Located on the west bank of the Guayas River, Guayaquil is the second-largest city in Ecuador. Its 3 million inhabitants are no strangers to natural disasters, as earthquakes and floods are a constant threat. It is ranked 4th on the list of cities most vulnerable to sea level rise, and Earth.Org has mapped flooding by 2100 to illustrate why. 

Located in the Guayaquil flooded grasslands, the eponymous city is dry for the most part, except during the months of January to April when it experiences heavy rainfall. The wetlands have been reclaimed for agriculture to the point of critically endangering the ecosystem. 

The Guayas River is tidal, meaning its level fluctuates with that of the sea. The lack of natural drainage from filling the surrounding wetlands, combined with the intense rainy season, makes flooding a common ailment for the citizens of Guayaquil. 

Well aware of the risks, the community runs emergency drills and monitors sea levels closely, but if these reach 1 to 2 meters, as they are expected to by the end of the century, there won’t be many affordable solutions available. Earth.Org has modelled the flooding Guayaquil could experience by 2100, as a call for awareness.

sea level rise by 2100 guayaquil

Sea level rise projections by 2100 for two scenarios with the amount of rise in meters indicated (mild = 2m; extreme = 3m). 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).

You might also like: Sea Level Rise by the End of the Century – New York City