The sky over the harbor lifts from iron to pearl. The bodega door chimes; two teenagers step in, their sneakers leaving crescent prints that will dry by noon and return by night. Dale checks the stain on the brick one more time, the engineer folds his plans, and the tide decides the schedule. Walking back from the seawall, you can taste the day’s heat lifting the metal in the air. The hiss at the curb thins, then returns at the next dip, and the next. The city has always been a coastline. The only new thing is how fast the shoreline is moving—and how little time we have to decide which blocks follow it under. The tide is keeping time; policy is lagging the beat.
Bibliography
1. Intergovernmental Panel on Climate Change (IPCC). Climate Change 2021: The Physical Science Basis. Cambridge: Cambridge University Press, 2021. Establishes the consensus that AMOC is very likely to weaken this century while judging a collapse before 2100 as very unlikely, setting the baseline risk frame used by planners and press.
2. Caesar, Levke, Stefan Rahmstorf, Alexander Robinson, Gábor Feulner, and Vlada Saba. “Observed Fingerprint of a Weakening Atlantic Ocean Overturning Circulation.” Nature 556 (2018): 191–196. Provides observational evidence (SST “fingerprint”) that AMOC is at a multi-century low, anchoring many “weakening” claims.
3. Thornalley, David J. R., Delia W. Oppo, Paul Keigwin, et al. “Anomalously Weak Labrador Sea Convection and Atlantic Overturning During the Past 150 Years.” Nature 556 (2018): 227–230. Uses paleo-proxies to show historical AMOC weakness, complementing Caesar et al.’s surface-based fingerprint.
4. McCarthy, G. D., E. Frajka-Williams, W. E. Johns, et al. “Measuring the Atlantic Meridional Overturning Circulation at 26° N.” Nature 521 (2015): 508–510. Describes the RAPID array and documents strong variability and a lower mean post-2008, giving the primary instrumental backbone for AMOC trends.
5. Levermann, Anders, Jenny Griesel, Michael Hofmann, Marcus Montoya, and Stefan Rahmstorf. “Dynamic Sea Level Changes Following Changes in the Thermohaline Circulation.” Climate Dynamics 24 (2005): 347–354. Classic paper quantifying the rapid regional sea-level “step” along the U.S. East Coast when AMOC/Gulf Stream weakens.
6. Goddard, Paul B., Jianjun Yin, Stephen M. Griffies, and Matthew Winton. “An Extreme Event of Sea-Level Rise Along the Northeast Coast of North America in 2009–2010.” Nature Communications 6 (2015): 6346. Links an AMOC/Gulf Stream anomaly to a sudden, damaging spike in Northeast U.S. coastal water levels.
7. Yin, Jianjun, Michael E. Schlesinger, and Ronald J. Stouffer. “Model Projections of Rapid Sea-Level Rise on the Northeast Coast of the United States.” Nature Geoscience 2 (2009): 262–266. Projects a distinct dynamic sea-level rise signal for the Northeast U.S. driven by circulation change, widely cited in regional planning.
8. Volkov, Denis L., Francisco M. Calafat, Stéphan D. Howden, and Frederick M. Bingham. “Unprecedented Acceleration of Sea Level Along the U.S. Southeast and Gulf Coasts During 2010–2022.” Nature Communications 14 (2023): 2765. Documents recent coastal sea-level acceleration and implicates circulation-driven dynamics that compound flood risk.
9. van Westen, René M., Henk A. Dijkstra, and colleagues. “Physics-Based Early Warning for a Collapse of the Atlantic Meridional Overturning Circulation.” Geophysical Research Letters 51 (2024). Develops indicators suggesting mid-century onset windows for an AMOC tipping process under continued warming, sharpening risk timelines.
10. Baker, Jonathan C. A., et al. “AMOC Collapse in the Next 75 Years Is Unlikely, but Continued Weakening Is Very Likely.” Nature (2025). Uses targeted modelling to argue against a near-term shutdown while emphasizing societally significant weakening—an important counterpoint in the literature.
11. Drijfhout, Sybren, Stefan Rahmstorf, and co-authors. “Multi-Century CMIP6 Extensions Indicate Elevated AMOC Shutdown Risk Beyond 2100.” Environmental Research Letters (2025). Extends standard scenarios to 2300–2500 and finds tipping thresholds likely crossed within decades, with shutdown lagging by 50–100 years.
12. Zhang, Rong, and Thomas L. Delworth. “Simulated Tropical Response to a Substantial Weakening of the AMOC.” Geophysical Research Letters 32 (2005): L16703. Shows a southward shift of the ITCZ and broad hydroclimate reorganization under a weakened AMOC, underpinning rainfall-belt impacts.
13. Poloczanska, Elvira S., et al. “Global Imprint of Climate Change on Marine Life.” Science 341, no. 6145 (2013): 1239–1242. Synthesizes observed range shifts and phenology changes in marine taxa, contextualizing fisheries responses to changing currents and temperatures.
14. Bryndum-Buchholz, Andreas, et al. “Twenty-First-Century Climate Change Impacts on Marine Animal Biomass and Ecosystem Structure.” Proceedings of the National Academy of Sciences 116, no. 26 (2019): 12907–12912. Uses the EcoOcean framework to project declines in total system biomass and stronger impacts at higher trophic levels under warming and circulation changes.