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Riccardo Riva

Researcher at Delft University of Technology

Publications -  118
Citations -  5264

Riccardo Riva is an academic researcher from Delft University of Technology. The author has contributed to research in topics: Post-glacial rebound & Sea level. The author has an hindex of 32, co-authored 103 publications receiving 4338 citations. Previous affiliations of Riccardo Riva include Utrecht University & University of Milan.

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Reassessment of the Potential Sea-Level Rise from a Collapse of the West Antarctic Ice Sheet

TL;DR: The potential contribution to eustatic and regional sea level from a rapid collapse of the West Antarctic Ice Sheet is reassessed and it is found that previous assessments have substantially overestimated its likely primary contribution.
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Assessing the impacts of 1.5 °C global warming - simulation protocol of the Inter-Sectoral Impact Model Intercomparison Project (ISIMIP2b)

Katja Frieler, +60 more
TL;DR: In Paris, France, December 2015, the Conference of the Parties (COP) to the United Nations Framework Concerning on Climate Change (UNFCCC) invited the Inter- governmental Panel on Climate change (IPCC).
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Global sea-level budget 1993 - present

Anny Cazenave, +89 more
TL;DR: In this paper, the authors present estimates of the altimetry-based global mean sea level (average variance of 3.1 +/- 0.3 mm/yr and acceleration of 0.1 mm/r2 over 1993-present), as well as of the different components of the sea level budget over 2005-present, using GRACE-based ocean mass estimates.
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Towards regional projections of twenty-first century sea-level change based on IPCC SRES scenarios

TL;DR: In this paper, the authors present maps of twenty-first century local relative sea-level (RSL) change estimates based on an ensemble of coupled climate model simulations for three emission scenarios.
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Reassessment of 20th century global mean sea level rise

TL;DR: A 20th-century GMSL reconstruction computed using an area-weighting technique for averaging tide gauge records that both incorporates up-to-date observations of vertical land motion (VLM) and corrections for local geoid changes resulting from ice melting and terrestrial freshwater storage and allows for the identification of possible differences compared with earlier attempts is presented.