H13Q-06
Typhoon Haiyan’s Effects on Interception Loss from a Secondary Tropical Forest near Tacloban, Leyte, the Philippines

Monday, 14 December 2015: 14:55
3022 (Moscone West)
Jun Zhang, VU University Amsterdam, Earth and Life Sciences, Amsterdam, Netherlands, Ilja H.J. van Meerveld, University of Zurich, Department of Geography, Zurich, Switzerland, Maarten J. Waterloo, Acacia Water, Gouda, Netherlands and L. Adrian Bruijnzeel Sr., King's College London, London, United Kingdom
Abstract:
Typhoon Haiyan made landfall in the central Philippines on November 8, 2013 as one of the strongest tropical cyclones ever recorded with maximum windspeeds of 314 km h-1. It affected humans, infrastructure and forests, including the 22-year-old community-managed secondary forest at Manobo near Tacloban on Leyte island. As part of a larger investigation of the impacts of secondary forests on streamflow, gross rainfall (P), throughfall (TF) and stemflow (SF) were monitored between June 2013 and June 2014 using 2 tipping bucket rainfall gauges, 2 large (200 cm by 30 cm) throughfall gutters connected to tipping buckets, 24 roving throughfall gauges (491 cm2 each) and 12 stemflow collectors. Leaf Area Index (LAI) above each of the throughfall collectors was measured regularly using a Canopy Analyzer. Average throughfall, stemflow, and interception loss (I) were determined for three different periods:(i) pre-Haiyan (reference), (ii) damaged canopy post Haiyan, and (iii) recovered canopy. Before the forest was disturbed, average TF/P, SF/P and I/P ratios were 0.83 ± 0.22, 0.03 ± 0.01 and 0.15 ± 0.22, respectively. During the period with the damaged canopy, the respective ratios were 0.91 ± 0.18, 0.004 ± 0.01 and 0.09 ± 0.15, while 3 months after the passage of Haiyan the forest canopy had recovered more or less in terms of leaf surface area with average TF/P, SF/P and I/P ratios of 0.86 ± 0.22, 0.01 ± 0.06,and 0.13 ± 0.21, respectively. The respective trends reflected the changes in LAI, which dropped from 5.24 ± 0.79 to 3.80 ± 0.80 right after Haiyan, recuperating to 4.69 ± 0.62 after recovery. These changes in rainfall partitioning after typhoon Haiyan are less pronounced than those reported previously for hurricane-affected forests in the Caribbean and the Pacific, possibly because the Manobo forest was relatively sheltered topographically.