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Giresun
Giresun () is a city in the Black Sea Region of northeastern Turkey, about west of the city of Trabzon. It is the seat of Giresun Province and Giresun District.İl Belediyesi
Turkey Civil Administration Departments Inventory. Retrieved 1 March 2023.
It has a population of 125,682 (2022).


Etymology

Giresun was known to the ancient Greeks as ''Choerades'' or more prominently as Kerasous or Cerasus (), the origin of the modern name. The name Kerasous consists of the Greek words κερασός (kerasós) "cherry" + -ουντ (a place marker). Thus, the Greek root of the word "cherry", κερασός (kerasós), predates the name of the city, and the ultimate origin of the word cherry (and thus the name of the city) is probably fro ...
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Giresun Province
Giresun Province (Greek language, Greek : Κερασούντα, ; ) is a Provinces of Turkey, province of Turkey on the Black Sea coast. Its adjacent provinces are Trabzon Province, Trabzon to the east, Gümüşhane Province, Gümüşhane to the southeast, Erzincan Province, Erzincan to the south, Sivas Province, Sivas to the southwest, and Ordu Province, Ordu to the west. Its area is 6,972 km2, and its population is 450,862 (2022). The provincial capital is Giresun. Its Vehicle registration plates of Turkey, license-plate code is 28. Geography Giresun is an agricultural region and its lower areas, near the Black Sea coast. It is Turkey's second largest producer of hazelnuts and it is famously home to the best quality hazelnuts in the world; a Giresun folk song tells "I will not eat a single hazelnut, unless you are by my side," while another tells of a lover shot dead under a hazelnut tree. Forests and pasture cover the high mountainous regions, and in places there is min ...
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Giresun District
Giresun District (also: ''Merkez'', meaning "central" in Turkish) is a district of the Giresun Province of Turkey. Its seat is the city of Giresun.İl Belediyesi
Turkey Civil Administration Departments Inventory. Retrieved 1 March 2023.
Its area is 376 km2, and its population is 145,361 (2022).


Composition

There are two in Giresun District: * Duroğlu * There are 53

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Trabzon
Trabzon, historically known as Trebizond, is a city on the Black Sea coast of northeastern Turkey and the capital of Trabzon Province. The city was founded in 756 BC as "Trapezous" by colonists from Miletus. It was added into the Achaemenid Empire by Cyrus the Great and was later part of the independent Kingdom of Pontus that challenged Rome until 68 BC. Thenceforth part of the Roman and later Byzantine Empire, the city was the capital of the Empire of Trebizond, one of the successor states of the Byzantine Empire after the Fourth Crusade in 1204. In 1461 it came under Ottoman rule. During the early modern period, Trabzon, because of the importance of its port, again became a focal point of trade to Persia and the Caucasus. Today Trabzon is the second largest city and port on the Black Sea coast of Turkey with a population of almost 300,000. The urban population of the city is 330,836 (Ortahisar), with a metropolitan population of 822,270. Name The Turkish name of the city ...
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Black Sea
The Black Sea is a marginal sea, marginal Mediterranean sea (oceanography), mediterranean sea lying between Europe and Asia, east of the Balkans, south of the East European Plain, west of the Caucasus, and north of Anatolia. It is bounded by Bulgaria, Georgia (country), Georgia, Romania, Russia, Turkey, and Ukraine. The Black Sea is Inflow (hydrology), supplied by major rivers, principally the Danube, Dnieper and Dniester. Consequently, while six countries have a coastline on the sea, its drainage basin includes parts of 24 countries in Europe. The Black Sea, not including the Sea of Azov, covers , has a maximum depth of , and a volume of . Most of its coasts ascend rapidly. These rises are the Pontic Mountains to the south, bar the southwest-facing peninsulas, the Caucasus Mountains to the east, and the Crimean Mountains to the mid-north. In the west, the coast is generally small floodplains below foothills such as the Strandzha; Cape Emine, a dwindling of the east end ...
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Humid Subtropical Climate
A humid subtropical climate is a subtropical -temperate climate type, characterized by long and hot summers, and cool to mild winters. These climates normally lie on the southeast side of all continents (except Antarctica), generally between latitudes 25° and 40° and are located poleward from adjacent tropical climates, and equatorward from either humid continental (in North America and Asia) or oceanic climates (in other continents). It is also known as warm temperate climate in some climate classifications. Under the Köppen climate classification, ''Cfa'' and ''Cwa'' climates are either described as humid subtropical climates or warm temperate climates. This climate features mean temperature in the coldest month between (or ) and and mean temperature in the warmest month or higher. However, while some climatologists have opted to describe this climate type as a "humid subtropical climate", Köppen himself never used this term. The humid subtropical climate classific ...
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Ordu
Ordu () or Altınordu is a port city on the Black Sea coast of Turkey and the capital of Ordu Province. The city forms the urban part of the Altınordu, Ordu, Altınordu district, with a population of 235,096 in 2023. Name Kotyora, the original name of the city is a legacy of indigenous Colchis, Colchians. The name is allegedly composed of an old Laz language word for pottery ('Koto', similar to Mingrelian language, Mingrelian 'Koto', Georgian language, Georgian 'Kotani' and Laz 'Katana') and a common Kartvelian languages, Kartvelian suffix indicating belonging ('Uri'). In Zan languages, Zan (aka Colchian) Kotyora means a place where pottery is made. This point is supported with several other Kartvelian place names existing in the region as well as the region itself historically being known as Beyliks of Djanik, Djanik (Djani being another name for Laz). The city was also historically known as ''Cotyora'' or ''Kotyora'' (). The contemporary name of Ordu meaning 'army camp' in O ...
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Cherry
A cherry is the fruit of many plants of the genus ''Prunus'', and is a fleshy drupe (stone fruit). Commercial cherries are obtained from cultivars of several species, such as the sweet '' Prunus avium'' and the sour '' Prunus cerasus''. The name 'cherry' also refers to the cherry tree and its wood, and is sometimes applied to almonds and visually similar flowering trees in the genus ''Prunus'', as in " ornamental cherry" or " cherry blossom". Wild cherry may refer to any of the cherry species growing outside cultivation, although ''Prunus avium'' is often referred to specifically by the name "wild cherry" in the British Isles. Botany True cherries ''Prunus'' subg. ''Cerasus'' contains species that are typically called cherries. They are known as true cherries and distinguished by having a single winter bud per axil, by having the flowers in small corymbs or umbels of several together (occasionally solitary, e.g. ''P. serrula''; some species with short racemes, ...
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Lake-effect Rain
Lake-effect rain, or bay-effect rain, is the liquid equivalent of lake-effect snow, where the rising air results in a transfer of warm air and moisture from a lake into the predominant colder air, resulting in a fast buildup of clouds and rainfall downwind of the lake. If the air temperature is not low enough to keep the precipitation frozen, it falls as a lake-effect rain. In order for lake-effect rain to form, the air moving across the lake must be significantly cooler than the air over the Sea surface temperature, water surface. The resulting rain bands can accumulate to can cause localized flash flooding, thunder, lightning and even waterspouts in extreme events. Although the effect is associated with the North American Great Lakes, it can occur downwind of any List of lakes by area, large lake that can hold its summer heat well into the cooler days of autumn and early winter. Another similar effect is sea-effect or ocean-effect rain, which is caused by three primary component ...
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Snow
Snow consists of 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 Sublimation (phase transition), sublimate away. Snowstorms organize and develop by feeding on sources of atmospheric moisture and cold air. Snowflakes Nucleation, nucleate around particles in the atmosphere by attracting supercooling, supercooled water droplets, which Freezing, freeze in hexagonal-shaped crystals. Snowflakes take on a variety of shapes, basic among these are platelets, needles, columns, and Hard rime, rime. As snow accumulates into a snowpack, it may blow into drifts. Over time, accumulated snow m ...
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Trewartha Climate Classification
The Trewartha climate classification (TCC), or the Köppen–Trewartha climate classification (KTC), is a climate classification system first published by American geographer Glenn Thomas Trewartha in 1966. It is a modified version of the Köppen–Geiger system, created to answer some of its deficiencies. The Trewartha system attempts to redefine the middle latitudes to be closer to vegetation zoning and genetic climate systems. Scheme Trewartha's modifications to the 1884 Köppen climate system sought to reclass the middle latitudes into three groups, according to how many months have a mean temperature of or higher: * ''C'' (subtropical)—8 or more months; * ''D'' (temperate)—4 to 7 months; * ''E'' ( boreal climate)—1 to 3 months. The tropical climates and polar climates remained the same as in the original Köppen climate classification. The "highland" climate is ambiguously defined. Newer users of KTC generally omit this option. Group A: Tropical climates This is ...
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Köppen Climate Classification
The Köppen climate classification divides Earth climates into five main climate groups, with each group being divided based on patterns of seasonal precipitation and temperature. The five main groups are ''A'' (tropical), ''B'' (arid), ''C'' (temperate), ''D'' (continental), and ''E'' (polar). Each group and subgroup is represented by a letter. All climates are assigned a main group (the first letter). All climates except for those in the ''E'' group are assigned a seasonal precipitation subgroup (the second letter). For example, ''Af'' indicates a tropical rainforest climate. The system assigns a temperature subgroup for all groups other than those in the ''A'' group, indicated by the third letter for climates in ''B'', ''C'', ''D'', and the second letter for climates in ''E''. Other examples include: ''Cfb'' indicating an oceanic climate with warm summers as indicated by the ending ''b.'', while ''Dwb'' indicates a semi-Monsoon continental climate, monsoonal continental climate ...
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