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001        FI15061914_00001
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245 00 |a Sea level projections to AD2500 with a new generation of climate change scenarios |h [electronic resource].
260        |a [S.l.] : |b Elsevier, |c 2012.
490        |a Global and Planetary 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 over the coming centuries is perhaps the most damaging side of rising temperature (Anthoff et al., 2009). The economic costs and social consequences of coastal flooding and forced migration will probably be one of the dominant impacts of global warming (Sugiyama et al., 2008). To date, however, few studies (Nicholls et al., 2008; Anthoff et al., 2009) on infrastructure and socio-economic planning include provision for multi-century and multi-metre rises in mean sea level. Here we use a physically plausible sea level model constrained by observations, and forced with four new Representative Concentration Pathways (RCP) radiative forcing scenarios (Moss et al., 2010) to project median sea level rises of 0.57 for the lowest forcing and 1.10 m for the highest forcing by 2100 which rise to 1.84 and 5.49 m respectively by 2500. Sea level will continue to rise for several centuries even after stabilisation of radiative forcing with most of the rise after 2100 due to the long response time of sea level. The rate of sea level rise would be positive for centuries, requiring 200–400 years to drop to the 1.8 mm/yr 20th century average, except for the RCP3PD which would rely on geoengineering.
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    0 |a Climate change.
650    0 |a Sea level rise.
650    0 |a Global warming.
650    0 |a Flooding.
720 1    |a Jevrejeva, S..
720 1    |a Moore, J.C..
720 1    |a Grinsted, A..
773 0    |t Sea level projections to AD2500 with a new generation of climate change scenarios
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/FI15061914/00001 |y Click here for full text
856 42 |3 Host material |u http://www.sciencedirect.com/science/article/pii/S0921818111001469 |y Sea level projections to AD2500 with a new generation of climate change scenarios
992 04 |a http://dpanther.fiu.edu/sobek/content/FI/15/06/19/14/00001/FI15061914thm.jpg
997        |a Sea Level Rise


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