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245 00 |a Long-term sea-level rise implied by 1.5 degree C and 2 degree C warming levels |h [electronic resource].
260        |a [S.l.] : |b Macmillan Publishers Limited, |c 2012-06-24.
490        |a Nature Climate Change.
506        |a Please contact the owning institution for licensing and permissions. It is the user's responsibility to ensure use does not violate any third party rights.
520 3    |a Sea-level rise (SLR) is a critical and uncertain climate change risk, involving timescales of centuries. Here we use a semiempirical model, calibrated with sea-level data of the past millennium, to estimate the SLR implications of holding warming below 2 C or 1.5 C above pre-industrial temperature, as mentioned in the Cancún Agreements. Limiting warming to these levels with a probability larger than 50% produces 75–80 cm SLR above the year 2000 by 2100. This is 25 cm below a scenario with unmitigated emissions, but 15 cm above a hypothetical scenario reducing global emissions to zero by 2016. The long-term SLR implications of the two warming goals diverge substantially on a multi-century timescale owing to inertia in the climate system and the differences in rates of SLR by 2100 between the scenarios. By 2300 a 1.5 C scenario could peak sea level at a median estimate of 1.5m above 2000. The 50% probability scenario for 2 C warming would see sea level reaching 2.7m above 2000 and still rising at about double the present-day rate. Halting SLR within a few centuries is likely to be achieved only with the large-scale deployment of CO2 removal efforts, for example, combining large-scale bioenergy systems with carbon capture and storage.
533        |a Electronic reproduction. |c Florida International University, |d 2015. |f (dpSobek) |n Mode of access: World Wide Web. |n System requirements: Internet connectivity; Web browser software.
650        |a Climate change.
650        |a Sea level rise.
650        |a Emission reduction.
650        |a Coastal management.
650        |a Greenhouse gas.
720        |a Schaeffer,Michael.
720        |a Hare,William.
720 1    |a Rahmstorf, Stefan.
720 1    |a Vermeer, Martin.
773 0    |t Long-term sea-level rise implied by 1.5 degree C and 2 degree C warming levels
830    0 |a dpSobek.
830    0 |a Sea Level Rise.
852        |a dpSobek |c Sea Level Rise
856 40 |u http://dpanther.fiu.edu/dpService/dpPurlService/purl/FI15060989/00001 |y Click here for full text
856 42 |3 Host material |u http://www.nature.com/nclimate/journal/v2/n12/full/nclimate1584.html |y Long-term sea-level rise implied by 1.5 degree C and 2 degree C warming levels
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/09/89/00001/Schaeffer et al_2012_Long-term sea-level rise implied by 1thm.jpg
997        |a Sea Level Rise


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