${session.getAttribute("locale")} 5 Transpiration and stomatal conductance in a young secondary tropical montane forest: contrasts between native trees and invasive understorey shrubs Wed 27 Nov 2019 14:09:54 AEST ]]> Effects of Reforestation of a Degraded Imperata Grassland on Dominant Flow Pathways and Streamflow Responses in Leyte, the Philippines Tue 25 Jun 2019 16:38:39 AEST ]]> Forest Landscape Restoration and Hydrological Recovery in the Humid Tropics: What can be expected realistically? Tue 14 May 2019 10:05:48 AEST ]]> Soil and Water Impacts of Reforesting Fire-Climax Grasslands on Leyte Island (Philippines): Key results obtained by ACIAR Project ASEM/2010/050 Tue 14 May 2019 10:05:47 AEST ]]> Typhoon-induced changes in rainfall interception loss from a tropical multi-species ‘reforest’ Thu 20 Jun 2019 16:08:13 AEST ]]> Separating effects of rainfall variability and typhoon disturbance on the runoff response of a tropical ‘reforest’ using a data-based mechanistic modeling approach Thu 02 Jan 2020 13:09:25 AEST ]]> Water budget and run‐off response of a tropical multispecies “reforest” and effects of typhoon disturbance Fri 18 Oct 2019 13:52:40 AEST ]]> Soil physical characteristics of a degraded tropical grassland and a ‘reforest’: Implications for runoff generation 50% of the rainfall might generate Hortonian overland flow in the grassland. Overland flow is unlikely in the reforest where lateral flow is likely to be generated around 60 cm depth for ~30% of rain-time, versus 2–3% between 20 and 60 cm. Within the limitations of the space-for-time substitution approach, these results suggest that 23 years of forest development at Manobo had a positive effect on hillslope hydrological functioning.]]> Fri 15 Feb 2019 10:48:16 AEST ]]> Runoff response and sediment yield of a landslide-affected fire-climax grassland micro-catchment (Leyte, The Philippines) before and after passage of typhoon Haiyan Fri 15 Feb 2019 10:39:50 AEST ]]>