Island City On a Wedge

Paper Discussion

Dr. James Doss-Gollin

Wednesday, February 4, 2026

Galveston, 1900

Source: Galveston Historical Foundation

September 8, 1900: Category 4 hurricane, 8,000+ deaths

The response:

  • 17-foot seawall (still standing)
  • Raised the entire city by up to 17 feet
  • Moved thousands of buildings

The question: Build a wall? Raise the land? Retreat? All three?

ICOW: The Middle Path

ICOW = Island City On a Wedge (Ceres et al., 2019)

  • Fast: evaluate millions of strategy combinations
  • Rich: graduated damage (not binary)
  • Flexible: portfolios of defenses (wall + retreat + elevate)

Key insight: You don’t need every street corner—just the right abstraction.

How ICOW Works

ICOW takes city geometry + defense choices → computes expected damages. Source: Ceres et al. (2019)

The Wedge Geometry

Today

  1. The Wedge Geometry

  2. The Economics

  3. Activity: Map Your City

Picture a Coastal City

The ICOW paper was modeled after Lower Manhattan. Source: Ceres et al. (2019)

What do coastal cities share?

  • Waterfront at low elevation
  • Terrain rises inland
  • Density highest near water

The Wedge Abstraction

The wedge geometry captures essential features. Source: Ceres et al. (2019)

What Gets Flooded?

Source: Ceres et al. (2019)

If water reaches Zone 4—what’s the damage?

→ Three zones underwater (large fraction of city value)

If water reaches Zone 3?

→ Zero… unless the dike fails

What happens when dikes fail?

Key Parameters

Parameter Symbol Meaning
Maximum elevation \(H_{\text{city}}\) How high does the city rise?
City depth \(D_{\text{city}}\) How far inland does the city extend?
Coastline length \(W_{\text{city}}\) How long is the waterfront?
Seawall height \(H_{\text{seawall}}\) Existing protection height

From the paper (Manhattan): \(H_{\text{city}} \approx 17\) m, \(D_{\text{city}} \approx 2\) km, \(W_{\text{city}} \approx 43\) km

Do these seem reasonable? (We’ll check in the activity.)

The Five Defense Levers

Lever What it does Real-world example
Withdrawal (\(W\)) Vacate low-lying land Managed retreat, buyouts
Dike Base (\(B\)) Where the wall starts Seawall location
Dike Height (\(D\)) How tall the wall is Seawall height
Resistance Height (\(R\)) Flood-proof buildings Elevating structures
Resistance Fraction (\(P\)) What % of buildings Retrofit programs

The key constraint: \(W + B + D \leq H_{\text{city}}\)

You can’t withdraw past the city limits, and you can’t build a dike taller than the land behind it.

The Economics

Today

  1. The Wedge Geometry

  2. The Economics

  3. Activity: Map Your City

Damage Isn’t Binary

Simple models say: flood = total loss, no flood = zero.

Reality: A 1-foot flood ruins your carpet. A 10-foot flood destroys the structure.

ICOW computes damage based on volume flooded:

\[\text{Damage} = \text{Zone Value} \times \frac{\text{Volume Flooded}}{\text{Total Volume}} \times 0.39\]

The 0.39 is an empirically-derived depth-damage parameter: the fraction of zone value destroyed at full inundation (from flood damage curves).

This connects to Monday’s EAD formula (Week 4 lecture)—but now we can compute damage for any surge height.

Dikes Aren’t Perfect

A dike doesn’t magically hold until overtopped, then fail.

Fragility curve: Failure probability ramps up as water approaches the crest

  • Water below 95% of crest: very low failure probability
  • Water at 95%+: failure probability ramps linearly
  • At 100%: certain overtopping

The levee effect: People behind dikes often don’t evacuate. If the dike fails, they’re caught off guard. ICOW models this: damage behind a failed dike is 1.3× worse than open flooding.

Activity: Map Your City

Today

  1. The Wedge Geometry

  2. The Economics

  3. Activity: Map Your City

The Task

Work in pairs. Use Google Maps to estimate ICOW geometry parameters for a real coastal city.

You’ll need:

Make a Prediction

Before we look anything up—take 30 seconds:

Which city do you think has the steepest geometry? (highest \(H_{\text{city}}/D_{\text{city}}\) ratio)

  • Miami Beach
  • Galveston
  • New Orleans
  • Rotterdam
  • Mumbai
  • Venice

Write down your guess. We’ll check later.

Pick a City

  • Galveston, TX
  • Miami Beach, FL
  • New Orleans, LA
  • Boston, MA
  • Mumbai, India
  • Jakarta, Indonesia
  • Lagos, Nigeria
  • Shanghai, China
  • Rotterdam, Netherlands
  • Venice, Italy
  • Ho Chi Minh City
  • Your hometown?

Estimate These Parameters

Parameter How to Estimate
\(H_{\text{city}}\) Elevation change: waterfront → highest urban point
\(D_{\text{city}}\) Horizontal distance: waterfront → highest point
\(W_{\text{city}}\) Length of exposed coastline
\(H_{\text{seawall}}\) Existing protection height (search online)

Tools: Google Maps terrain view, Google Earth elevation, Wikipedia

You’ll need all four parameters for Friday’s lab!

Share Out

Pair up with a table that studied a different city:

  1. Compare your \(H_{\text{city}}/D_{\text{city}}\) ratios
  2. Which city is steeper? Which is flatter?
  3. What does that imply for dike strategy?

Class discussion: A steep city vs. a flat city—who benefits more from a 3m dike?

Key Takeaways

  1. ICOW abstracts complex cities into a few key parameters
  2. The wedge geometry captures essential physics: higher surges flood more area
  3. Different cities → different optimal strategies
  4. Friday’s lab: You’ll use ICOW.jl to compute EAD for a single year

Preview: Friday’s Lab

Friday we’ll implement single-year EAD analysis:

  • Use the same parameters you estimated today
  • Add a storm surge distribution
  • Compute expected annual damage
  • Explore how the five levers change EAD

One More Thing…

Rotterdam is 6 meters below sea level.

How does ICOW even work there?

(We’ll find out Friday.)

References

Ceres, R. L., Forest, C. E., & Keller, K. (2019). Optimization of multiple storm surge risk mitigation strategies for an island City On a Wedge. Environmental Modelling & Software, 119, 341–353. https://doi.org/10.1016/j.envsoft.2019.06.011