Evidence map›Paper›PMID 29610380›Full record

ArticlePhilosophical transactions. Series A, Mathematical, physical, and engineering sciences2018

Stabilization of global temperature at 1.5°C and 2.0°C: implications for coastal areas.

Robert J Nicholls, Sally Brown, Philip Goodwin, Thomas Wahl, Jason Lowe, Martin Solan, Jasmin A Godbold, Ivan D Haigh, Daniel Lincke, Jochen Hinkel and 2 more

Abstract read
In one paragraph

Article in Philosophical transactions. Series A, Mathematical, physical, and engineering sciences, 2018. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 20 papers.

0numbers the graph read from it
0cells of the map it votes in
20citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

20 citing papers in PubMed.

  1. Article
  2. Warming of +1.5 °C is too high for polar ice sheets.Communications earth & environment · 2025
    Review
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  5. Article
  6. Data-driven predictions of the time remaining until critical global warming thresholds are reached.Proceedings of the National Academy of Sciences of the United States of America · 2023
    Article
  7. Article
  8. Article
  9. Article
  10. Article
  11. The changing Arctic Ocean: consequences for biological communities, biogeochemical processes and ecosystem functioning.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2020
    Article
  12. Article
  13. Article
  14. Climate change and ecosystems: threats, opportunities and solutions.Philosophical transactions of the Royal Society of London. Series B, Biological sciences · 2020
    Article
  15. Benthic-based contributions to climate change mitigation and adaptation.Philosophical transactions of the Royal Society of London. Series B, Biological sciences · 2020
    Article
  16. Article
  17. Article
  18. Article
  19. Article
  20. The myriad challenges of the Paris Agreement.Philosophical transactions. Series A, Mathematical, physical, and engineering sciences · 2018
    Article
4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

12 authors.

Robert J NichollsFaculty of Engineering and the Environment, University of Southampton, Highfield, Southampton SO17 1BJ, UK r.j.nicholls@soton.ac.uk.ORCID http://orcid.org/0000-0002-9715-1109
Sally BrownFaculty of Engineering and the Environment, University of Southampton, Highfield, Southampton SO17 1BJ, UK.
Philip GoodwinOcean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK.ORCID http://orcid.org/0000-0002-2575-8948
Thomas WahlCivil, Environmental, and Construction Engineering and National Center for Integrated Coastal Research, University of Central Florida, 12800 Pegasus Drive, Orlando, FL 32816-2450, USA.ORCID http://orcid.org/0000-0003-3643-5463
Jason LoweReading Unit, Met Office Hadley Centre, University of Reading, Reading, UK.ORCID http://orcid.org/0000-0002-8201-3926
Martin SolanOcean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK.ORCID http://orcid.org/0000-0001-9924-5574
Jasmin A GodboldBiological Sciences, University of Southampton, Highfield, Southampton SO17 1BJ, UK.ORCID http://orcid.org/0000-0001-5558-8188
Ivan D HaighOcean and Earth Science, National Oceanography Centre Southampton, University of Southampton, Waterfront Campus, European Way, Southampton SO14 3ZH, UK.ORCID http://orcid.org/0000-0002-9722-3061
Daniel LinckeGlobal Climate Forum, Neue Promenade 6, 10178 Berlin, Germany.ORCID http://orcid.org/0000-0003-4250-5077
Jochen HinkelGlobal Climate Forum, Neue Promenade 6, 10178 Berlin, Germany.ORCID http://orcid.org/0000-0001-7590-992X
Claudia WolffGeographisches Institut, Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Strasse 14, 24098 Kiel, Germany.
Jan-Ludolf MerkensGeographisches Institut, Christian-Albrechts-Universität zu Kiel, Ludewig-Meyn-Strasse 14, 24098 Kiel, Germany.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The effectiveness of stringent climate stabilization scenarios for coastal areas in terms of reduction of impacts/adaptation needs and wider policy implications has received little attention. Here we use the Warming Acidification and Sea Level Projector Earth systems model to calculate large ensembles of global sea-level rise (SLR) and ocean pH projections to 2300 for 1.5°C and 2.0°C stabilization scenarios, and a reference unmitigated RCP8.5 scenario. The potential consequences of these projections are then considered for global coastal flooding, small islands, deltas, coastal cities and coastal ecology. Under both stabilization scenarios, global mean ocean pH (and temperature) stabilize within a century. This implies significant ecosystem impacts are avoided, but detailed quantification is lacking, reflecting scientific uncertainty. By contrast, SLR is only slowed and continues to 2300 (and beyond). Hence, while coastal impacts due to SLR are reduced significantly by climate stabilization, especially after 2100, potential impacts continue to grow for centuries. SLR in 2300 under both stabilization scenarios exceeds unmitigated SLR in 2100. Therefore, adaptation remains essential in densely populated and economically important coastal areas under climate stabilization. Given the multiple adaptation steps that this will require, an adaptation pathways approach has merits for coastal areas.This article is part of the theme issue 'The Paris Agreement: understanding the physical and social challenges for a warming world of 1.5°C above pre-industrial levels'.

Indexed as

climate adaptationclimate mitigationcoastal impactsocean pHsea-level rise

Identifiers

PMID29610380
PMCPMC5897821

What OpenQuestion holds

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LicenceCC BY
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Registered trials

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Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.