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Ngangao Forest

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The Afromontane regions are subregions of the Afrotropical realm , one of the Earth's eight biogeographic realms , covering the plant and animal species found in the mountains of Africa and the southern Arabian Peninsula . The Afromontane regions of Africa are discontinuous, separated from each other by lower-lying areas, and are sometimes referred to as the Afromontane archipelago , as their distribution is analogous to a series of sky islands .

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29-472: Ngangao Forest is one of the few remaining indigenous cloud forest fragments of the Taita Hills , Kenya . It is located on a rock surrounded by the villages of Makandenyi, Maghimbinyi, Mgambonyi and Kitumbi. It lies 10 km from Wundanyi and can easily be reached by road. There is even frequent public transport from Wundanyi to Makandenyi (at least 10 vehicles daily). The very basic "Ngangao forest camp"

58-673: A 35-metre (115 ft)-high artificial mountain clad in epiphytes such as orchids , ferns, clubmosses , bromeliads and others. Due to a relatively mild climate and summer fog, the San Francisco Botanical Garden has three outdoor cloud forest collections, including a 2-acre Mesoamerican Cloud Forest established in 1985. The Buffalo and Erie County Botanical Gardens contains a " Panama Cloud Forest" garden in House 11. Afromontane Afromontane communities occur above 1,500–2,000 metres (4,900–6,600 ft) elevation near

87-475: A large proportion of loss in TCF cover is still occurring despite formal protection. Although far from being universally accepted as true cloud forests, several forests in temperate regions have strong similarities with tropical cloud forests. The term is further confused by occasional reference to cloud forests in tropical countries as "temperate" due to the cooler climate associated with these misty forests. In 1970,

116-518: Is a generally tropical or subtropical , evergreen, montane , moist forest characterized by a persistent, frequent or seasonal low-level cloud cover, usually at the canopy level, formally described in the International Cloud Atlas (2017) as silvagenitus . Cloud forests often exhibit an abundance of mosses covering the ground and vegetation, in which case they are also referred to as mossy forests . Mossy forests usually develop on

145-496: Is a near-endemic. The tree genera Afrocrania , Balthasaria , Curtisia , Ficalhoa , Hagenia , Kiggelaria , Kuloa , Leucosidea , Platypterocarpus , Trichocladus , Widdringtonia , and Xymalos are Afromontane endemics or near-endemics, as are the plant genera Ardisiandra , Cincinnobotrys , and Stapfiella . Afromontane areas have a wide range of plant communities, including intermediate types. These include: In South Africa , Afromontane forests cover only 0.5% of

174-425: Is dependent on local climate (which is affected by the distance to the sea), the exposition and the latitude (typically from 25°N to 25°S), and the elevation (which varies from 500 m to 4000 m above sea level). Typically, there is a relatively small band of elevation in which the atmospheric environment is suitable for cloud forest development. This is characterized by persistent fog at the vegetation level, resulting in

203-587: Is located next to the forester's house at the edge of forest. With its 120 hectares (297 acres), Ngangao is the second largest forest and one of the lesser disturbed forests of the Taita Hills. As a result, it is a stronghold for many plant and animal species. There are three endemic birds species of the Taita Hills. The Taita thrush ( Turdus (olivaceus) helleri ), Taita apalis ( Apalis (thoracica) fuscigularis ) and Taita white-eye ( Zosterops (poliogaster) silvanus ) occur in relative large numbers. Some plants, like

232-427: Is the tree crowns that intercept the wind-driven cloud moisture, part of which drips to the ground. This fog drip occurs when water droplets from the fog adhere to the needles or leaves of trees or other objects, coalesce into larger drops and then drop to the ground. It can be an important contribution to the hydrologic cycle . Cloud forests are often peatlands , showcasing many classic peatland attributes. Due to

261-456: The Zimmermannia ovata , are only found in the dryer parts of Ngangao Forest. 03°22′S 038°20′E  /  3.367°S 38.333°E  / -3.367; 38.333 This Coast Province location article is a stub . You can help Misplaced Pages by expanding it . Cloud forest A cloud forest , also called a water forest , primas forest , or tropical montane cloud forest ,

290-710: The Philippines , Hawaii , Papua New Guinea , and in the Caribbean . The 1997 version of the World Conservation Monitoring Centre's database of cloud forests found a total of 605 tropical montane cloud forest sites in 41 countries. 280 sites, or 46% of the total, were located in Latin America , known in biogeography as the Neotropical realm . Twelve countries had tropical montane cloud forest sites, with

319-585: The saddles of mountains, where moisture introduced by settling clouds is more effectively retained. Cloud forests are among the most biodiversity-rich ecosystems in the world, with a large number of species directly or indirectly depending on them. Other moss forests include black spruce / feathermoss climax forest , with a moderately dense canopy and a forest floor of feathermosses , including Hylocomium splendens , Pleurozium schreberi , and Ptilium crista-castrensis . These weft-form mosses grow in boreal moss forests. The presence of cloud forests

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348-570: The 1970s. A total of around 736 cloud forest sites have been identified in 59 countries by the World Conservation Monitoring Centre , with 327 of them legally protected areas as of 2002. Important areas of cloud forest are in Central and South America (mainly Costa Rica , Venezuela , Honduras , Mexico , Ecuador , and Colombia ), East and Central Africa , India , Sri Lanka , Thailand , Vietnam , Indonesia , Malaysia ,

377-621: The Bolivian yungas , and the laurisilva of the Atlantic Islands), and occasionally subtropical and even temperate forests in which similar meteorological conditions occur are considered to be cloud forests. In comparison with lower-altitude tropical moist forests, cloud forests show a reduced tree stature combined with increased stem density and generally, a lower diversity of woody plants. Trees in these regions are generally shorter and more heavily stemmed than in lower-altitude forests in

406-676: The Congo , and Tanzania , and the Eastern Arc highlands of Kenya and Tanzania. Other Afromontane regions include the Drakensberg range of southern Africa, the Cameroon Highlands , and the Cameroon Line volcanoes, including Mount Cameroon , Bioko , and São Tomé . Although some Afromontane enclaves are widely separated, they share a similar mix of plant species which are often distinct from

435-681: The United States, the Atlanta Botanical Garden has a large tropical cloud forest greenhouse with a large collection of cloud forest epiphytes from around the world. It implements a refrigeration system to decrease the temperature at night. For many years, the Singapore Botanic Gardens had a so-called coolhouse. The Gardens by the Bay features a 0.8 hectares (2.0 acres) coolhouse that is simply named " Cloud Forest ". The latter features

464-559: The country's land area. The Afromontane forests occur along the mountainous arc of the Drakensberg Range, from Limpopo Province in the northeast to the Western Cape Province in the southwest. The Afromontane forests generally occur in well-watered areas, including ravines and south-facing slopes. The Afromontane forests are intolerant of fire, and the frequent fires of the surrounding fynbos , savanna , and grassland limit

493-743: The equator, and as low as 300 metres (980 ft) elevation in the Knysna-Amatole montane forests of South Africa . Afromontane forests are generally cooler and more humid than the surrounding lowlands. The Afromontane archipelago mostly follows the East African Rift from the Red Sea to Zimbabwe , with the largest areas in the Ethiopian Highlands , the Albertine Rift Mountains of Uganda , Rwanda , Burundi , Democratic Republic of

522-451: The extent of environmentally suitable areas for cloud forest in Mexico will sharply decline in the next 70 years. A number of climate models suggest low-altitude cloudiness will be reduced, which means the optimum climate for many cloud forest habitats will increase in altitude. Linked to the reduction of cloud moisture immersion and increasing temperature, the hydrological cycle will change, so

551-406: The global land surface in 2001 and harboured ~3,700 species of birds, mammal, amphibians and tree ferns (~15% of the global diversity of those groups), with half of those species entirely restricted to cloud forests. Worldwide, ~2.4% of cloud forests (in some regions, more than 8%) were lost between 2001 and 2018, especially in readily accessible places. While protected areas have slowed this decline,

580-443: The high water content of the soil, the reduced solar radiation and the low rates of decomposition and mineralization , the soil acidity is very high, with more humus and peat often forming the upper soil layer. Stadtmüller (1987) distinguishes two general types of tropical montane cloud forests: Only 1% of the global woodland consists of cloud forests. They previously comprised an estimated 11% of all tropical forests in

609-529: The initial cloud forest cover remains. Significant areas have been converted to plantations , or for use in agriculture and pasture . Significant crops in montane forest zones include tea and coffee , and the logging of unique species causes changes to the forest structure. In 2004, an estimated one-third of all cloud forests on the planet were protected at that time. Because of their delicate dependency on local climates, cloud forests will be strongly affected by global climate change . Results show that

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638-737: The majority in Venezuela (64 sites), Mexico (64), Ecuador (35) and Colombia (28). Southeast Asia and Australasia had 228 sites in 14 countries – 66 in Indonesia, 54 in Malaysia, 33 in Sri Lanka, 32 in the Philippines, and 28 in Papua New Guinea. 97 sites were recorded in 21 African countries, mostly scattered on isolated mountains. Of the 605 sites, 264 were in protected areas. Cloud forests occupied 0.4% of

667-402: The most widely used term, in some regions, these ecosystems or special types of cloud forests are called mossy forest, elfin forest , montane thicket, and dwarf cloud forest. The definition of cloud forest can be ambiguous, with many countries not using the term (preferring such terms as Afromontane forest and upper montane rain forest, montane laurel forest , or more localised terms such as

696-487: The original extent of cloud forests on the Earth was around 50 million hectares . Population growth , poverty and uncontrolled land use have contributed to the loss of cloud forests. The 1990 Global Forest Survey found that 1.1% of tropical mountain and highland forests were lost each year, which was higher than in any other tropical forests. In Colombia, one of the countries with the largest area of cloud forests, only 10–20% of

725-399: The reduction of direct sunlight and thus of evapotranspiration . Within cloud forests, much of the moisture available to plants arrives in the form of fog drip , where fog condenses on tree leaves and then drips onto the ground below. Annual rainfall can range from 500 to 10,000 mm/year and mean temperature between 8 and 20 °C (46.4 and 68 °F). While cloud forest today is

754-605: The results of climate change will be a loss in biodiversity, altitude shifts in species ranges and community reshuffling, and, in some areas, complete loss of cloud forests. Cloud-forest conditions are hard and expensive to replicate in a glasshouse because it is necessary to maintain very high humidity. Day temperatures have to be between 70-75F while night temperatures have to be maintained between 55-60F. In most cases, sophisticated refrigeration equipment has to be used to provide night temperatures below 60F. Such displays are usually quite small, but there are some notable exceptions. In

783-453: The same regions, often with gnarled trunks and branches, forming dense, compact crowns. Their leaves become smaller, thicker and harder with increasing altitude. The high moisture promotes the development of a high biomass and biodiversity of epiphyte , particularly bryophytes , lichens , ferns (including filmy ferns ), bromeliads and orchids . The number of endemic plants can be very high. An important feature of cloud forests

812-522: The surrounding lowland regions. Podocarps , of genera Podocarpus and Afrocarpus , are a characteristic tree, along with Prunus africana , Hagenia abyssinica , Juniperus procera , and Olea spp. . In the higher mountains, the Afromontane forest or woodland zone transitions to a higher Afroalpine zone of grasslands, shrublands, or moorlands. The plant families Curtisiaceae and Oliniaceae are Afromontane endemics and family Barbeyaceae

841-462: The system will dry out. This would lead to the wilting and the death of epiphytes, which rely on high humidity. Frogs and lizards are expected to suffer from increased drought. Calculations suggest the loss of cloud forest in Mexico would lead to extinction of up to 37 vertebrates specific to that region. In addition, climate changes can result in a higher number of hurricanes , which may increase damage to tropical montane cloud forests. All in all,

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