Nantes is the sixth-largest city in France, and, historically, one of its largest port cities. Much of the city’s activity and residences are built near the water, and sea level rise may cause material damage and eco-societal paralysis. 

Earth.Org has mapped the flooding that could occur in Nantes by 2100. 

Built on the Loire estuary, the surrounding area used to be segmented by many channels, creating small islands and sand ridges. Smaller waterways were later filled in, submerging most of the islands, leaving only the larger Isle of Nantes between the banks of the Loire. 

The river is tidal, meaning its level fluctuates with sea levels. The range can reach around 6 meters (20 feet), as a result of dredging to make the area accessible to larger ships. The eastern part of Nantes is quite flat, and the lowest points of the city are only 2 meters above sea level. 

A recent paper published in Nature estimates that, under high emissions scenarios, global sea levels could rise by an average of 1 to 2 meters by 2100. Adding the large tidal range of the Loire to this means Nantes could experience some severe flooding by the end of the century. Earth>org has mapped what this could look like, along with the amount of population that would be displaced.

sea level rise by 2100 nantes

Sea level rise projections by 2100 for two scenarios with the amount of rise in meters indicated (mild = 3m; extreme = 4m). Percentage and total population displacement indicated bottom right.


Global mean sea level is projected to rise by 2m at the end of this century. However, in order to determine local sea level rise (SLR), one has to take into account local coastal flood levels which could be 2.8m above Mean Higher-High Water (MHHW) at extreme forecasts. These local levels bring variability to the projected SLR from 1m to 6.5m (eg. Rio vs Kolkata).

The SLR scenarios used in this study are based on the forecasts from Climate Central – Coastal Risk Screening Tool  with the following parameters:

Sea level Projection Source:

From two highly cited journals by Kopp et al., estimating SLR mainly due to ocean thermal expansion and ice melt. The mid-range scenario projected 0.5-1.2m of SLR based on different representative concentration pathways (RCP) defined by the IPCC. While the pessimistic scenario added more mechanisms of ice-sheet melting, estimating SLR at 1m-2.5m in 2100, with a projection of 10m SLR at 2300.

Coastal Flooding

More frequent coastal flooding is a direct impact of sea-level rise. Based on the Global tides and surge reanalysis by Muis et al., (2016), it is estimated that the extreme coastal water level could be from 0.2 – 2.8m over the mean level. While in extreme cases like China and the Netherlands it could experience 5-10m of extreme sea levels. Here, the coastal local flood level is added on top of the projected SLR.

Pollution Scenario:

Allows choosing the RCP, the greenhouse gas concentration trajectory defined by the IPCC.  The mild level is based on RCP4.5, of 2°C temperature rise; while the Extreme level is based on RCP 8.5, of 4°C temperature rise.


Applies to the baseline SLR, defined in the “Sea level projection” section, upon which we add flooding. “Mild” refers to the mid-range scenario of 0.5-1.2m, and “extreme” to the pessimistic scenario of 1-2.5m. We used the high-end value of each scenario (mild = 1m; extreme = 2.5m).

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