During the TREND (Tropical Environmental Data) experiment conducted in Thailand, wind observations were made at several levels below and above a tropical forest canopy. These data allowed us to compute the widely used canopy coupling index and to study its dependence on ambient conditions. Our resul
On the canopy flow index of a tropical forest
โ Scribed by R. T. Pinker; J. F. Moses
- Publisher
- Springer
- Year
- 1982
- Tongue
- English
- Weight
- 513 KB
- Volume
- 22
- Category
- Article
- ISSN
- 0006-8314
No coin nor oath required. For personal study only.
โฆ Synopsis
The usefulness ofthe canopy flow index concept is demonstrated for a two-story evergreen tropical forest. A sample of about 2500 wind profiles was utilized. It encompasses a large range of ambient wind conditions and spans the whole monsoon cycle in Southeast Asia.
It was found that the use of two canopy flow indices (one for the upper and one for the lower canopy) would be necessary to simulate the average canopy flow. For the upper canopy, an average value of 4.04 was obtained; for the lower canopy an index of 1.77 was computed. The indices seem to be independent of the ambient wind speed (if 2 m s-l IS exceeded), yet strongly dependent on wind direction.
๐ SIMILAR VOLUMES
Extensive measurements of stomatal resistance using a porometer in a maple-beech hardwood forest over two growing seasons and at two different canopy levels are described. The analysis permits a generalization that yields a final equation relating overall canopy resistance to solar irradiance and so
A microclimatic characterization of a dry tropical evergreen forest and a nearby clearing is presented. It is based on meteorological data for selected time intervals of approximately two weeks each, which span different stages of the monsoon cycle. It was found that the intensity of interaction be
## Abstract The diurnal variation of the average albedo, during 1970, over a tropical dry evergreen forest and a nearby clearing was investigated. The study is based on a most comprehensive set of solar radiation data in Southeast Asia. A strong dependence of the albedo on the zenith angle is evide
To evaluate an interactive eect of snow on energy exchange between the forest and atmosphere, the energy balance above a forest was measured continuously between February and April of 1997 in the Hitsujigaoka Experimental Forest, Sapporo, northern Japan. The forest was a dense, 23-year-old, conifero