrology as well as the Mediterranean climate with subtropical influences, have created diverse habitats that in turn provide favourable circumstances for the equally diverse mix of plants and animals that thrive in the area. The park is home to at least 70 species of mammals , 144 species of birds , 36 species of reptiles and 11 species of amphibia . It also contains

1254-576: 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

1320-796: 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 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

1386-406: 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

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1452-425: Is not well understood. Sea turtles , seals , and dolphins are considered to reside in the park area, although sufficient regularity of occurrences is unclear. Three primary species of sea turtles are to be found along the pristine beaches of the park such as the loggerhead sea turtle , green sea turtle and leatherback sea turtle . Dolphins such as the short-beaked common dolphin , common bottlenose dolphin and

1518-459: The Adriatic and Ionian Sea . The marine park is located near military bases, so permission may be required from local authorities first. The hiring of a professional local diver for serving as tour guide is thoroughly recommended. Roads are in inaccessible, and the only ways to reach the above areas are by sea or through all day hiking. The Karaburun-Sazan Marine Park is strategically located in

1584-679: The Albanian Ionian Sea Coast . Running towards the Llogara Pass , the mountains gets divided into two mountain chains . Reza e Kanalit encompasses the southern portion of the Karaburun Peninsula. It is marked by a narrow and steep platform, extending from the peninsula to the Dukat Valley close to Orikum . The mountains are about 24 km (15 mi) long and about 4–7 km (2.5–4.3 mi) wide. The marine park's mountainous terrain and its geographic features result in

1650-464: The endangered sperm whale has been reported in the waters of the park. Outstanding is the mediterranean monk seal , one of the most endangered mammals in the world, mostly seek refuge in the inaccessible caves and canyons of the park. The marine area is characterised by exceptionally rich and varied flora. The coasts along Karaburun and Sazan are rocky with significant calcareous limestone cliffs , properly covered with Mediterranean maquis with

1716-630: The marine park . In 2014, the Regina Blu ferry was established by a Radhime-based hotel owner making trips between the peninsula and the island of Sazan , while stopping along the secluded beaches. The peninsula belongs to the Sazan Zone that is a constituent of the Albanides tectonic unit. Albanides form the link between Dinarides and Hellenides orogenic belts. They are considered allocthonous and mobilist theories deduce they come from

1782-415: 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

1848-604: 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

1914-466: The Ionian Sea. Karaburun peninsula is sometimes called Ceraunian Peninsula due to the name of the mountain range. Formed during the mesozoic era of the cretaceous and paleogene period, the crests of the mountain range form a northwest-southeast line with a series of distinct peaks along its irregular structure that are broken apart by steep and unequally slopes. The highest peaks are namely,

1980-459: 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 the precipitation pattern (" s " represents dry summers). Köppen has defined a dry summer month as

2046-465: The Maja Çaderës, Maja e Flamurit, Maja e Koretës and Maja e Ilqes. The western section comprises a rough relief and is dotted with sandy and rocky beaches , sea caves , steep cliffs and several bays amongst them Cave of Haxhi Ali , Cape of Gjuhëz , Bay of Skaloma , Bay of Arushë , Bay of Dafinë , and most notably Bay of Grama , where ships and vessels anchored during classical antiquity . On

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2112-782: 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

2178-447: 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 ,

2244-448: 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

2310-616: The area being of high interest to both visitors and researchers. It experiences a mediterranean climate . This means that the winters are rainy and dry, and the summers are warm to hot. Mean monthly temperature ranges between 8–10  °C (46–50  °F ) (in January) and 24–26 °C (75–79 °F) (in July). Mean annual precipitation ranges between 1,000 millimetres (39 inches) and 1,200 millimetres (47 inches) depending on geographic region and prevailing climate type. The relief comprises

2376-431: 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

2442-400: The coast) of desert and semi-arid climates , and equatorward of oceanic climates . Mediterranean climate zones are typically located along 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

2508-434: 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,

2574-440: 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 the Köppen classification, dry-summer climates ( Csa , Csb ) usually occur on

2640-399: The east. These formations have been continuously under the effect of Karst and are exploited as marble (metamorphosed limestone) since antiquity. The widespread Karst topography is responsible for the absence of potable water and thus the absence of any population on the peninsula. Despite the dry surface and upper soil layers, there are several water sources that pour deep directly into

2706-561: The eastern shore of the Strait of Otranto . It lies primarily between latitudes 40° and 26° N and longitudes 19° and 18° E. The marine park comprises 125.70 km (48.53 sq mi) in Vlorë County in southwestern Albania . The marine park includes the Karaburun Peninsula with Reza e Kanalit and Sazan Island . In terms of geology , the peninsula belongs to the Ceraunian Mountains , which rises steeply along

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2772-557: 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

2838-464: The high and steep rock faces of the bay, which served also as a marble quarry, there are hundreds of rock inscriptions dating back to the 4th century BC. Under the Köppen climate classification , the peninsula experiences a mediterranean climate with hot summers and generally warm to cool, dry winters. The ideal climate and contrasting landscapes located at the sea have favored the development of

2904-706: 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

2970-404: The island is inhabited by 15 species of mammals , 39 species of birds , 8 species of reptiles , 1 species of amphibia and as well as 122 species of invertebrates. The marine park features ruins of sunken ancient Greek , Roman and World War II ships, rich underwater fauna , steep cliffs and giant caves , ancient inscriptions of sailors on shore, secluded beaches and scenic views of

3036-435: 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 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

3102-432: 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,

3168-530: 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

3234-650: 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

3300-421: The sea. The geological evolution has formed also capes such as Galloveci cape and Kepi i Gjuhëzës , as well as a total number of 20 caves along the whole coast. 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

3366-472: The sea. The uninhabited Sazan Island is primarily made up of limestone rocks, which was formed during the Cretaceous period. The waters of Mezokanal in the south separate the island from the peninsula. The most characteristic feature of the island is its unique climate. The island's climate is not mediterranean but rather subtropical on account of its warm winters and hot summers, resembling those of

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3432-462: The smaller mammals typically include the red squirrel , hazel dormouse and pine vole . There are 8 species of bats to be found merely in the island of Sazan . Several of them, like the Kuhl's and Nathusius's pipistrelle , are widespread and common, while others, like the Mediterranean long-eared bat , are relatively rare and restricted in distribution. The biodiversity of the local oceanic fauna

3498-453: 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 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

3564-419: 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

3630-546: 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

3696-886: The south of Crete , of Tunisia and Egypt . The marine park contains diverse landforms offering favourable conditions for a great vegetation and biodiversity. In terms of phytogeography , it falls completely within the Illyrian deciduous forests terrestrial ecoregion , of the Palearctic Mediterranean forests, woodlands, and scrub biome . The marine park is distinguished for its diversity of habitats and its richness in flora and fauna . Hundreds of species of mammals, birds, fish, and reptiles have been documented, including several that are either endangered or threatened . Almost 55 species of mammals , 105 species of birds , 28 species of reptiles and 10 species of amphibia are known to occur within peninsula, while

3762-520: The southeast stretches the Bay of Vlorë . In classical antiquity , its name was the "Akrokeraunian Peninsula" (Ακροκεραύνιο ακρωτήριο), whose name was derived from the eponymous Akrokeraunian mountains ; this is because, in terms of geology , the Rrëza e Kanalit on the peninsula represent the continuation of said mountains, which are the highest and most extensive mountain range system that extends parallel to

3828-564: 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 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

3894-537: 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 ,

3960-531: The tectonic merging of Paleozoic schist formations, Mesozoic limestone and marble deposits. It is principally made up of carbonic limestone from the Mesozoic period, while the northwest is composed of terrigenous sediment . The south is chiefly composed of Pliocene rock formations and a variety of sediments . The rocks found in the west of the Sazan Island are primarily Cretaceous rocks. The east

4026-461: 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

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4092-702: 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

4158-457: 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 the subtropics also meet Cs requirements, though they, too, are not normally associated with Mediterranean climates. The same goes for

4224-541: 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

4290-410: 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

4356-554: 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

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