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Tropical Montant Cloud Forest Initiative Workshop Report
 



 

Tropical Montane Cloud Forest Initiative
"Empowering communities, conservationists and researchers to ensure cloud forest conservation"

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UNESCO International Hydrological Programme


DEFINITION

Hamilton et al. (1993) acknowledge that "clear definition of tropical montane cloud forest is fraught with difficulty". Despite having a number of key recognisable features, these vary greatly from one area to another, and this, combined with an enormous range in the terminology used to identify TMCFs leads to considerable confusion. At a Tropical Montane Cloud Forests Inter- national State-of-knowledge Symposium and Workshop held in Puerto Rico in June 1993, a synthesis working definition was developed which has been used as a guide for the purposes of the current project (Box 1).

Box 1.

Synthesis Working Definition

Hamilton, Juvik, and Scatena (from Hamilton et al, (1993)); "The tropical montane cloud forest is composed of forest ecosystems of distinctive floristic and structured form. It typically occurs as a relatively narrow altitudinal zone where the atmospheric environment is characterised by persistent, frequent or seasonal cloud cover at the vegetation level. Enveloping cloud or wind-driven clouds influence the atmospheric interaction through reduced solar radiation and vapour deficit, canopy wetting, and general suppression of evapotranspiration. The net precipitation (throughfall) is significantly enhanced (beyond rainfall contribution) through direct canopy interception of cloud water (horizontal precipitation or cloud stripping) and low water use by the vegetation.

In comparison with lower latitude tropical moist forest, the stand characteristics generally include reduced tree stature and increased stem density. Canopy trees usually exhibit gnarled trunks and branches; dense compact crowns; and small, thick and hard (sclerophyll) leaves. TMCF is also characterised by having a high proportion of biomass as epiphytes (bryophytes, lichens and filmy ferns) and a corresponding reduction in woody climbers. Soils are wet and frequently waterlogged and highly organic in the form of humus and peat (histosol). Biodiversity in terms of tree species of herbs, shrubs and epiphytes can be relatively high (considering the small areal extent) when compared with tree species-rich lowland rain forest. Endemism is often very high.

TMCF occurs on a global scale within a wide range of annual and seasonal rainfall regimes i.e. 500-10,000mm.year). There is also significant variation in the altitudinal position of this mountain vegetation belt. For large, inland mountain systems, TMCF may typically be found between 2000-3500m (Andes, Rwenzoris), whereas in coastal and insular mountains this zone may descend to 100m (Hawai'i). Under exceptionally humid marine, equatorial conditions, a TMCF zone may develop on steep, small island mountains at elevaitons as low as 500m or even lower (Kosrae in Micronesia and Gau in Fiji)."

 

Philip Bubb
Tropical Montane Cloud Forest Initiative
UNEP World Conservation Monitoring Centre
219 Huntingdon Road
Cambridge
CB3 0DL United Kingdom

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