Titlebook: Water and the Rainforest in Malaysian Borneo; Hydrological Researc Ian Douglas Book 2022 Springer Nature Switzerland AG 2022 Equatorial Rai

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Overland Flow,w as 1.0–3.0% of throughfall, suggesting that most of the flow in headwater streams is generated by emerging sub-surface flow. Rainfall simulator experiments with high rainfall intensities around 200 mm h. found around 20% of throughfall becoming overland flow: perhaps an indication of what might ha

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,Rainfall and Its Interception by the Forest,tween 1400 and 1600 hours. Spatially rainfalls vary over distances of only a few kilometres, being strongly moderated by the combined effects of monsoonal wind direction and topography. The wettest year in 1986–2019, was 2011 with 3872 mm and the driest was 1997 with 1920 mm, a difference of almost

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Overland Flow,w as 1.0–3.0% of throughfall, suggesting that most of the flow in headwater streams is generated by emerging sub-surface flow. Rainfall simulator experiments with high rainfall intensities around 200 mm h. found around 20% of throughfall becoming overland flow: perhaps an indication of what might ha

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Infiltration, Soil Water and Pipeflow,ollapse hollows connected to a pipe system sometimes develops. In a wet month, a single monitored pipe supplied 67.5% of streamflow accounting for 41% of the rainfall over a 200 m long micro-catchment. Statistically, 72.3% of the variance in pipe stormflow response could be explained as a function o

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Sediment Supply and Movement on Slopes,major heavy rainfall occurs. Ants are the dominant movers of material on the forest floor, responsible for over 60% of scavenging by invertebrates. Tree uprooting creates a “pit and mound” topography of exposed soil on steeper slopes at Danum. This natural mechanism of displacing weathered bedrock i

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