
Local Shocks, Global Ripples: Climate Disruptions in Maritime Trade Networks
Climate change is projected to intensify economic damages worldwide, while trade can buffer these impacts by reallocating goods across regions. This adaptive role depends on the reliability of global trade networks, and maritime chokepoints are exposed: localized shocks can propagate through shipping networks, generating welfare losses far beyond the directly affected region. This paper studies this mechanism using the Panama Canal, whose lock system relies on a freshwater reservoir (Gatun Lake), tracing three margins: Canal operations, trade flows, and network propagation. Canal throughput declines once Gatun Lake falls below the Authority’s 82-foot water-security threshold. Low-water months have about 8% fewer transits and 6% less toll revenue, with the adjustment concentrated in the number of transits rather than in cargo per vessel. To estimate the trade response, I construct a scarcity index and decompose it into seasonal, low-frequency, and unanticipated components. Predictable seasonal scarcity has no detectable trade effect, while the low-frequency component remains entangled with global demand cycles. The unanticipated component–hydrological variation shippers cannot plan around–reduces trade on Canal-exposed routes by ~1% per foot, while trade along routes that bypass the Canal expands. To quantify propagation, I develop a structural maritime network model with endogenous routing and spillovers. A one-foot unexpected decline raises transport costs on Canal-incident links by ~0.11%. General-equilibrium spillovers amplify the average trade decline among Canal-exposed pairs from about 1% to about 4%. Losses concentrate in the Canal’s neighbors, Latin America and the Caribbean; every U.S. state loses, while some economies along the Suez, Cape, and Malacca corridors gain as trade reallocates. Globally, the aggregate effect is approximately zero–a redistribution across trading partners, not a net loss.


