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What-If

Explore what could change.

Choose a place, a documented issue and one of its documented interventions, then set how far it goes.

ILLUSTRATIVE SCENARIO — NOT A SCIENTIFIC PREDICTION. Built from documented causes, impacts and solutions plus general qualitative patterns. It contains no modelled numbers.

3 · Intervention
PilotScaledTransformative

Adopted across much of the area, with dedicated budgets and enforcement.

Illustrative scenario

What if Miami took a scaled approach to “Stormwater pumps and one-way valves”?

Starting point · documented

OceansSeverity: Critical
Sea level rise and tidal flooding in Miami

Rising seas cause recurrent sunny-day flooding and threaten freshwater supplies.

The intervention · documented

Stormwater pumps and one-way valves

Installing pumping and backflow prevention where gravity drainage no longer works.

Reduces recurrent tidal street flooding in treated areas.

Schematic direction of change

Local action builds resilience, but ocean warming and acidification depend on global emissions.

Schematic, unitless illustration: relative pressure over time without the intervention compared with the intervention in place. Not based on measured data.NowLonger term →Relative pressure (unitless)
Without the intervention With the interventionSchematic shape only — no data, units or dates.

Causes this could address

  • Porous limestone bedrockWater moves through the underlying limestone, so seawalls alone cannot prevent water emerging inland.
  • Gravity-based stormwater drainageDrainage designed to discharge by gravity loses capacity as sea level rises.

Impacts that could ease

  • Recurrent high-tide floodingStreets and low-lying property flood during seasonal high tides without any storm present.
  • Saltwater intrusion into drinking waterSalt moving inland through the Biscayne aquifer threatens wellfields that supply the region.

Wider reach at higher intensity is an assumption of this illustration.

How change might unfold

  1. Near term

    Reduced local pressures such as pollution or overfishing give ecosystems some relief.

  2. Medium term

    More resilient ecosystems may recover faster between disturbances.

  3. Long term

    Long-term outcomes depend heavily on the trajectory of global warming.

Faded stages are less likely to be reached at scaled intensity.

What this would not change

Marine heatwaves and sea level rise are driven globally and will continue without global emission cuts.

What it depends on

  • Sustained funding and institutional capacity
  • Consistent enforcement and monitoring
  • Local stakeholder support
  • Participation of affected communities

ILLUSTRATIVE SCENARIO — NOT A SCIENTIFIC PREDICTION. Built from documented causes, impacts and solutions plus general qualitative patterns. It contains no modelled numbers.