globalchange  > 气候变化事实与影响
DOI: doi:10.1038/nclimate2737
论文题名:
Earth system modelling: Restoration of the oceans
作者: Richard Matear
刊名: Nature Climate Change
ISSN: 1758-808X
EISSN: 1758-6928
出版年: 2015-08-03
卷: Volume:5, 页码:Pages:1028;1029 (2015)
语种: 英语
英文关键词: Social scientist/Social science ; Geography/geographer ; Sociology/sociologist ; Environmental economics/Economist ; Climate policy ; Environmental policy ; Global change ; Earth system science ; Climatologist ; Climate science ; Carbon management ; Carbon markets ; Energy ; Renewables ; Palaeoclimatology/Palaeoclimatologist ; Climate modelling/modeller ; Carbon cycle ; Atmospheric scientist ; Oceanography/marine science ; Sustainability ; Geophysicist/Geophysics ; Biogeoscience/Biogeoscientist ; Hydrology/Hydrogeology ; Greenhouse gas verification ; Ecologist/ecology ; Conservation ; Meteorology/meteorologist
英文摘要:

Undoing the effects of continuing high carbon dioxide emissions on the oceans could take centuries, if it is possible at all.

Evidence is mounting that the climate is changing because of rising atmospheric carbon dioxide1 with the potential that global warming and ocean acidification may significantly harm the ocean environment and the ecosystem services we depend on2. In the absence of a global agreement to limit emissions, all options must be considered to minimize these potential impacts1. Carbon dioxide removal (CDR), which requires the capture and storage of atmospheric carbon, is one potential technological solution to help mitigate high atmospheric carbon dioxide. Writing in Nature Climate Change, Sabine Mathesius and colleagues explore the ability of CDR to mitigate global warming and ocean acidification3. Although the thought of deliberately manipulating the climate by CDR may be unpalatable to many, it is necessary that such options be evaluated to enable informed choices of the viable ways to tackle our carbon dioxide problem.

The study by Mathesius et al.3 explores whether CDR under high CO2 emissions can achieve an environmental outcome similar to a rapid transition to low-carbon energy use (that is, the Representative Concentration Pathway (RCP) 2.6 scenario). For their reference simulation with CDR they use the 'business as usual' high carbon emissions scenario (RCP8.5 extended4) from the present day to 2700. They show, consistent with other computer simulations, that under such a scenario the ocean environment will undergo substantial changes. By the year 2500, the global surface ocean warms by more than 5 °C and the global surface pH declines by more than 0.6 units from the pre-industrial values. Such large changes in the ocean environment have the potential to be catastrophic for many marine organisms, as is evident from the numerous species extinctions that occurred during the Paleocene–Eocene Thermal Maximum, when global temperatures and carbon dioxide levels had a similar magnitude of change5.

NASTCO / ISTOCK / THINKSTOCK

  1. IPCC Summary for Policymakers in Climate Change 2013: The Physical Science Basis (eds Stocker, T. F. et al.) (Cambridge Univ. Press, 2013).
  2. Hennige, S., Roberts, M. & Williamson, P. (eds) An Updated Synthesis of the Impacts of Ocean Acidification on Marine Biodiversity (Secretariat of the Convention on Biological Diversity, Technical Series no. 75, 2014).
  3. Mathesius, S., Hofmann, M., Caldeira, K. & Schellnhuber, H. J. Nature Clim. Change 5, 11071113 (2015).
  4. Meinshausen, M. et al. Climatic Change 109, 213241 (2011).
  5. Pelejero, C., Calvo, E. & Hoegh-Guldberg, O. Trends Ecol. Evol. 25, 332344 (2010).

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Affiliations

  1. Richard Matear and Andrew Lenton are at the Commonwealth Scientific and Industrial Research Organisation (CSIRO), Oceans and Atmosphere Research, GPO Box 1538, Hobart, TAS, Australia 7001

URL: http://www.nature.com/nclimate/journal/v5/n12/full/nclimate2737.html
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/4636
Appears in Collections:气候变化事实与影响
科学计划与规划
气候变化与战略

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Recommended Citation:
Richard Matear. Earth system modelling: Restoration of the oceans[J]. Nature Climate Change,2015-08-03,Volume:5:Pages:1028;1029 (2015).
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