A cloud forest, also called a fog forest, 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. 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.
Distribution and climate
Dependent on local climate, which is affected by the distance to the sea, the exposition and the latitude (from 23°N to 25°S), the altitude varies from 500 m to 4000 m above sea level. Typically, there is a relatively small band of altitude 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 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.
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.
Only 1% of the global woodland consists of cloud forests.
Important areas of cloud forest are in Central and South America, East and Central Africa, Indonesia, Malaysia, the Philippines, Papua-New Guinea, and in the Caribbean.
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.
Distribution of temperate cloud forests
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- Argentina - Salta, Jujuy, Catamarca and Tucumán (Southern Andean Yungas)
- Australia - Lamington National Park, Springbrook National Park, Mount Bartle Frere and Mount Bellenden Ker (Queensland) and Mount Gower (Lord Howe Island)
- Bolivia - Yungas region, La Paz Department, Chapare Province, Cochabamba Department
- Canada - Coastal British Columbia
- Chile - Bosque de Fray Jorge National Park
- Costa Rica - Monteverde Cloud Forest Reserve
- Ecuador - Tandayapa, Mindo.
- People's Republic of China - Yunnan Plateau, mountains of southern and eastern China
- Ethiopia - Kaffa in the Southern Nations, Nationalities, and People's Region
- India - Shola forests in Western Ghats, higher ranges of Namdapha National Park, forests of Northeast India
- Indonesia - Various places in Sulawesi (such as Nokilalaki and Rantemario Mountains), the Maluku Islands (Moluccas - particularly Buru, Seram and Waigeo Islands), and New Guinea (mostly Jayawijaya Mountains and Foja-Mamberamo valleys).
- Iran - Eastern part of Alborz mountains, north of Iran, Golestan Province
- Japan - parts of Yakushima Island
- Malaysia - Mount Kinabalu, Cameron Highlands, Genting Highlands and Fraser's Hill
- Mexico - El Cielo Biosphere in the state of Tamaulipas
- New Zealand - parts of Fiordland, Mount Taranaki and Mount Cargill, near Dunedin
- Pakistan - Shoghran Forest in the Kaghan Valley, and regions of Upper Swat in the north west of Pakistan
- Portugal - Azores and Madeira (laurisilva)
- South Africa
- Spain - Canary Islands (laurisilva)
- Taiwan - Yuanyang Lake Nature Reserve, Chatianshan Nature Reserve, and Fuxing District in Taoyuan City
- Thailand - Doi Inthanon, Doi Chiang Dao, Doi Phu Kha, Phu Khe and Khao Luang
- United States - North Coast
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.
Due to 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:
- 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.
Importance of cloud 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) 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 mountain gorilla (Gorilla b. beringei). Many of those endemic animals have important functions, such as seed dispersal and forest dynamics in these ecosystems.
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 amount 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 have a so-called coolhouse, whereas the newly opened (2012) Gardens by the Bay feature a very big 0.8 hectares (2.0 acres) coolhouse that is simply named "Cloud Forest". The latter features a 42-metre (138 ft)-high artificial mountain clad in epiphytes such as orchids, ferns, clubmosses, bromeliads and others. The cloud forest also features a display on the threat to cloud-forest ecology posed by global warming.
- Clarke, C.M. 1997. Nepenthes of Borneo. Natural History Publications (Borneo), Kota Kinabalu, p. 29.
- (Häger, 2006; Hamilton et al., 1995)
- (Häger 2006; Hamilton et al., 1995)
- (Hamilton et al., 1995)
- (García-Santos et al, 2009)
- (García-Santos, 2007)
- (Häger, 2006)
- "Resources Data - UNEP-WCMC". unep-wcmc.org.
- (Hamilton et al., 1995; Häger, 2006)
- (Bruijnzeel and Proctor quote from Hamilton et al., 1995)
- (Hamilton et al., 1995; Häger 2006)
- "Fog drip - AMS Glossary". American Meteorological Society. Retrieved 2014-12-15.
- (Hamilton et al., 1995; Van Steenis, 1972 and Grubb and Tanner, 1976)
- (Vogelmann, 1973 and Bruijnzeel, 1990 quote by Hamilton et al., 1995)
- (Bruijnzeel and Hamilton, 2000)
- (García-Sntos, 2007)
- (Kapelle, 2004 quote by Häger, 2006)
- Ponce-Reyes, Rocio; Nicholson, Emily; Baxter, Peter W. J.; Fuller, Richard A.; Possingham, Hugh (1 May 2013). "Extinction risk in cloud forest fragments under climate change and habitat loss". Diversity Distrib. 19 (5-6): 518–529. doi:10.1111/ddi.12064 – via Wiley Online Library.
- (Foster, 2001, Bubb et al. 2004)
- (Bubb et al., 2004)
- (Foster, 2001)
- Ponce-Reyes, Rocío; Reynoso-Rosales, Víctor-Hugo; Watson, James E. M.; VanDerWal, Jeremy; Fuller, Richard A.; Pressey, Robert L.; Possingham, Hugh P. (1 June 2012). "Vulnerability of cloud forest reserves in Mexico to climate change". Nature Clim. Change. 2 (6): 448–452. doi:10.1038/nclimate1453 – via www.nature.com.
- Bruijnzeel, L.A.; Hamilton, L.S. (2000). Decision Time For Cloud Forests: Water-Related Issues And Problems Of The Humid Tropics And Other Warm Humid Regions. Paris, France: UNESCO's IHP Humid Tropics Programme Series No.13.
- Foster, P., 2001, The potential negative impacts of global climate change on tropical montane cloud forests, Elsevier Science/ Earth-Science Review* Bubb, P., May, I., Miles, L., Sayer, J., 2004, Cloud Forest Agenda, UNEP-WCMC, Cambridge, UK, http://www.unep.wcmc.org/resouces/publicashions/UNEP_WCMC_bio_series/20.htm
- García-Santos, G., Marzol, M. V., and Aschan, G. (2004) Water dynamics in a laurel montane cloud forest in the Garajonay National Park (Canary Islands, Spain), Hydrol. Earth Syst. Sci., 8, 1065-1075. http://www.hydrol-earth-syst-sci.net/8/1065/2004/hess-8-1065-2004.html
- Häger, A., 2006, Einfluss von Klima und Topographie auf Struktur, Zusammensetzung und Dynamik eines tropischen Wolkenwaldes in Monteverde, Costa Rica, Göttingen: Disssertation Georg August Universität Göttingen
- García-Santos, G. (2007). An eco-hydrological and soils study in a montane cloud forest in the National Park of Garajonay, La Gomera (Canary Islands, Spain). PhD Dissertation, Amsterdam: VU University. http://dare.ubvu.vu.nl/handle/1871/12697
- García-Santos, G., Bruijnzeel, L.A. and Dolman, A.J. (2009). Modelling canopy conductance under wet and dry conditions in a subtropical cloud forest. Agricultural and Forest Meteorology, 149 (10), 1565-1572 doi:10.1016/j.agrformet.2009.03.008
|Wikimedia Commons has media related to Cloud forests.|
- Chelemhá cloud forest reserve in Alta Verapaz, Guatemala
- Cloud Forest Fable and Video
- Laurisilva Montane Cloud Forest in the National Park of Garajonay, Canary Islands
- Monteverde Costa Rica Cloud Forest
- Tropical Montane Cloud Forest Initiative
- Monteverde Cloud Forest Ecology
- Roach, John (August 13, 2001). "Cloud Forests Fading in the Mist, Their Treasures Little Known". National Geographic News
- An Ecological Reserve in the Cloud Forest of Mindo Ecuador
- Tropical hydrology and cloud forests project
- Hydrology of tropical cloud forests project
- Cloud Forest Video - Rara Avis CR
- Tropical Montane Cloud Forests – Science for Conservation and Management (L.A. Bruijnzeel, F.N. Scatena and L.S. Hamilton, 2011)
- Andes Biodiversity and Ecosystem Research Group