Geography of Cape Verde
Cape Verde (formally, the Republic of Cabo Verde) is a group of arid Atlantic islands which are home to a number of birds and reptiles and constitute a unique ecoregion in the World Wildlife Fund classification.
Location and description
The Cape Verde Islands are located in the mid-Atlantic Ocean some 570 km (354 mi) off the west coast of the continent of Africa. The landscape varies from dry plains to high active volcanoes with cliffs rising steeply from the ocean. The climate is arid.
The archipelago consists of ten (10) islands and five (5) islets, divided into the windward (Barlavento) and leeward (Sotavento) groups. The six (6) islands in the Barlavento group are Santo Antão, São Vicente, Santa Luzia, São Nicolau, Sal, and Boa Vista. The islands in the Sotavento group are Maio, Santiago, Fogo, and Brava. All but Santa Luzia are inhabited.
Three islands – Sal, Boa Vista, and Maio – generally are level and lack natural water supplies. Mountains higher than 1,280 metres (4,199 ft) are found on Santiago, Fogo, Santo Antão, and São Nicolau.
Sand carried by high winds has caused erosion on all islands, especially the windward ones. Sheer, jagged cliffs rise from the sea on several of the mountainous islands. The lack of natural vegetation in the uplands and coast also contributes to soil erosion. Only the interior valleys support natural vegetation.
- Geographic coordinates
- 16°N 24°W / 16°N 24°W
- Total: 4,072 km2
- Land: 4,072 km2
- Water: 0 km2
- Area – comparative
- US: slightly larger than Rhode Island
- Canada: slightly larger than the Queen Charlotte Islands
- UK: slightly larger than Suffolk
- 965 km
- Maritime claims
- Measured from claimed archipelagic baselines
- Territorial sea: 12 nmi (22.2 km)
- Contiguous zone: 24 nmi (44.4 km)
- Exclusive economic zone: 200 nmi (370.4 km)
- Exclusive economic zone
- EEZ area: 800,561 km2
- Continental shelf: 5,591 km2
- Coral reefs: 0.09% of world
- Sea mounts: 0.04% of world
- source: Sea Around Us Project's Countries' EEZ
- Steep, rugged, rocky, volcanic.
- Elevation extremes
- Lowest point: Atlantic Ocean 0 m
- Highest point: Mount Fogo 2,829 m (a volcano on Fogo Island)
- Natural resources
- Salt, basalt rock, limestone, kaolin, fish. clay, gypsum
- Land use
- Arable land: 11.66%
- Permanent crops: 0.74%
- Other: 87.59% (2012)
- Irrigated land
- 34.76 km2 (2004)
- Total renewable water resources
- 0.03 km3 (2011)
- Freshwater withdrawal (domestic/industrial/agricultural)
- total: 0.02 km3/yr (6%/1%/93%)
- per capita: 48.57 m3/yr (2004)
- Natural hazards
- Prolonged droughts; seasonal harmattan wind produces obscuring dust; volcanically and seismically active.
- Geography - note
- Strategic location 500 km from west coast of Africa near major north-south sea routes; important communications station; important sea and air refueling site.
Table of islands
Cabo Verde shares maritime boundaries with Mauritania and Senegal. Cabo Verde has signed treaties with Senegal and Mauritania delimiting the specific boundaries. However, the two treaties conflict in their delimitation of the precise borders.
|Climate chart (explanation)|
A cold Atlantic current produces an arid atmosphere around the archipelago. December–June is cool and dry, with temperatures at sea level averaging 21 °C (69.8 °F); July–November is warm and dry, with temperatures averaging 27 °C (80.6 °F). Although some rain comes during the latter season, rainfall is sparse overall and very erratic. Accumulations are generally around 130 mm (5.12 in) annually in the northern islands and 300 mm (11.81 in) in the south. The archipelago is subject to cyclical droughts; a devastating drought began in 1968 and was broken only briefly in 1975, 1978, 1984, and 1986.
Rainfall is irregular, historically causing periodic droughts and famines. (Desalination plants now provide water to more than half the country's population. Experiments with fog collectors have been conducted since 1962, however, such collectors had not been expanded beyond the Serra Malagueta community of Santiago Island, as of 2009.) The average precipitation per year in Praia is 240 mm (9.45 in). During the winter, storms blowing from the Sahara sometimes form dense dust clouds that obscure the sun; however, sunny days are the norm year round. The clearest skies are found between February and June, with very little rainfall during these months. Saharan dust, Harmattan wind, laden dust from the Sahara. This occurs between November and March and is generally similar to the "Calima" affecting the Canary Islands.
The ocean near Cabo Verde is an area of tropical cyclone formation; since these storms have the whole Atlantic over which to develop as they move westward, they are among the most intense hurricanes, and are called Cape Verde-type hurricanes.
The Cape Verde islands are a very degradated area. Also, most islands do not always get a monsoon. In fact, it is not surprising that some atmospheric precipitation of islands are limited in tropical rain.
If rain arrives, it is usually between August and October. The first "rainy season" brings high temperatures and high humidity that condenses as dew mountain. The other rainy season is between December and June, when the northeast trade winds are common during this season, only altitudes above 600m tend to receive regular rain. The island of Sal receives an average of 0.0mm in May. When the rain comes, if it comes, it can be very strong. Half of the rain in a particular year can often fall into a single storm. Most of the Cape Verde islands are dry, but on islands with high mountains and farther away from the continental land mass, by orography, the humidity is much higher, giving a rainforest habitat, very degraded by the strong human presence. Northeastern slopes of high mountains often receive a lot of rain and southwestern slopes do not. This is because they are umbria areas, situated in the north hillsides or slopes of the mountainous areas, oriented behind the sun in the Northern Hemisphere, in the shadyside orographic. So the amount of solar radiation that it receive is much lower than it would if it had without the island's relief which intercepts much of the sun. In terms of botanical ecology, these umbria areas are identified as being cool and moist.
The current north of the Canaries, has a cooling effect on the islands of Cabo Verde, making the air temperature more bearable than it would expect in any case at this latitude. Conversely, the islands do not receive the upwellings (cold streams) that affect the West African coast, so the air temperature is cooler than in Senegal, but the sea is actually warmer, because the orographic relief of some islands, such as Sao Miguel with steep mountains, cover it with rich woods and luxuriant vegetation where the humid air condenses and soak the plants, rocks, soil, logs, moss etc.
Hurricanes often begin their training in the waters around the islands of Cabo Verde, but it is rare that the strength of the storm reaches close to the islands. A Cape Verde type hurricane is formed in the area south of the islands, near Sao Miguel, after a tropical wave on the African continent during the rainy season. The storm picks up strength when it crosses the warm waters of Atlantic.
The laurel forest is a type of cloud forest, the cloud forests, are developed preferably about mountains, where the dense moisture from the sea or ocean, is precipitated by the action of the relief. Opposing the terrain to a front of warm, moist air mass, it forces to increase the height above sea level of that body wet and warm air mass, which cools and decreases the dew point, causing it to condense part of the moisture that falls as rain or fog, creating a habitat especially cool, saturated with moisture in the air and soil.
It is the balance between the dry and warm influence of the subtropical anticyclone, hot and dry summer and orography the responsible for carrying cool wet. As latitude increases, this increases the impact of the storms, which in its journey from west to east, swept the western coasts of continents, dumping heavy rains as carrying high humidity. Precipitation multiply if these air masses are crossing mountains in the way. The resulting climate is wetter, but with an annual oscillation of the temperature moderated by the proximity of the ocean. Appear mostly occupying favorable areas named geographically Umbrias, this is north hillsides or slopes of the mountainous areas that are oriented behind the sun, because the islands are in the Northern Hemisphere, between 600 and 1500 meters, thus benefiting from the humidity provided by the trade winds to form such a sea of clouds. In its botanical ecology, the mountain umbria is identified with cool and moisture.
Cape Verde is the driest archipelago of the ecoregion of Macaronesia. That with a greater influence of African species due to its geographical location near the African mainland of the Sahel. At first, the islands of Cabo Verde housed an extensive savanna and dry forest cover, but mostly it was removed to convert to agricultural land, which, together with the arid climate and rugged terrain, has led to a soil erosion and desertification widespread. However, the archipelago can be divided into four broad ecological zones (arid, semiarid, subhumid and humid), according to altitude and average annual rainfall ranging from 200 mm in the arid areas of the coast to more than 1 000 mm in the humid mountain. Mostly rainfall precipitation is due to condensation of the ocean mist. Today much of the forest cover comprises relatively immature agroforestry plantations, in which are used non-native species such as Prosopis juliflora, Leucaena leucocephala and Jatropha curcas. The native laurel forest species are in wet area only in mountainous areas.
On the lower and drier islands the vegetation before human colonization consisted of savanna or steppe vegetation, with the flattest inland portion supporting semi-desert plants. At higher altitudes, a form of arid shrubland was also present. Once this islands were covered with savanna on the plains and arid shrubland on the mountainsides, but over 500 years of human habtitation, since colonisation by the Portuguese in the 15th century, nearly all the original vegetation has been cleared by widespread agriculture including the grazing of goats, sheep and cattle and the planting of imported crop species. There are some remaining patches of dry forest high on steep mountainside including a number of endemic plant species, but these are inaccessible and hard to study.
On the higher islands and somewhat wetter islands, exclusively in mountainous areas, like Santo Antao island, the climate is suitable for the development of dry monsoon forest, and laurel forest as this vegetation is believed to have been present in the past. However, most vegetation has now been converted to agriculture and forest fragments are now restricted to areas where cultivation is not possible, such as mountain peaks and steep slopes. The demand for wood has resulted in deforestation and desertification.
Of particular note is the endemic type of humid subtropical laurel forest of macaronesian laurisilva, found on several of the Macaronesian islands of the North Atlantic and Macaronesian African mainland enclaves, namely Madeira Islands, the Azores, Cape Verde Islands and the Canary Islands, a relict of the Pliocene subtropical forests, supporting numerous endemic species.
This laurisilva forests are found in the islands of Macaronesia in the eastern Atlantic, in particular the Azores, Madeira Islands, and western Canary Islands, from 400 m to 1200 m elevation. Trees of the genera Apollonias (Lauraceae), Ocotea (Lauraceae), Persea (Lauraceae), Clethra (Clethraceae), Dracaena (Ruscaceae), and Picconia (Oleaceae) are characteristic. The Madeira Islands laurel forest was designated a World Heritage Site by UNESCO in 1999.
There are four endemic bird species including the Raso lark along with more common swifts, larks, warblers, and sparrows. The islands are an important breeding site for seabirds including the Cape Verde shearwater and Fea's petrel (Pterodroma feae), which breeds only here and in Madeira. Santiago Island holds the only breeding site of the endemic and critically endangered Bourne's heron. The 11 endemic reptile species include a giant gecko (Tarentola gigas), and there are other geckos and skinks in abundance. The giant skink (Macroscincus coctei) is now thought to be extinct.
Threats and protection
Almost all of the natural environment has been destroyed by conversion to agriculture and logging for firewood, as well as natural soil erosion, all of which has threatened several species of birds and reptiles. The remaining original forest exists at high altitudes only. Newer problems include illegal beach sand extraction and overfishing while the nesting birds are vulnerable to introduced mammals including cats and rats.
Visiting the ecoregion
The higher altitudes of the islands are accessible on the islands of Fogo, where there is a road to the volcano and walks up to the crater, and the mountainous Santo Antão where there are hiking routes.
- "BBC". BBC. Retrieved 2010-06-26.
- "What do you do when your island runs out of water?". Deutsche Welle. 2017-05-26.
- "Cape Verde: Desalination against aridity". Deutsche Welle. 2017-06-21.
- Sabino, António A. (2007), Fog Water Collection Projects in Cape Verde: Potentialities and Constraints. Case Study of the Natural Park of Serra Malagueta. 4th International Conference on Fog, Fog Collection and Dew
- "Can fog solve water shortages?". IRIN News. 2009-01-09.
- Madeira Laurel Forest, Madeira Wind Birds 2005
This article incorporates public domain material from the CIA World Factbook website https://www.cia.gov/library/publications/the-world-factbook/index.html.
- World Wildlife Fund, ed. (2001). "Cape Verde Islands dry forests". WildWorld Ecoregion Profile. National Geographic Society. Archived from the original on 2010-03-08.
- "Cape Verde Islands dry forests". Terrestrial Ecoregions. World Wildlife Fund.