Simulations show that the amount of sea level rise in coastal cities around the world could vary significantly by the end of the century, depending on the emissions scenario and local factors.

Under a low emissions scenario, global mean sea levels could rise by around 0.2-0.4 meters by 2100. However, under a high emissions scenario, sea levels could rise by more than 1 meter.

Local factors, such as land subsidence, glacial melting, and storm surge, could also affect sea level rise in particular areas. For example, cities in areas with high rates of land subsidence, such as Jakarta, Indonesia, could experience even greater sea level rise.

Here are some specific examples of simulated sea level rise in major coastal cities around the world:

- New York City, USA: 1.1 meters under a high emissions scenario

- Miami, USA: 1.4 meters under a high emissions scenario

- London, UK: 0.9 meters under a high emissions scenario

- Shanghai, China: 1.2 meters under a high emissions scenario

- Mumbai, India: 1.2 meters under a high emissions scenario

- Dhaka, Bangladesh: 1.3 meters under a high emissions scenario

It is important to note that these simulations are just projections, and the actual amount of sea level rise could be different. Nevertheless, they provide valuable information that can help coastal communities plan for the future and adapt to the impacts of climate change.