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Climate change, sustainability and the need for a new industrial revolution in Scotland

Published online by Cambridge University Press:  22 April 2013

David Sugden
Affiliation:
School of GeoSciences, University of Edinburgh, Edinburgh, EH8 9XP
Janette Webb
Affiliation:
Institute of Governance, School of Social and Political Science, University of Edinburgh, Edinburgh, EH1 1LZ
Andrew Kerr
Affiliation:
Edinburgh Centre for Low Carbon Innovation and Skills, High School Yards, Edinburgh, EH8 9XP
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Abstract

This paper sets the wider global and Scottish context for this Special Issue of EESTRSE. Climate change is inextricably linked to wellbeing, security and sustainability. It poses a fundamental challenge to the way we organise society and our relationship to the exploitation of the Earth's resources. Rising levels of CO2 in the atmosphere, linked to burning fossil fuels and land use, present a major risk of climate change, with serious but uncertain impacts emerging at a regional scale. A new industrial revolution is needed to achieve energy security and to reduce greenhouse gas emissions, with energy efficiency and energy production emitting low or no CO2 at its heart. At present, on a global scale, there is a mismatch between the emphasis on economic growth and the need to reduce emissions and achieve a sustainable use of resources. A more sustainable blueprint for the future is emerging in Europe and Scotland has much to gain economically and socially from this change. Scotland's ambitious emission reduction targets (42% cut by 2020 and 80% by 2050) are achievable, but require major commitment and investment. Despite success in cutting emissions from activities within Scotland, Scotland's consumption-based emissions rose by 11% in 1996–2004.

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Copyright © The Royal Society of Edinburgh 2012 
Figure 0

Figure 1 The rise in atmospheric CO2 (parts per million) compared to the rise in CO2 produced by human activities: (a) The rise in CO2 as measured in Hawaii 1960–2010. Such an island location in the midst of the Pacific Ocean and distant from industrial activity is representative of global trends. The annual fluctuations, superimposed on the overall rise, reflect the seasonal fluctuations caused by vegetation growth in the land-dominated northern hemisphere; (b) The rise in emissions resulting from human activities 1960–2010, calculated from statistics of production and deforestation. PgCyr –1=One petagram=one Gigatonne (Gt). LUC=land use change.

Source: Le Quéré et al.2009.
Figure 1

Figure 2 The concentration of the main greenhouse gases in the atmosphere compared to pre-industrial times (ppm=parts per million; ppb=parts per billion). Greenhouse gases are conventionally expressed as equivalent amounts of CO2, where equivalent means having the same warming affect over 100 years. One ton of carbon-dioxide equivalent is abbreviated as 1tCO2e and one thousand million tons as 1GtCO2e.

Source of data: IPCC 2007b.
Figure 2

Figure 3 Predictions of the rate (black line) and uncertainty (red and blue lines) of global warming forced by rising concentrations of CO2e in the atmosphere. The categories I–VI represent forcing by scenarios of increased levels of greenhouse gases. The implication is that the average climate is likely to stabilise at a warmer level, but of course this does not take into account regional variations.

Source: IPCC 2007a.
Figure 3

Figure 4 The flow of embedded carbon (Mt CO2/yr) incorporated in imported goods. The scale of the flow to the USA and Europe is striking and a measure of how much the richest countries have exported their CO2 emissions to other countries.

Source: Davis & Caldeira 2010.
Figure 4

Figure 5 (a) The Pumpherston shale-oil works in 1941. The shales in the central lowlands of Scotland were mined and processed to produce diesel oil/paraffin, the beginnings of the global petroleum industry. (b) James (Paraffin) Young, chemist, entrepreneur and Fellow of the Royal Society of Edinburgh.

Figure 5

Figure 6 Possible cuts in emissions by sector to be achieved in 2030 en route to the 2050 reduction targets. The different levels of reduction in different sectors reflects what is most feasible.

Source: UK Committee for Climate Change 2010a.
Figure 6

Figure 7 The CO2e emissions targets to 2022 arising from the Climate Change (Scotland) Act 2009.

Source: Scottish Government 2011b.