Understanding Sea Level Rise Projections and the Role of Scenarios
The 21st century has witnessed an unprecedented rise in global mean sea level (GMSL), a trend that is projected to continue till at least 2100. The Intergovernmental Panel on Climate Change (IPCC) reports that GMSL rose faster in the 20th century than in any prior century over the last three millennia. The rise has been attributed to ocean thermal expansion and mass loss from glaciers and ice sheets, with minor contributions from changes in land-water storage.
However, these projections come with a degree of uncertainty. The future sea level rise could be influenced by earlier-than-projected disintegration of marine ice shelves, abrupt onset of marine ice sheet instability, and faster-than-projected changes in the surface mass balance and discharge from Greenland. These processes are characterized by deep uncertainty due to limited process understanding, limited availability of evaluation data, uncertainties in their external forcing, and high sensitivity to uncertain boundary conditions and parameters.
Why Do We Use Scenarios in Climate Change Science for Projections?
Scenarios are used in climate change science to understand the potential future impacts of climate change. They provide a structured way to explore and communicate complex, uncertain future conditions. In the context of climate change, scenarios are not predictions or forecasts, but rather plausible descriptions of how the future might evolve.
What are Shared Socioeconomic Pathways (SSPs)?
Shared Socioeconomic Pathways (SSPs) are scenarios used by climate researchers to project the potential future states of societies and economies. They consider various factors like population growth, economic development, education, urbanization, and the rate of technological change. The IPCC has defined five SSPs, each representing a different trajectory for societal development in the absence of climate policy intervention and a different level of challenges to mitigation and adaptation.
How are SSPs related to Sea Level Rise and Coastal Management?
SSPs play a crucial role in understanding the potential impacts of sea level rise and formulating effective coastal management strategies. They help us understand how different societal pathways might influence greenhouse gas emissions, which in turn drive global warming and sea level rise. By understanding these potential future states, we can better plan for and manage the risks associated with sea level rise.
Sea Level Rise on each SSP in Europe
Each SSP represents a different potential future, and thus, a different potential impact from sea level rise. For instance, under SSP1-1.9, where warming is held to approximately 1.5°C above 1850-1900 levels by 2100, the projected sea level rise is lower compared to SSP5-8.5, a high reference scenario with no additional climate policy, where emission levels are highest.
In Europe, as in the rest of the world, the impact of sea level rise will vary significantly depending on the SSP. Coastal areas will face increased risks from flooding, erosion, and other coastal hazards. The ability of these areas to adapt to these changes will depend on a variety of factors, including the rate of sea level rise, the physical characteristics of the coast, and the societal and economic pathway followed.
In conclusion, understanding and considering SSPs is crucial in our fight against climate change. They provide us with a framework to understand potential future societal and economic conditions, helping us prepare for and mitigate the impacts of sea level rise. As we continue to refine these pathways and our understanding of their implications, they will remain an essential tool in our climate change arsenal.