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Modelling the time course of shade,temperature, and wood recovery in streams with riparian forest restoration
Authors:Robert J Davies‐Colley  Mark A Meleason  Raeme MJ Hall  J Christopher Rutherford
Institution:1. National Institute of Water and Atmospheric Research Limited , Box 11–115, Hamilton, New Zealand E-mail: r.davies‐colley@niwa.co.nz;2. 4742 Liberty Rd #312, Salem, OR, 97302, United States;3. 315 Madras Street, Christchurch, 8013, New Zealand;4. National Institute of Water and Atmospheric Research Limited , Box 11–115, Hamilton, New Zealand
Abstract:Action is increasingly being taken in New Zealand and elsewhere to restore ecological function to streams through planting of riparian zones. We used simulation modelling to explore the relative performance of three strategies to restore the riparian zone of a pastoral stream to native forest by: (1) passive regeneration; (2) planting then abandonment of a Pinus radiata plantation; and (3) active restoration by planting selected native trees. We linked the forest model LINKNZ with a shade and temperature model (sWAIORA), and a wood model (OSU_STREAMWOOD) to simulate recovery trajectories for key forest stream attributes in hypothetical streams (1.3–14.0 m channel width) in the central North Island, New Zealand. Both active restoration strategies outperformed passive regeneration in shade, temperature and stream wood volume for most of the simulation time (800 years). Although the abandoned pine plantation provided greatest shade initially (<100 years), active native planting provided the greatest benefits overall. In general, recovery of stream shade (and temperature) is expected within decades, is accelerated by deliberate planting, and is fastest in small streams in which thermal stress from sunlight exposure is greatest. However, full recovery of stream and riparian function may take centuries, being dependent on large trees providing wood to structure the channel.
Keywords:riparian scenarios  simulation modelling  stream wood  light exposure  thermal regime
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