Coastal squeeze occurs when rising sea levels encroach on lowβlying shorelines faster than the land can naturally migrate inland. The rate of seaβlevel rise (R) combined with the time horizon (T) determines the vertical increase in water level that the coast must accommodate.
The geometry of the coastal plain controls how much horizontal shoreline retreat (S) is required to maintain the same relative elevation. A gentler coastal slope (ΞΈ) forces a larger landward shift for a given vertical rise, while a steep slope limits the retreat distance.
By coupling seaβlevel projections with the slope of the shore, we can estimate the potential loss of coastal habitat and the risk of infrastructure being overtopped. This simple model is a firstβorder tool for planners assessing vulnerability to future seaβlevel scenarios.
What is coastal squeeze?
How does the rate of sea-level rise affect coastal areas?
What role does the geometry of the coastal plain play in coastal squeeze?
How do I use this Coastal Squeeze Calculator?
What are the implications of coastal squeeze for coastal communities?
How does climate change contribute to coastal squeeze?
Can this calculator be used for long-term planning?
Results are for informational purposes only and do not constitute professional advice.
