Explore the words cloud of the RISeR project. It provides you a very rough idea of what is the project "RISeR" about.
The following table provides information about the project.
Coordinator |
UNIVERSITY OF LEEDS
Organization address contact info |
Coordinator Country | United Kingdom [UK] |
Total cost | 1˙997˙680 € |
EC max contribution | 1˙997˙680 € (100%) |
Programme |
1. H2020-EU.1.1. (EXCELLENT SCIENCE - European Research Council (ERC)) |
Code Call | ERC-2018-STG |
Funding Scheme | ERC-STG |
Starting year | 2019 |
Duration (year-month-day) | from 2019-02-01 to 2024-01-31 |
Take a look of project's partnership.
# | ||||
---|---|---|---|---|
1 | UNIVERSITY OF LEEDS | UK (LEEDS) | coordinator | 1˙978˙233.00 |
2 | UNIVERSITY OF SOUTHAMPTON | UK (SOUTHAMPTON) | participant | 19˙447.00 |
Global sea-level rise is one of our greatest environmental challenges and is predicted to continue for hundreds of years, even if global greenhouse-gas emissions are stopped immediately. However, the range, rates and responses to sea-level rise beyond 2100 are poorly understood. Current models that project sea-level rise centuries into the future have large uncertainties because the recent observations upon which they are based, encompass too limited a range of climate variability. Therefore, it is crucial to turn to the geological record where there are large-scale changes in climate. Global temperatures during the Last Interglacial were ~1oC warmer than pre-industrial values and 3-5oC warmer at the poles (a pattern similar to that predicted in the coming centuries), and global sea level was 6-9 m higher, far above that experienced in human memory.
Through the RISeR project, I will lead a step-change advance in our understanding of the magnitude, rates and drivers of sea-level change during the Last Interglacial, to inform both global and regional sea-level projections beyond 2100. Specifically I will:
1. Develop new palaeoenvironmental reconstructions of Last Interglacial sea-level change from northwest Europe; 2. Provide the first ever chronological constraints on the timing, and therefore rates, of relative sea-level change that occurred in northwest Europe during the Last Interglacial; 3. Use state-of-the-art numerical modelling to distinguish the relative contributions of the Greenland and Antarctica ice sheets to global sea-level rise during the Last Interglacial; 4. Provide estimates of the land areas and exposed populations in northwest Europe at risk of inundation by long-term (2100) sea-level rise, providing high-end scenarios critical for coastal-risk management practice.
These ambitious objectives will result in a state-of-the-art integrated study of the most appropriate analogue for a critical global environmental challenge; future sea-level rise.
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The information about "RISER" are provided by the European Opendata Portal: CORDIS opendata.