A cloud forest, also called a water forest, primas forest, or tropical montane cloud forest (TMCF), 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 the saddles of mountains, where moisture introduced by settling clouds is more effectively retained.
The presence of cloud forests is dependent on local climate (which is affected by the distance to the sea), the exposition and the latitude (from 23°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 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 fogcondenses 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.
While cloud forest today is 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 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 tropical moist forests, cloud forests show a reduced tree stature combined with increased stem density and generally the lower diversity of woody plants. Trees in these regions are generally shorter and more heavily stemmed than in lower-altitude forests in 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 is the tree crowns can 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.
Stadtmüller (1987) distinguishes two general types of tropical montane cloud forests:
Areas with a high annual precipitation due to a frequent cloud cover in combination with heavy and sometimes persistent orographic rainfall; such forests have a perceptible canopy strata, a high number of epiphytes, and a thick peat layer which has a high storage capacity for water and controls the runoff;
In drier areas with mainly seasonal rainfall, cloud stripping can amount to a large proportion of the moisture available to plants.
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 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.
Temperate cloud forests
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.
Watershed function: Because of the cloud-stripping strategy, the effective rainfall can be doubled in dry seasons and increase the wet season rainfall by about 10%. Experiments of Costin and Wimbush (1961)[non-primary source needed] showed that the tree canopies of non-cloud forests intercept and evaporate 20 percent more of the precipitation than cloud forests, which means a loss to the land component of the hydrological cycle.
Vegetation: Tropical montane cloud forests are not as species-rich as tropical lowland forests, but they provide the habitats for many species found nowhere else. For example, the Cerro de la Neblina, a cloud-covered mountain in the south of Venezuela, accommodates many shrubs, orchids, and insectivorous plants which are restricted to this mountain only.
Fauna: The endemism in animals is also very high. In Peru, more than one-third of the 270 endemic birds, mammals, and frogs are found in cloud forests. One of the best-known cloud forest mammals is the Spectacled Bear (Tremarctos ornatus).Many of those endemic animals have important functions, such as seed dispersal and forest dynamics in these ecosystems.
Seaborne moisture is vital to the cloud forest of Fray Jorge that is surrounded by the arid southern reaches of the Atacama Desert.
In 1970, 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 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.
Impact of climate change
Because of their delicate dependency on local climates, cloud forests will be strongly affected by global climate change. Results show that 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 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, 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.
In botanical gardens
Cloud-forest conditions are hard and expensive to replicate in a glasshouse because it is necessary to maintain a very high humidity. This is usually expensive as a high temperature must usually be maintained as well, and a high temperature combined with high humidity calls for good air circulation or else fungi and algae will develop. Such displays usually are quite small, but there are some notable exceptions. 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 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.
^Mark Aldrich, Clare Billington, Mary Edwards and Ruth Laidlaw (1997) "Tropical Montane Cloud Forests: An Urgent Priority for Conservation" WCMC Biodiversity Bulletin No. 2, World Conservation Monitoring Centre.
^Köhler, Lars; Tobón, Conrado; Frumau, K. F. Arnoud; Bruijnzeel, L. A. (Sampurno) (2007-12-01). "Biomass and water storage dynamics of epiphytes in old-growth and secondary montane cloud forest stands in Costa Rica". Plant Ecology. 193 (2): 171-184. doi:10.1007/s11258-006-9256-7. ISSN1573-5052. S2CID1032485.
Bruijnzeel, L. A; Proctor, J (1995). "Hydrology and Biogeochemistry of Tropical Montane Cloud Forests: What Do We Really Know?". In Hamilton, Lawrence S.; Juvik, James O.; Scatena, F. N. (eds.). Tropical Montane Cloud Forests. Ecological Studies. 110. pp. 38-78. doi:10.1007/978-1-4612-2500-3_3. ISBN978-1-4612-7564-0.
Grubb, PJ; Tanner, EVJ (July 1976). "The montane forests and soils of Jamaica: a reassessment". Journal of the Arnold Arboretum. 57 (3): 313-68. JSTOR43794514.
Häger, Achim (2006). Einfluss von Klima und Topographie auf Struktur, Zusammensetzung und Dynamik eines tropischen Wolkenwaldes in Monteverde, Costa Rica [Influence of climate and topography on the structure, composition and dynamics of a tropical cloud forest in Monteverde, Costa Rica] (Disssertation) (in German). hdl:11858/00-1735-0000-0006-B0EE-1.
Hamilton, Lawrence S; Juvik, James O; Scatena, F. N (1995). "The Puerto Rico Tropical Cloud Forest Symposium: Introduction and Workshop Synthesis". In Hamilton, Lawrence S.; Juvik, James O.; Scatena, F. N. (eds.). Tropical Montane Cloud Forests. Ecological Studies. 110. pp. 1-18. doi:10.1007/978-1-4612-2500-3_1. ISBN978-1-4612-7564-0.