Tumbes is a city in northwestern Peru , on the banks of the Tumbes River . It is the capital of the Tumbes Region , as well as of Tumbes Province and Tumbes District . Located near the border with Ecuador , Tumbes has 111,595 inhabitants as of 2015. It is served by the Cap. FAP Pedro Canga Rodriguez Airport . It is located on the Gulf of Guayaquil along with Zorritos.
24-561: Tumbes , Tumbez , or Túmbez may refer to: Tumbes, Peru Tumbes River or Túmbez River of Ecuador and Peru in South America Tumbes Region in coastal Peru Tumbes Province , a political subdivision of Peru Tumbes Reserved Zone Tumbez, Virginia Caleta Tumbes , a town and fisherman cove in Chile See also [ edit ] Tumpis Indians,
48-399: A people of Ecuador and Peru Gulf of Guayaquil-Tumbes mangroves ecoregion of Peru and Ecuador Manglares de Tumbes National Sanctuary of Peru [REDACTED] Topics referred to by the same term This disambiguation page lists articles about distinct geographical locations with the same name. If an internal link led you here, you may wish to change the link to point directly to
72-492: A cultural group of natives called Tumpis . At its peak, its population is estimated to have reached 178,000. After 1400, Inca Pachacuti ruled over Tumbes and the territory became an important political stronghold during the Inca Empire . Later Inca emperor Huayna Capac expanded Tumbes by ordering the construction of roads, houses and palaces. Tumbes was first visited by Spanish conquistador Francisco Pizarro during
96-773: A few instances), dry summers, though summers are not typically as hot as hot desert climates. Unlike hot desert climates, cold desert climates tend to feature cold, dry winters. Snow tends to be rare in regions with this climate. The Gobi Desert in northern China and Mongolia is one example of a cold desert. Though hot in the summer, it shares the freezing winters of the rest of Inner Asia . Summers in South America's Atacama Desert are mild, with only slight temperature variations between seasons. Cold desert climates are typically found at higher altitudes than hot desert climates and are usually drier than hot desert climates. Cold desert climates are typically located in temperate zones in
120-421: A final conflict in 1995. Peruvian President Alberto Fujimori and Ecuadorian Presidente Jamil Mahuad signed a final document in which Ecuador accepted Perú's right over Tumbes and other territories claimed by Ecuador until then. Tumbes has a hot arid climate (Köppen BWh ), although it receives an average annual rainfall of 307.5 millimetres or 12.1 inches, due to its high potential evapotranspiration . Rainfall
144-566: Is determined. The precipitation threshold (in millimetres) involves first multiplying the average annual temperature in °C by 20, then adding 280 if 70% or more of the total precipitation is in the high-sun summer half of the year (April through September in the Northern Hemisphere , or October through March in the Southern), or 140 if 30–70% of the total precipitation is received during the applicable period, or 0 if less than 30% of
168-550: Is seen in sections of Africa and Arabia . During colder periods of the year, night-time temperatures can drop to freezing or below due to the exceptional radiation loss under the clear skies. However, temperatures rarely drop far below freezing under the hot subtype. Hot desert climates can be found in the deserts of North Africa such as the wide Sahara Desert , the Libyan Desert or the Nubian Desert ; deserts of
192-403: Is used as an isotherm so that a location with a BW type climate with the appropriate temperature above this isotherm is classified as "hot arid subtype" ( BW h ), and a location with the appropriate temperature below the isotherm is classified as "cold arid subtype" ( BW k ). Most desert/arid climates receive between 25 and 200 mm (1 and 8 in) of rainfall annually, although some of
216-627: Is very variable due to the El Niño Southern Oscillation , with strong El Niños frequently seeing more than twice the mean rain. Desert climate#Hot desert climates The desert climate or arid climate (in the Köppen climate classification BWh and BWk ) is a dry climate sub-type in which there is a severe excess of evaporation over precipitation . The typically bald, rocky, or sandy surfaces in desert climates are dry and hold little moisture, quickly evaporating
240-953: The Horn of Africa such as the Danakil Desert or the Grand Bara Desert ; deserts of Southern Africa such as the Namib Desert or the Kalahari Desert ; deserts of West Asia such as the Arabian Desert , or the Syrian Desert ; deserts of South Asia such as Dasht-e Lut and Dasht-e Kavir of Iran or the Thar Desert of India and Pakistan; deserts of the United States and Mexico such as
264-721: The Indian Subcontinent , southwestern Africa, interior Australia, the Southwestern United States , northern Mexico , sections of southeastern Spain , the coast of Peru , and Chile . This makes hot deserts present in every continent except Antarctica. At the time of high sun (summer), scorching, desiccating heat prevails. Hot-month average temperatures are normally between 29 and 35 °C (84 and 95 °F), and midday readings of 43–46 °C (109–115 °F) are common. The world's absolute heat records, over 50 °C (122 °F), are generally in
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#1732765217765288-804: The Mojave Desert , the Sonoran Desert or the Chihuahuan Desert ; deserts of Australia such as the Simpson Desert or the Great Victoria Desert and many other regions. In Europe , the hot desert climate can only be found on southeastern coast of Spain as well as small inland parts of southeastern, especially parts of the Tabernas Desert . Hot deserts are lands of extremes: most of them are among
312-534: The Sahara Desert such as Kufra , Libya , record an even drier 0.86 mm (0.034 in) of rainfall annually. The official weather station in Death Valley , United States reports 60 mm (2.4 in) annually, but in 40 months between 1931 and 1934 a total of just 16 mm (0.63 in) of rainfall was measured. To determine whether a location has an arid climate, the precipitation threshold
336-652: The 30s and 40s latitudes, usually in the leeward rain shadow of high mountains, restricting precipitation from the westerly winds. An example of this is the Patagonian Desert in Argentina, bounded by the Andes ranges to its west. In the case of Central Asia, mountains restrict precipitation from the eastern monsoon . The Kyzyl Kum , Taklamakan and Katpana Desert deserts of Central Asia are other significant examples of BWk climates. The Ladakh region and
360-520: The Republic of the Gran Colombia challenged that right and then Ecuador claiming de jure rights through unmodified colonial Royal Decrees ( Real Cédulas ), but to no avail. The Protocol of Rio de Janeiro signed in 1942 with Ecuador legally confirmed Peru's previously de facto rights over Tumbes after a victorious war. However, lasting peace between both countries was not achieved until 1998, after
384-504: The already little rainfall they receive. Covering 14.2% of Earth's land area, hot deserts are the second-most common type of climate on Earth after the Polar climate . There are two variations of a desert climate according to the Köppen climate classification : a hot desert climate ( BWh ), and a cold desert climate ( BWk ). To delineate "hot desert climates" from "cold desert climates", a mean annual temperature of 18 °C (64.4 °F)
408-994: The city of Leh in the Great Himalayas in India also have a cold desert climate. In North America, the cold desert climate occurs in the drier parts of the Great Basin Desert and the Bighorn Basin in Big Horn and Washakie County in Wyoming . The Hautes Plaines , located in the northeastern section of Morocco and in Algeria , is another prominent example of a cold desert climate. In Europe , this climate only occurs in some inland parts of southeastern Spain, such as in Lorca . Polar climate desert areas in
432-599: The first South American Indigenous interpreters who later aided Pizarro and his followers during the conquest of Peru, were born in Tumbes. During its colonial period, Tumbes was sparsely populated and formed a part of the Audiencia of Quito through an unmodified Cedula of 1563 and Cedula of 1740. When Tumbes declared its independence from Spain, it opted to join Peru believing in the right of free determination of peoples. First,
456-599: The hot deserts, where the heat potential can be the highest on the planet. This includes the record of 56.7 °C (134.1 °F) in Death Valley , which is currently considered the highest temperature recorded on Earth . Some deserts in the tropics consistently experience very high temperatures all year long, even during wintertime. These locations feature some of the highest annual average temperatures recorded on Earth, exceeding 30 °C (86 °F), up to nearly 35 °C (95 °F) in Dallol, Ethiopia . This last feature
480-444: The hottest, the driest, and the sunniest places on Earth because of nearly constant high pressure; the almost permanent removal of low-pressure systems, dynamic fronts, and atmospheric disturbances; sinking air motion; dry atmosphere near the surface and aloft; the exacerbated exposure to the sun where solar angles are always high makes this desert inhospitable to most species. Cold desert climates ( BWk ) usually feature hot (or warm in
504-414: The intended article. Retrieved from " https://en.wikipedia.org/w/index.php?title=Tumbes&oldid=1169250989 " Category : Place name disambiguation pages Hidden categories: Short description is different from Wikidata All article disambiguation pages All disambiguation pages Tumbes, Peru Tumbes has its origins back in pre-Inca times when it was inhabited by
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#1732765217765528-549: The most consistently hot areas of Central Australia , the Sahel and Guajira Peninsula can be, due to extreme potential evapotranspiration , classed as arid with the annual rainfall as high as 430 millimetres or 17 inches. Although no part of Earth is known for certain to be rainless, in the Atacama Desert of northern Chile, the average annual rainfall over 17 years was only 5 millimetres (0.20 in). Some locations in
552-670: The start of the Spanish conquest of the Inca Empire in 1528. Molina noted that Tumbes was a well organized town. Pizarro made a second expedition in 1532 during which he encountered resistance from the curaca (chieftain) Chilimaza in what became known as the Battle of the Manglares . Pizarro was eventually successful and is said to have planted a cross in the invaded territory as a sign of Hispanic victory. Felipillo and Yacané ,
576-650: The total precipitation is so received there. If the area's annual precipitation is less than half the threshold (50%), it is classified as a BW (desert climate), while 50–100% of the threshold results in a semi-arid climate. Hot desert climates ( BWh ) are typically found under the subtropical ridge in the lower middle latitudes or the subtropics , often between 20° and 33° north and south latitudes. In these locations, stable descending air and high pressure aloft clear clouds and create hot, arid conditions with intense sunshine. Hot desert climates are found across vast areas of North Africa , West Asia , northwestern parts of
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