## Abstract Alluvial forests are under high pressure from human activities because of their value as agricultural, wildlife, timber and recreational land. Despite this, spatial patterns of alluvial forest deforestation are not well known. We studied forest alterations in a 2800โha alluvial ecosyste
The stemflow of trees in a Bornean lowland tropical forest
โ Scribed by Odair J. Manfroi; Kuraji Koichiro; Tanaka Nobuaki; Suzuki Masakazu; Michiko Nakagawa; Tohru Nakashizuka; Lucy Chong
- Publisher
- John Wiley and Sons
- Year
- 2004
- Tongue
- English
- Weight
- 394 KB
- Volume
- 18
- Category
- Article
- ISSN
- 0885-6087
- DOI
- 10.1002/hyp.1474
No coin nor oath required. For personal study only.
โฆ Synopsis
Abstract
Stemflow volume generation in lowland tropical forests was measured over a 1โyear period in the Malaysian state of Sarawak. The stemflow volume generated by 66 freeโstanding trees with a diameter at breast height (DBH) over 1 cm and a tree height over 1 m were measured daily in a representative 10 m ร 10 m plot of the forest. Throughfall in the plot was also measured using 20 gauges in a fixed position. Of the 2292 mm of total rainfall observed during the yearโlong period, stemflow accounted for 3ยท5%, throughfall for 82% and there was an interception loss of 14ยท5%. Understory trees (DBH < 10 cm) played an important role in stemflow generation, producing 77% of the overall stemflow volume and 90% during storms with less than 20 mm of rainfall. Also, owing to their efficiency at funneling rainfall or throughfall water received by their crowns, some understory trees noticeably reduced the catches of the throughfall gauges situated under the reach of their crown areas. During storms producing greater than 20 mm of rainfall, 80% of the total stemflow occurred; trees with a large DBH or height and for which the ratio between crown's diameter and depth is less than 1, tended to generate more stemflow volume in these storms. Mean areal stemflow as a fraction of rainfall in this lowland tropical forest was 3ยท4%, but may range from 1โ10% depending upon the proportion of trees that are high or poor stemflow yielders. Trees with DBH greater than 10 cm were likely to contribute less than 1% of the 3ยท4% mean areal stemflow in the forest. Copyright ยฉ 2004 John Wiley & Sons, Ltd.
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