Related Experiment Video
Updated: Nov 22, 2025

04:41
A Simple Planting Technique for Re-establishing Trees Where Frequent Inundation Occurs
Published on: January 26, 2018
6.4K
Intertidal wetland vegetation dynamics under rising sea levels
Duncan Rayner1, William Glamore1, Lisa Grandquist2
1Water Research Laboratory, School of Civil and Environmental Engineering, UNSW Sydney, NSW, Australia.
The Science of the Total Environment
|January 9, 2021
Summary
Intertidal wetlands can persist with current sea level rise (SLR) if sediment accretion keeps pace. Accelerated SLR beyond wetland accretion capacity will cause significant species shifts and habitat loss.
Area of Science:
- Ecological modeling
- Coastal geomorphology
- Climate change adaptation
Background:
- Intertidal wetlands face decline due to climate change, especially sea level rise (SLR).
- Wetland adaptation strategies include upslope retreat, sediment capture, and organic accretion.
- Assessing accretion rates against SLR is crucial for predicting wetland resilience.
Purpose of the Study:
- To evaluate the impact of sediment accretion versus sea level rise (SLR) on saltmarsh species composition.
- To develop an eco-hydraulic model for predicting inundation and species distribution.
- To forecast future saltmarsh composition under various SLR and accretion scenarios.
Main Methods:
- Developed an eco-hydraulic calculation method for tidal inundation statistics.
- Utilized high-resolution hydrodynamic models to simulate SLR and accretion scenarios.
- Applied the eco-hydraulic method to predict saltmarsh species composition changes.
Main Results:
- Saltmarsh species composition and extent are predicted to persist under current SLR rates.
- Accelerated SLR exceeding wetland accretion capacity will lead to species shifts and increased open water.
- Current sediment accretion rates may be insufficient for future adaptation to projected SLR.
Conclusions:
- Wetland resilience to SLR is dependent on the balance between accretion and inundation.
- Effective adaptation requires increased sediment capture and elevation change to match accelerating SLR.
- Proactive management strategies are needed to enhance coastal wetland adaptation to climate change.
Related Concept Videos
Responses to Drought and Flooding
11.5K
Water plays a significant role in the life cycle of plants. However, insufficient or excess of water can be detrimental and pose a serious threat to plants.
11.5K
Responses to Salt Stress
13.8K
Salt stress—which can be triggered by high salt concentrations in a plant’s environment—can significantly affect plant growth and crop production by influencing photosynthesis and the absorption of water and nutrients.
13.8K
Primary Production
24.6K
The total amount of energy acquired by primary producers in an ecosystem is called gross primary production (GPP). However, of this energy, producers use some for metabolic processes, and some is lost as heat, decreasing the amount of energy available to the next trophic level. The remaining usable amount of energy is called the net primary productivity (NPP). In terrestrial ecosystems, NPP is driven by climate, while light penetration and nutrient availability drive NPP in aquatic ecosystems.
24.6K
Adaptations that Reduce Water Loss
27.2K
Though evaporation from plant leaves drives transpiration, it also results in loss of water. Because water is critical for photosynthetic reactions and other cellular processes, evolutionary pressures on plants in different environments have driven the acquisition of adaptations that reduce water loss.
27.2K
What is an Ecosystem?
44.9K
Overview
44.9K
Seedless Vascular Plants
65.6K
Seedless Vascular Plants Were the First Tall Plants on Earth
65.6K

