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Benjamin H. Strauss

Researcher at Climate Central

Publications -  36
Citations -  3622

Benjamin H. Strauss is an academic researcher from Climate Central. The author has contributed to research in topics: Coastal flood & Population. The author has an hindex of 16, co-authored 34 publications receiving 2801 citations. Previous affiliations of Benjamin H. Strauss include Princeton University.

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Probabilistic 21st and 22nd Century Sea-Level Projections at a Global Network of Tide-Gauge Sites

TL;DR: In this article, the authors presented a global set of local sea-level (LSL) projections to inform decisions on timescales ranging from the coming decades through the 22nd century and provided complete probability distributions, informed by a combination of expert community assessment, expert elicitation, and process modeling.
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New elevation data triple estimates of global vulnerability to sea-level rise and coastal flooding.

TL;DR: A new digital elevation model utilizing neural networks is employed and it is shown that the new DEM more than triples the NASA SRTM-based estimates of current global population occupying land below projected sea levels in 2100, with more than 200 million people could be affected based on RCP4.5 and 2 degC of warming.

Earth's Future Probabilistic 21st and 22nd century sea-level projections at a global network of tide-gauge sites

TL;DR: This article presented a global set of local sea-level (LSL) projections to inform decisions on timescales ranging from the com- ing decades through the 22nd century, and provided complete probability distributions, informed by a combination of expert community assessment, expert elicitation, and process modeling.
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Modelling sea level rise impacts on storm surges along US coasts

TL;DR: In this paper, the influence of sea level rise on expected storm surge-driven water levels and their frequencies along the contiguous United States is investigated, and substantial changes in the frequency of what are now considered extreme water levels may occur even at locations with relatively slow local sea-level rise, when the difference in height between presently common and rare water levels is small.