BREAKING THE 400 ppm BARRIER: PHYSICAL AND SOCIAL IMPLICATIONS OF THE RECENT CO2 RISE

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The document analyzes the rise of atmospheric CO2, which reached a record high of over 400 ppm in May 2013, and discusses the resulting climate impacts and the necessity of immediate mitigation to avoid dangerous warming.

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  • Atmospheric CO2 concentrations have increased by more than 40% since 1750, rising from 278 ppm to a global average of 394 ppm in 2012. This increase is primarily driven by fossil fuel emissions, which account for two-thirds of the 545 GtC cumulative emissions, and secondarily by land use change, mainly deforestation.
  • In May 2013, the Mauna Loa Observatory in Hawaii recorded a daily CO2 concentration exceeding 400 ppm for the first time in recorded history. This level is the highest in the last 800,000 years and likely the last 2.1 million years.
  • The oceans have absorbed approximately 30% of anthropogenic CO2 emissions, leading to ocean acidification. This process threatens marine calcifying organisms and ecosystem services, including fisheries and coastal infrastructure; for example, reef-building corals are estimated to be lost at a rate of 1–2% per year.
  • Paleoclimate records from ice cores show a strong quantitative correlation between CO2 and global surface temperature over millennial scales. While some warming events are triggered by orbital variations, CO2 acts as a decisive driver or amplifier of warming.
  • Under a 'business as usual' scenario, CO2 concentrations could exceed 500 ppm by the mid-21st century, likely causing a global mean surface temperature increase of more than 2°C. Conversely, reducing emissions by 2% per year starting by 2020 could limit concentrations to below 450 ppm.
  • The 400 ppm threshold is viewed as a significant political marker rather than a physical tipping point, highlighting the 'inaction and indifference' of governments toward climate changes that disproportionately affect vulnerable populations with low adaptive capacity.

Cite the original document

APA
Faria, S. H., Spadaro, J. V., & Markandya, A. (2013). BREAKING THE 400 ppm BARRIER: PHYSICAL AND SOCIAL IMPLICATIONS OF THE RECENT CO2 RISE. Basque Centre for Climate Change. https://www.bc3research.org/h6T8Uy8Nm4gFs0O/201401130413341104337663.pdf
Chicago
Faria, Sérgio H., Joseph V. Spadaro, and Anil Markandya. BREAKING THE 400 ppm BARRIER: PHYSICAL AND SOCIAL IMPLICATIONS OF THE RECENT CO2 RISE. Basque Centre for Climate Change, 2013. https://www.bc3research.org/h6T8Uy8Nm4gFs0O/201401130413341104337663.pdf.
Wikipedia
{{cite report |last1=Faria |first1=Sérgio H. |last2=Spadaro |first2=Joseph V. |last3=Markandya |first3=Anil |title=BREAKING THE 400 ppm BARRIER: PHYSICAL AND SOCIAL IMPLICATIONS OF THE RECENT CO2 RISE |publisher=Basque Centre for Climate Change |date=2013 |url=https://www.bc3research.org/h6T8Uy8Nm4gFs0O/201401130413341104337663.pdf |access-date=23 October 2026 |via=Climate Insights Directory}}
BibTeX
@techreport{faria2013breaking, author = {Faria, Sérgio H. and Spadaro, Joseph V. and Markandya, Anil}, title = {{BREAKING THE 400 ppm BARRIER: PHYSICAL AND SOCIAL IMPLICATIONS OF THE RECENT CO2 RISE}}, institution = {Basque Centre for Climate Change}, year = {2013}, url = {https://www.bc3research.org/h6T8Uy8Nm4gFs0O/201401130413341104337663.pdf}, urldate = {2026-10-23}, note = {Indexed by Climate Insights Directory} }

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