Using a Hydrological Model to Understand the Hydrological Processes in a Mosaic Tropical Peatland Landscape of Pulau Padang, Indonesia
- 1Asia Pacific Resources International Ltd., Pangkalan Kerinci, Indonesia (adibtya_asyhari@aprilasia.com)
- 2Centre for Ecology and Hydrology, Bangor, United Kingdom
- 3Centre for Landscape and Climate Research, School of Geography, Geology, and the Environment, University of Leicester, Leicester, United Kingdom
- 4Center for Agricultural Land Resources Research and Development, Bogor, Indonesia
- 5Department of Forestry, University of Tanjungpura, Pontianak, Indonesia
- 6Department of Soil Science and Land Resources, IPB University, Bogor, Indonesia
- 74S Analytics & Modelling Ltd., Edmonton, Canada
- 8Department of Renewable Resources, University of Alberta, Edmonton, Canada
- 9DHI Water and Environment Pte. Ltd., Singapore, Singapore
- 10AgResearch (Lincoln Research Centre), Lincoln, New Zealand
Tropical peatlands play an important role in addressing the climate and nature functions. In these ecosystems, hydrology strongly controls their geomorphology, ecology, and carbon cycle. More frequent and severe droughts driven by climate extremes (e.g. El Niño Southern Oscillation and the Indian Ocean Dipole events) may alter their local hydrology. In addition, growing dependencies on tropical peatlands due to population growth and economic development has resulted in land-cover change. Alteration in the hydrological processes under changing climate and land-cover may have crucial implications on tropical peatlands, but such impacts remain poorly understood.
In this context, we used a coupled MIKE SHE and MIKE Hydro River model to represent the hydrological processes within Pulau Padang (~1,100 km2), a peat-dominated island in the eastern coast of Sumatra, Indonesia. The island is a mosaic landscape of peat swamp forest, smallholder area, and industrial plantation. We collected a comprehensive vegetation and peat properties data from field measurements, supported by high-resolution digital terrain model derived from airborne LiDAR, for the model setup. We calibrated and validated the model against observed groundwater level and stream flow data distributed across the island. Finally, we also evaluated the impacts of land-cover change trajectory in the island by comparing the water balance components (i.e. evapotranspiration, runoff, and storage change) for different hydroclimatic extremes (i.e. El Niño and La Nina) under its current condition (baseline year of 2016) to that of its past (25-year look back period) and future (50-year trajectory) conditions.
This research should contribute to advance the understanding of the landscape scale hydrological processes in tropical peatlands under land-cover change trajectory, which are important to provide scientific basis for stakeholders involved in guiding responsible peatland management practices. This presentation will discuss the modeling approach and preliminary results.
How to cite: Asyhari, A., Kurnianto, S., Suardiwerianto, Y., Hidayat, M. F., Harahap, Mhd. I. F., Evans, C., Page, S., Agus, F., Astiani, D., Sabiham, S., Mezbahuddin, S., Balamurugan, M., Ghimire, C. P., and Deshmukh, C. S.: Using a Hydrological Model to Understand the Hydrological Processes in a Mosaic Tropical Peatland Landscape of Pulau Padang, Indonesia, EGU General Assembly 2022, Vienna, Austria, 23–27 May 2022, EGU22-6791, https://doi.org/10.5194/egusphere-egu22-6791, 2022.
