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)."