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Gabú
Gabu is the largest town in eastern Guinea-Bissau and capital of the Gabu Region. History From 1537, the town was the centre of the eponymous kingdom of Kaabu, also written Ngabou or N’Gabu. Its population was originally a Mandé people from what is currently Mali, and the kingdom was initially vassal to the Mali Empire. As the latter waned, Sama Koli, Gabu's governor, proclaimed himself king, but maintained many of the trappings of Malian cultural heritage. The kingdom built earthen ramparts around the settlement (now vanished) and established trade relations with the Portuguese on the coast. In the early nineteenth century, the Fula ethnic group converted to Islam and began the Kansala War to end Mandé dominance. It ended with a big fire which caused extensive damage and casualties on both sides. Gabu there after became linked with the Imamate of Futa Jallon and was finally assimilated into the Portuguese Empire. The Portuguese named the town "Nova Lamego" ie "New Lam ...
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Gabu Region
Gabú Region is the easternmost region in Guinea-Bissau. Its capital is Gabú. The region borders Senegal to the north, Guinea to the east and south and the Guinea-Bissau regions of Tombali and Bafatá to the west. It covers an area of 9,150 km2, making it the largest of Guinea-Bissau's administrative regions. It is an inland region covered with savannah or light savannah woodland and receives an annual rainfall of more than . As of 2009, the total population of the region was 205,608, with the urban population being 51,211 and rural being 154,397. The sex ratio of the region is 94 females for every hundred males. As of 2009, the net activity rate was 72.44 per cent, proportion of employed labour force was 43.86 per cent, proportion of labour force was 74.48 and the proportion of potentially active population was 43.86 per cent. The absolute poverty rate, people earning less than $2 a day, in the region stood at 72.4 per cent, with a regional contribution of 13.6 per cent ...
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Guinea-Bissau
Guinea-Bissau ( ; pt, Guiné-Bissau; ff, italic=no, 𞤘𞤭𞤲𞤫 𞤄𞤭𞤧𞤢𞥄𞤱𞤮, Gine-Bisaawo, script=Adlm; Mandinka: ''Gine-Bisawo''), officially the Republic of Guinea-Bissau ( pt, República da Guiné-Bissau, links=no ), is a country in West Africa that covers with an estimated population of 1,726,000. It borders Senegal to the north and Guinea to the south-east. Guinea-Bissau was once part of the kingdom of Kaabu, as well as part of the Mali Empire. Parts of this kingdom persisted until the 18th century, while a few others were under some rule by the Portuguese Empire since the 16th century. In the 19th century, it was colonised as Portuguese Guinea. Portuguese control was restricted and weak until the early 20th century with the pacification campaigns, these campaigns solidified Portuguese sovereignty in the area. The final Portuguese victory over the remaining bastion of mainland resistance, the Papel ruled Kingdom of Bissau in 1915 by the Portu ...
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Regions Of Guinea-Bissau
Guinea-Bissau is divided into 8 regions (singular: ''região'', plural: ''regiões'') and 1 autonomous sector (''sector autónomo''). The regions are subdivided into a total of 37 sectors (singular: ''setor'', plural: ''setores'') ; which are further subdivided into smaller groups called ''sections'' (singular: ''secção'', plural: ''secções''); which are further subdivided into populated places (i.e.: towns, villages, localities, settlements, communities, etc.). Here are the following listed below: Regions The regions can also be grouped into 3 provinces: * ''Leste'' (East): Bafatá, Gabu * ''Norte'' (North): Biombo, Cacheu, Oio * ''Sul'' (South): Bolama, Quinara, Tombali See also *List of regions of Guinea-Bissau by Human Development Index This is a list of regions of Guinea-Bissau by Human Development Index as of 2019 with data for the year 2019. See also *List of countries by Human Development Index References {{Subnational entities by Human Development Ind ...
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Flag Of Guinea-Bissau
The national flag of Guinea-Bissau was adopted in 1973 when independence from Portugal was proclaimed. Gallery File:Flag of Portuguese Guinea (proposal).svg, Proposed flag for the Portuguese Guinea (1965) File:Flag of PAIGC.svg, Flag of PAIGC Military flag of Guinea-Bissau.svg, Flag of the Armed Forces Design Like the former flag of Cape Verde, the flag is based on that of the African Party for the Independence of Guinea and Cape Verde (PAIGC). The party was established in 1956 to peacefully campaign for independence from Portugal during its Estado Novo regime, but turned to armed conflict in the 1960s and was one of the belligerents in the 1963–74 Guinea-Bissau War of Independence. It is still the dominant party in Guinea-Bissau. The PAIGC party flag was derived from that of Ghana, which was the first design to use the Pan-African combination of red, yellow, green, and black in 1957. In the Ghanaian view, the black star stands for the unity of Africa. Red stands fo ...
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Tropical Savanna Climate
Tropical savanna climate or tropical wet and dry climate is a tropical climate sub-type that corresponds to the Köppen climate classification categories ''Aw'' (for a dry winter) and ''As'' (for a dry summer). The driest month has less than of precipitation and also less than 100-\left (\frac \right)mm of precipitation. This latter fact is in a direct contrast to a tropical monsoon climate, whose driest month sees less than of precipitation but has ''more'' than 100-\left (\frac \right) of precipitation. In essence, a tropical savanna climate tends to either see less overall rainfall than a tropical monsoon climate or have more pronounced dry season(s). In tropical savanna climates, the dry season can become severe, and often drought conditions prevail during the course of the year. Tropical savanna climates often feature tree-studded grasslands due to its dryness, rather than thick jungle. It is this widespread occurrence of tall, coarse grass (called savanna) which has led to ...
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Thunderstorm
A thunderstorm, also known as an electrical storm or a lightning storm, is a storm characterized by the presence of lightning and its acoustic effect on the Earth's atmosphere, known as thunder. Relatively weak thunderstorms are sometimes called thundershowers. Thunderstorms occur in a type of cloud known as a cumulonimbus. They are usually accompanied by strong winds and often produce heavy rain and sometimes snow, sleet, or hail, but some thunderstorms produce little precipitation or no precipitation at all. Thunderstorms may line up in a series or become a rainband, known as a squall line. Strong or severe thunderstorms include some of the most dangerous weather phenomena, including large hail, strong winds, and tornadoes. Some of the most persistent severe thunderstorms, known as supercells, rotate as do cyclones. While most thunderstorms move with the mean wind flow through the layer of the troposphere that they occupy, vertical wind shear sometimes causes a de ...
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Wet Season
The wet season (sometimes called the Rainy season) is the time of year when most of a region's average annual rainfall occurs. It is the time of year where the majority of a country's or region's annual precipitation occurs. Generally, the season lasts at least a month. The term ''green season'' is also sometimes used as a euphemism by tourist authorities. Areas with wet seasons are dispersed across portions of the tropics and subtropics. Under the Köppen climate classification, for tropical climates, a wet season month is defined as a month where average precipitation is or more. In contrast to areas with savanna climates and monsoon regimes, Mediterranean climates have wet winters and dry summers. Dry and rainy months are characteristic of tropical seasonal forests: in contrast to tropical rainforests, which do not have dry or wet seasons, since their rainfall is equally distributed throughout the year.Elisabeth M. Benders-Hyde (2003)World Climates.Blue Planet Biomes. Retr ...
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Harmattan
The Harmattan is a season in West Africa that occurs between the end of November and the middle of March. It is characterized by the dry and dusty northeasterly trade wind, of the same name, which blows from the Sahara over West Africa into the Gulf of Guinea. The name is related to the word in the Twi language. The temperature is cold in most places, but can also be hot in certain places, depending on local circumstances. The Harmattan blows during the dry season, which occurs during the months with the lowest sun. In this season the subtropical ridge of high pressure stays over the central Sahara and the low-pressure Intertropical Convergence Zone (ITCZ) stays over the Gulf of Guinea. On its passage over the Sahara, the Harmattan picks up fine dust and sand particles (between 0.5 and 10 microns). It is also known as the "doctor wind", because of its invigorating dryness compared with humid tropical air. Effects This season differs from winter, because it is characterized ...
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Dry Season
The dry season is a yearly period of low rainfall, especially in the tropics. The weather in the tropics is dominated by the tropical rain belt, which moves from the northern to the southern tropics and back over the course of the year. The temperate counterpart to the tropical dry season is summer or winter. Rain belt The tropical rain belt lies in the southern hemisphere roughly from October to March; during that time the northern tropics have a dry season with sparser precipitation, and days are typically sunny throughout. From April to September, the rain belt lies in the northern hemisphere, and the southern tropics have their dry season. Under the Köppen climate classification, for tropical climates, a dry season month is defined as a month when average precipitation is below . The rain belt reaches roughly as far north as the Tropic of Cancer and as far south as the Tropic of Capricorn. Near these latitudes, there is one wet season and one dry season annually. At the ...
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Diurnal Temperature Variation
In meteorology, diurnal temperature variation is the variation between a high air temperature and a low temperature that occurs during the same day. Temperature lag Temperature lag is an important factor in diurnal temperature variation: peak daily temperature generally occurs ''after'' noon, as air keeps net absorbing heat even after noon, and similarly minimum daily temperature generally occurs substantially after midnight, indeed occurring during early morning in the hour around dawn, since heat is lost all night long. The analogous annual phenomenon is seasonal lag. As solar energy strikes the Earth's surface each morning, a shallow layer of air directly above the ground is heated by conduction. Heat exchange between this shallow layer of warm air and the cooler air above is very inefficient. On a warm summer's day, for example, air temperatures may vary by from just above the ground to waist height. Incoming solar radiation exceeds outgoing heat energy for many hours afte ...
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Bissau
Bissau () is the capital, and largest city of Guinea-Bissau. Bissau had a population of 492,004. Bissau is located on the Geba River estuary, off the Atlantic Ocean, and is Guinea-Bissau's largest city, major port, and its administrative and military centre. Etymology The term Bissau may have come from the name of a clan N'nssassun, in its plural form Bôssassun.direct link to pdf Intchassu (Bôssassu) was the name given to the nephew of King Mecau—the first sovereign of the island of Bissau—, son of his sister Pungenhum. Bôssassu formed a clan of the Papel peoples. History The city was founded in 1687 by Portugal as a fortified port and trading center. In 1942 the capital of Portuguese Guinea was transferred from Bolama to Bissau. After the declaration of independence by the anti-colonial guerrillas of PAIGC in 1973, the capital of the rebel territories was declared to be Madina do Boe, while Bissau remained the colonial capital. When Portugal granted independence, fo ...
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Köppen Climate Classification
The Köppen climate classification is one of the most widely used climate classification systems. It was first published by German-Russian climatologist Wladimir Köppen (1846–1940) in 1884, with several later modifications by Köppen, notably in 1918 and 1936. Later, the climatologist Rudolf Geiger (1894–1981) introduced some changes to the classification system, which is thus sometimes called the Köppen–Geiger climate classification system. The Köppen climate classification divides climates into five main climate groups, with each group being divided based on seasonal precipitation and temperature patterns. 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'' indi ...
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