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The experimental site was located in Madrid (40° 27' 23.82" N, 3° 45' 6.91" W, 597 m of altitude) under average environmental conditions similar to those of the seed source stand (rainfall: 452 mm, summer precipitation: 58 mm, temperature: 14.4°C, mean temperature of the coldest month: 5.3°C, mean temperature of the warmest month: 24.8°C).
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But, (I_{text{a}} = 0.2 times S) Q = frac{{(P - 0.2S ^{2} }}{P + 0.8S},{text{whenn }}P > 0. 2 {text{S}},{text{ otherwise }}Q (2) S = frac{25,400}{text{CN}} - 254, (3) where Q represents the run-off (mm), P stands for rainfall (mm), S stands for potential maximum retention (mm) and I a denotes the initial abstractions (due to infiltration, evaporation, interception).
Although House (1992) stated that the presence or absence of understorey is a factor of the density of the stand and of the rainfall regime, Zerga (2015) reported a similar finding in Ethiopia and indicated that the dominant leaf litterfall under Eucalyptus stands prohibits the growth of other plants due to its allelopathic effect.
The June rainfall total stands at 10.1 inches, only 0.17 inches shy of the June record for New York.
Although surface seeding with packing produced satisfactory plant stands, reliance on timely rainfall is required for this to be successful.
This is especially critical for stand establishment in years with low rainfall after planting.
Very few landslides occurred in the 0 100% of 100-year rainfall category, regardless of stand age or slope gradient class.
Key findings are that landslide detection probability decreased with increasing stand age, but was similar across rainfall intensities.
and a 2.9-year-old Pinus tecunumanii Eguiluz & J.P.Perry stand, both located in the summer rainfall region of South Africa.
An important finding was made by the Two Streams study, namely that the evaporation from the A. mearnsii stand (largely dryland) exceeded the annual rainfall by a substantial margin (Table 1) (Clulow et al. 2011).
We estimated the probability of detecting landslides on aerial photos for six strata defined by forest stand age and a broad range of rainfall intensity, expressed as percent of the 100-year, 24-h, maximum rainfall.
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