Sertão
From Wikipedia, the free encyclopedia
In Brazil, the sertão (meaning "backland" in Portuguese) refers to the semi-arid region in Northeastern Brazil comprising parts of the states of Alagoas, Bahia, Pernambuco, Paraíba, Rio Grande do Norte, Ceará and Piauí. The plural of sertão is sertões. The term "sertanejo" is similar to the generic use of "cowboy" in the United States.
Geographically, the sertão consists mainly of low uplands that form part of the Brazilian Highlands. Most parts of the sertão are between 200 and 500 metres above sea level, with higher elevations found on the eastern edge in the Planalto da Borborema, where it merges into a subhumid region known as agreste, in the Serra da Ibiapaba in western Ceará and in the Serro do Periquito of central Pernambuco. In the north, the sertão extends to the northern coastal plains of Rio Grande Do Norte state, whilst in the south it fades out in the northern fringe of Minas Gerais.
Two major rivers cross the sertão, the Rio Jaguaribe and the Rio Piranhas further east. Apart from the Rio São Francisco which originates outside the region, other rivers dry out after the rainy periods end.
[edit] Climate and vegetation
Because the sertão lies close to the equator, temperatures remain nearly uniform throughout the year and are typically tropical, often extremely hot in the west.
However, the sertão is distinctive in its low rainfall compared to other areas of Brazil. Because of the relatively cool temperatures in the South Atlantic Ocean, the intertropical convergence zone remains north of the region for most of the year, so that most of the year is very dry.
Although annual rainfall averages between 500 and 800 millimetres over most of the sertão and 1300 millimetres on the northern coast at Fortaleza, it is confined to a short rainy season. This season extends from January to April in the west, but in the eastern sertão it generally occurs from March to June. However, rainfall is extremely erratic and in some years the rains are minimal, leading to catastrophic drought, whilst in others rains are extremely heavy and floods occur. This variability has caused extreme famines among subsistence farmers in the region, exacerbated by the extreme imbalance of land ownership throughout the sertão. The worst of these famines, between 1877 and 1879, was said to have killed over half the region's population.
In its natural state, the sertão was covered by a distinctive scrubby caatinga vegetation, consisting generally of low thorny bushes adapted to the extreme climate. Several species of tree in the caatinga have become valuable horticultural plants, such as the cashew nut. Most of the sertão vegetation is now substantially degraded as a result of centuries of cattle ranching or clearing for cotton farming.
Parts of the sertão are recognised as a biodiversity hotspot because of the unique florio.
[edit] See also
[edit] References
nonfiction
- Michael H. Glantz; Currents of Change : El Niño's Impact on Climate and Society; published 1996 by Cambridge University Press. ISBN 0521576598
- Michael H. Glantz (editor); Drought Follows The Plow: Cultivating Marginal Areas; published 1994 by Cambridge University Press. ISBN 0521442524
- Fagan, Brian; Floods, Famines, and Emperors : El Niño and the Fate of Civilizations; published 2000 by Basic Books. ISBN 0465011217
fiction
