Abstract

AbstractMany tropical peatlands are subjected to artificial drainage that leads to degradation. Hence, hydrological restoration has recently been prioritized. Nevertheless, as field monitoring data are limited, little is known about how restoration measures, such as ditch dams and bunds, can regulate tropical peatland water tables. We used a hydrodynamic model —DigiBog_Hydro— to simulate the effectiveness of ditch dams and bunds across three El Niño–Southern Oscillation (ENSO) scenarios, which are El Niño, La Niña and Neutral, in three typical sites. The sites were moderately degraded (Mod‐Dgr) and severely degraded (Sev‐Dgr) peatland plots (each 0.2 km2), representing typical peatland conditions in Sebangau National Park, Kalimantan, Indonesia. Our fine‐scale (1 m × 1 m spatial resolution) modelling revealed that in the dry season of any ENSO scenario, the significant effects of ditch‐dams alone on peatland water‐level were limited to lateral distances of 26 m (in Mod‐Dgr) and 12 m (in Sev‐Dgr) from the ditch. In the dry season of an El Niño year, the combination of ditch dams and bunds helped maintain water levels up to 72 cm (in Mod‐Dgr) and 69 cm (in Sev‐Dgr) higher than in the no‐restoration condition. During the extreme‐dry period of an El Niño year, the bunds reduced the number of days when the water table was deeper than 40 cm in Mod‐Dgr and in Sev‐Dgr by 50% and 73%, respectively. We suggest that bunds used in combination with ditch dams are a practical restoration measure for tropical peatlands, providing critical extra water storage and helping maintain water tables near the peatland surface in dry periods. We also demonstrate how fine‐scale hydrodynamic modelling is beneficial for planning and assessment of restoration measures in tropical peatlands.

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