Spatial variability of throughfall in a Chinese pine (Pinus tabulaeformis) plantation in northern China

Azevedo J, Morgan D L (1974). Fog precipitation in costal California forests. Ecology, 55: 1,135–1,141

Carlyle-Moses D E, Flores Laureano J S, Price A G (2004). Throughfall and throughfall spatial variability in Madrean oak forest communities of northeastern Mexico. J Hydrol, 297: 124–135

Crockford R H, Richardson D P (2000). Partitioning of rainfall into throughfall, stemflow and interception: effect of forest type, ground cover and climate. Hydrol Process, 14: 2,903–2,920

Dong S R, Guo J T, Man R Z (1987). Throughfall, stemflow and interception of Chinese Pine (Pinus tabulaeformis) plantation in Northern China. J Beijing For Univ, 9(1): 58–67 (in Chinese)

Gash J H C, Wright I R, Lloyd C R (1980). Comparative estimates of interception loss from three coniferous forests in Great Britain. J Hydrol, 48: 89–150

Gash J H C, Wright I R, Lloyd C R (1980). A predictive model of rainfall interception in forests. 1. Derivation of the model from observation in a plantation of Corscian pine. Agric For Meteorol, 9: 367–384

Iroumé A, Huber A (2002). Comparison of interception losses in a broadleaved native forest and a Pseudotsuga menziesii (Douglas fir) plantation in the Andes Mountains of southern Chile. Hydrol Process, 16: 2,347–2,361

Kimmins J P (1973). Some statistical aspects of sampling throughfall precipitation on nutrient cycling studies in British Columbian coastal forests. Ecology, 54: 1,008–1,019

Kong F Z, Song B, Pei T F (1990). Mathematical model of the relationship between interception and rainfall. Chin J Appl Ecol, 1(3): 201–207 (in Chinese)

LAI-2000 Plant Canopy Analyzer: Instruction Manual (1990). LI-COR, Lincoln, Nebraska, USA

Lloyd C R, Marquesf A O (1988). Spatial variability of throughfall and stemflow measurements in Amazonian rainforest. Agric For Meteorol, 42: 63–73

Loustau D, Berbigier P, Granier A, Hadj Moussa F E (1992). Interception loss, throughfall and stemflow in a maritime pine stand: I. Variability of throughfall and stemflow beneath the pine canopy. J Hydrol, 138: 449–467

Pei T F, Deng Y C (1996). The simulation and model of rainfall process distribution in forest canopy. I. The models of throughfall, stemflow and canopy interception under constant rainfall intensity. Sci Silv Sin, 32(1): 1–10 (in Chinese)

Pook E W, Moore P H R, Hall T (1991). Rainfall interception by trees of Pinus radiata and Eucalypt viminalis in a 1,300 mm rainfall area of southeastern new south Wales: I. gross losses and their variability. Hydrol Process, 5: 127–141

Rodrigo A, Avila A (2001). Influence of sampling size in the estimation of mean throughfall in two Mediterranean holm oak forests. J Hydrol, 243: 216–227

Teklehaimanot Z, Jarvis P G, Ledger D C (1991). Rainfall interception and boundary layer conductance in relation to tree spacing. J Hydrol, 123: 261–278

Valente F, David J S, Gash J H C (1997). Modeling interception loss for two sparse eucalypty and pine forests in central Portugal using reformulated Rutter and Gash analytical models. J Hydrol, 190: 141–162

Veneklaas E J, Van E K R (1990). Rainfall interception lose for two tropical mountain rain forests. Hydrol Process, 4: 311–326

Viville D (1993). Interception on a mountainous declining spruce stand in the Strengbach catchment (Voges, France). J Hydrol, 144: 892–898

Wen Y G, Liu S R (1995). Quantity analyses of the characteristic of rainfall interception of main forestry system in China. Sci Silv Sin, 31(4): 289–298

Zeng D H, Pei T F, Fan Z P, Jiang F Q, Zhu J J (1996). Simulation of canopy interception by Mongolian pine. Chin J Appl Ecol, 7(2): 134–138 (in Chinese)

Zhang Z Q (2002). Forestry Hydrology: Process and Mechanism. Beijing: China Environmental Science Press (in Chinese)