Rainfall interception in a lower montane forest in Ecuador: effects of canopy properties

被引:133
作者
Fleischbein, K
Wilcke, W
Goller, R
Boy, J
Valarezo, C
Zech, W
Knoblich, K
机构
[1] Tech Univ Berlin, Inst Okol, Fachgebiet Bodenkunde, D-10587 Berlin, Germany
[2] Univ Giessen, Inst Angew Geowissensch, D-35390 Giessen, Germany
[3] Univ Bayreuth, Lehrstuhl Bodenkunde & Bodengeog, D-95440 Bayreuth, Germany
[4] Univ Nacl Loja, Area Agropecuaria & Recursos Nat Renovables, Programa Agroforesteria, Loja, Ecuador
关键词
epiphytes; leaf area index; lower montane forest; rainfall interception; storage capacity;
D O I
10.1002/hyp.5562
中图分类号
TV21 [水资源调查与水利规划];
学科分类号
081501 ;
摘要
Rainfall interception in forests is influenced by properties of the canopy that tend to vary over small distances. Our objectives were: (i) to determine the variables needed to model the interception loss of the canopy of a lower montane forest in south Ecuador, i.e. the storage capacity of the leaves S and of the trunks and branches S(t), and the fractions of direct throughfall p and stemflow p(t); (ii) to assess the influence of canopy density and epiphyte coverage of trees on the interception of rainfall and subsequent evaporation losses. The study site was located on the eastern slope of the eastern cordillera in the south Ecuadorian Andes at 1900-2000 m above sea level. We monitored incident rainfall, throughfall, and stemflow between April 1998 and April 2001. In 2001, the leaf area index (LAI), inferred from light transmission, and epiphyte coverage was determined. The mean annual incident rainfall at three gauging stations ranged between 2319 and 2561 mm. The mean annual interception loss at five study transects in the forest varied between 591 and 1321 mm, i.e. between 25 and 52% of the incident rainfall. Mean S was estimated at 1(.)91 mm for relatively dry weeks with a regression model and at 2(.)46 mm for all weeks with the analytical Gash model; the respective estimates of mean S(t) were 0(.)04 mm and 0(.)09 mm, of mean p were 0(.)42 and 0(.)63, and of mean pt were 0(.)003 and 0(.)012. The LAI ranged from 5(.)19 to 9(.)32. Epiphytes, mostly bryophytes, covered up to 80% of the trunk and branch surfaces. The fraction of direct throughfall p and the LAI correlated significantly with interception loss (Pearson's correlation coefficient r = -0(.)77 and 0(.)35 respectively, n = 40). Bryophyte and lichen coverage tended to decrease S, and vascular epiphytes tended to increase it, although there was no significant correlation between epiphyte coverage and interception loss. Our results demonstrate that canopy density influences interception loss but only explains part of the total variation in interception loss. Copyright (c) 2004 John Wiley & Sons, Ltd.
引用
收藏
页码:1355 / 1371
页数:17
相关论文
共 57 条
[1]   Rainfall interception loss in unlogged and logged forest areas of Central Kalimantan, Indonesia [J].
Asdak, C ;
Jarvis, PG ;
van Gardingen, P ;
Fraser, A .
JOURNAL OF HYDROLOGY, 1998, 206 (3-4) :237-244
[2]  
Balslev H., 2002, BOT AUSTROECUATORIAN, P51
[3]  
Bendix J., 1992, Erdkunde, V46, P118
[4]   Ground-based measurements of leaf area index:: a review of methods, instruments and current controversies [J].
Bréda, NJJ .
JOURNAL OF EXPERIMENTAL BOTANY, 2003, 54 (392) :2403-2417
[5]  
Bruijnzeel L.A., 2001, THE FORESTS HDB, P301, DOI DOI 10.1002/9780470757062.CH12
[6]  
Bruijnzeel L.A., 2000, IHP Humid Tropics Programme Series 03
[7]  
BRUIJNZEEL LA, 1995, ECOL STU AN, V110, P38
[8]  
BUHL A, 2000, SPSS, P734
[9]   Spatial heterogeneity of element and litter turnover in a Bornean rain forest [J].
Burghouts, TBA ;
Van Straalen, NM ;
Bruijnzeel, LA .
JOURNAL OF TROPICAL ECOLOGY, 1998, 14 :477-505
[10]   Water balance and nutrient inputs in bulk precipitation in tropical montane cloud forest in Panama [J].
Cavelier, J ;
Jaramillo, M ;
Solis, D ;
deLeon, D .
JOURNAL OF HYDROLOGY, 1997, 193 (1-4) :83-96