Why should we be concerned?
9. As part of the UK's commitment to address the
issue of climate change during its Presidency of the G8, an international
symposium was held in Exeter during February 2005 to advance scientific
understanding of the long-term implications of climate change.
Some of the key challenges are detailed in Table 2 below.Table
2: Key climate challenges
Avoiding
Dangerous Climate Change - Exeter 2005[11]
Key Challenges
- The ten hottest
years globally since records began in 1860 have occurred since
1991.
- By 2050 between
15%-37% of a sample of 1,103 land plants and animals will eventually
become extinct as a result of climate change.[12]
- The physical
effects of climate change (e.g. the impact on agriculture, increased
mortality, extreme weather and health effects) could cost society
some £70 per tonne of carbon emitted, based on 2000 prices.[13]
- Although agricultural
yields in the EU and the US are predicted to benefit from marginal
increases in average global temperature, yields will fall once
the increased temperature reaches 2°C and above.
- With a 0.8°C
average rise in global temperatures, an additional 400 million
people could be at risk from water stress, with the risk of malaria
in North America increased by a factor of 1.27.
- An increase of
1°C could more than double the number of people at risk from
water stress to an additional 829 million, and decrease the rice
yield in S Asia by 6-10%.
- A rise of between
1-3°C could cause the thermohaline circulationthe
global ocean 'conveyor', of which the Gulf Stream is partto
collapse, impacting upon fisheries, ecosystems and agriculture
throughout Northern and Western Europe. This would constitute
an 'extreme event', the full consequences of which are yet to
be fully understood.
- Increases of
between 2-3°C could cause the Amazon rainforest to collapse
and be replaced by savannah. There will be and increased desertification
as forests and grasslands are lost.
- With an increase
of 2.3°C above pre-industrial levels, there could be some
7 million additional people at risk of hunger in the developing
world.
- A temperature
increase of 2.5-3°C could reduce China's rice yields by 10-20%.
Crop failure in Southern Africa could increase from 50% to 75%
with an increase of 2.5-4°C.
10. Climate change is a global phenomenon which has
an impact upon all aspects of society and the environment. Even
taking into consideration the degree of uncertainty noted by some
commentators, the Intergovernmental Panel on Climate Change (IPCC)
states that the global temperature will increase by at least
1.4°C this century.[14]
Whilst this may not sound significant, the world is already experiencing
the adverse effects of a 0.6°C increase in global temperature.
11. The IPCC states that:
There is new and stronger evidence that most of the
warming observed over the last fifty years is attributable to
human activities.
12. The IPCC predicted in 2001 that average global
temperatures upwards of 0.6°C above pre-industrial levels
would result in increased frequency of heatwaves, with associated
elevated mortality, and decreasing water resources.[15]
13. In August 2003, approximately 15,000 people in
Northern France and some 2,000 people in England and Wales died
as a result of the unusually hot weather.[16]
Across Europe this figure reached 30,000. According to statistical
analyses, approximately half of the severity of the hot summer
can be attributed to global warming with 90% certainty.[17]
14. In the Arctic, average temperatures in the last
few decades have risen at a rate almost twice that of the rest
of the world. Arctic sea ice has already reduced by 15-20%. A
study by NASA found that the Greenland ice sheet was retreating
at a rate of one metre per year in 2001. The most recent study
indicates that it is now retreating at approximately 10 metres
per year. Increased temperatures of just 1.5°C above pre-industrial
levels will precipitate the complete melting of the Greenland
ice sheet, the consequences of which would be severe, particularly
for coastal regions, resulting in an eventual rise in sea level
of some 7 metres (23 feet).[18]
15. Increased global temperatures and the resulting
higher sea levels commonly cited as a consequence are not the
only effects the world will experience as a result of climate
change. Extreme weather phenomena will also become increasingly
common, with heightened frequency and severity of storms, resulting
in increased flooding and coastal erosion. In the early 1980s
the Thames Barrier was used less than once a year. It is now used
on average six times a year.[19]
16. In the UK insurance claims for storm and flood
damage (not all of which are attributable to climate change) have
doubled between 1998 and 2003, when compared to the previous five
years. In 2003, this amounted to £6 billion. Predictions
by the Association of British Insurers suggest this figure could
double or even triple by 2050 unless measures are taken to both
adapt for and mitigate future climate change.[20]
These costs will ultimately be passed on to the consumer, with
some properties such as those in high risks areas for flooding,
becoming uninsurable.[21]
Estimates by Swiss Re, the world's second largest insurer, suggest
that the worldwide financial costs of climate change could double
in the next 10 years to US$150 billion each year.[22]
17. Climate change will also impact upon the marine
environment. A recently published Defra report notes the impact
of climate change on both our coasts and the ocean's temperature,
salinity and acidity.[23]
Researchers from the US Scripps Institution of Oceanography in
San Diego have found clear evidence of an unequivocal link between
greenhouse gas emissions from human activity and oceanic warming.[24]
The concentration of atmospheric carbon dioxide, a potent greenhouse
gas, has increased by approximately 35% since the start of the
industrial revolution. Research by the Plymouth Marine Laboratory
has found that the oceans, a massive sink for atmospheric carbon
which have already taken up just under 50% of all man-made emissions
of CO2, have been gradually increasing in acidity as
a result. This could have several far-reaching consequences; any
changes in oceanic biochemistry will impact upon plankton and
shellfish at the bottom of the food chain, and thus alter the
entire marine ecosystem. It may also signal the demise of coral
reefs.[25]
'Global dimming'
18. Recent research provides evidence for 'global
dimming'. This refers to the reduction of energy from the sun
reaching the surface of the planet due to air pollution. Industrial
waste emissions include small particles as well as the invisible
global warming gases. These particles can be seen in dense urban
areas as smog, and can move into the upper atmosphere where they
both act as a physical barrier to incoming sunlight, and also
increase the reflectivity of the clouds. Consequently, the intensity
of sunlight is reduced, resulting in a global cooling effect,
recently implicated in the failure of the summer monsoon in the
Sahel which caused the great famines in the 1980s. This global
cooling may also have masked the warming effects of greenhouse
gases, causing scientists to underestimate the impact of greenhouse
gas emissions on global warming. Due to efforts to reduce air
pollution, we have recently seen a decrease in 'global dimming',
with improved air qualityimportant for respiratory disordersand
the return of the monsoon. However it is suggested that this might
have the additional consequence of accelerating global warming
yet further.[26]
Adaptation and mitigation
19. There are two main strategies by which the impacts
of climate change can be addressed. Mitigation strategies are
long-term methods by which emissions of greenhouse gases are reduced
to minimise the extent of climate change in the future. Adaptation
strategies acknowledge that a degree of climate change as a result
of past human activity is already inevitable, and employ methodologies
to reduce the predicted impact of climate change. While they are
often discussed independently of one another, both strategies
are complementary. The Tyndall Centre for Climate Research told
us:
Adaptation and mitigation strategies are intimately
linkedthe less emphasis is placed on mitigation, the more
difficult adaptation will be.[27]
20. The Association of British Insurers also argued
that adaptation to climate change needs to take place in parallel
with efforts to mitigate the causes:
We are already locked into a significant degree of
climate change, no matter what we do to reduce emissions of greenhouse
gases. National and international efforts to reduce greenhouse
gases may lessen the degree of climate change in the coming century,
but they will not prevent it completely.[28]
21. The Biosciences Federation argued for further
adaptation measures to predict, cope with and prepare for the
consequences of climate change:
The UK Climate Change Programme should consider more
deeply UK policies for coping and adapting to impending changes
in climate, particularly with regards to impacts on biodiversity
and ecosystems.
The Federation argues that there is likely to be
a substantial impact on biodiversity with large changes in the
structure of natural biological communities.[29]
1 "Climate Change Science: Adapt, Mitigate, or
Ignore?", Science, 9 January 2004 Back
2
Intergovernmental Panel on Climate Change, Third assessment Report,
Climate Change 2001: The Scientific Basis, 2001 Summary
for policymakers pp 2, 7, 10 Back
3
Prime Minister's Speech on climate change, 14 September 2004,
at www.number10.gov.uk/output/page6333.asp Back
4
Defra, Global Atmosphere Research Programme, Annual Report
2002-2003, November 2003, p 5 Back
5
Department of Trade and Industry, Our energy future - creating
a low carbon economy, Cm 5761, February 2003, p 8 Back
6
"Government 'looks to do more' in climate change programme
review", ENDS Report vol 359, December 2004 p 48 Back
7
National Audit Office, Renewable Energy, February 2005 Back
8
Defra, Review of the UK Climate Change Programme, December 2004,
Executive summary Back
9
Defra, The environment in your pocket 2004, October
2004, p 7 Back
10
Defra, Review of the UK Climate Change Programme, Consultation
Paper, December 2004 p 11; IPCC 2001 Back
11
All facts cited were sourced from the Exeter climate change symposium
(see www.stabilisation2005.com/index.html) unless otherwise stated Back
12
Sir David King, The Guardian, 24 November 2004 Back
13
HM Treasury, Government Economic Service Working Paper 140 Estimating
the Social Cost of Carbon, January 2002, p 6 Back
14
IPCC, Climate Change 2001: The scientific basis, 2001 p
527 Back
15
IPCC, Climate Change 2001: The scientific basis, 2001 Back
16
UK health impacts of climate change, POSTnote 232, Parliamentary
Office of Science and Technology, November 2004 Back
17
Sir David King, The Guardian, 24 November 2004 Back
18
ACIA, Impacts of a Warming Arctic: Arctic Climate Impact Assessment,
Cambridge University Press, 2004; Gregory, 2004 from Scientific
symposium 'Avoiding Dangerous Climate Change', Exeter, February
2005 Back
19
House of Lords, Thirtieth Report of the European Union Committee,
Session 2003-04, The EU and Climate Change HL Paper 179-I,
para 11 Back
20
Ev 215 Back
21
Office of Science and Technology, Foresight Report Future Flooding,
2004 Back
22
Prime Minister's Speech on climate change, 14 September 2004,
at www.number10.gov.uk/output/page6333.asp Back
23
Defra, Charting Progress: An integrated assessment of the state
of UK seas, PB 9911, March 2005 Back
24
Scripps Institution of Oceanography press release, 'Scripps researchers
find clear evidence of human-produced warming in the world's oceans',
17 February 2005. The study was presented at the American Association
for the Advancement of Science annual meeting, February 2005. Back
25
Turley et al., 'Reviewing the Impact of Increased Atmospheric
CO2 on Oceanic pH and the Marine Ecosystem', Proceedings
of the International Symposium on Stabilisation of Greenhouse
Gases, Exeter, February 2005 Back
26
BBC2, Horizon Global dimming, January 2005; Stanhill, G.
and Cohen, S. 'Global Dimming: A Review of the Evidence', Agricultural
and Forest Meteorology, 107: 255-278 (2001); Roderick, M.
and Farquhar, G. 'The Cause of Decreased Pan Evaporation Over
the Past 50 Years', Science, 298: 1410-1411 (2002);
U39, para1 Back
27
Ev 18 Back
28
Ev 215 Back
29
Ev 24 Back