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© Crown copyright 2004
Debunking the myths of
Climate Change
Helen Young
Former Lead Presenter
BBC Weather Centre
© Crown copyright 2004
CLIMATE CHANGE:- A HOT TOPIC
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CLIMATE CHANGE:- IN THE MEDIA
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CLIMATE CHANGE:- weather events
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WEATHER and CLIMATE
Weather – instantaneous atmospheric conditions - temperature, rainfall, pressure, wind etc
Climate - the long-term signal derived from individual weather events.
‘Averaged out’ weather over a long period of time.
- Climate scientists normally use a period of 30 years
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WEATHER 1990ish
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WEATHER 2005ish
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CLIMATE CHANGE:- A GLOBAL ISSUE
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SCIENTIFIC COMMUNITIES- IPCC
Recognizing the problem of potential global climate change, the World Meteorological Organization (WMO) and the United Nations Environment Programme (UNEP) established the Intergovernmental Panel on Climate Change (IPCC) in 1988. It is open to all members of the UN and WMO.
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NATURE
The Met Office’s first Super Computer!
1981
Changes in Met Office Computing
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Arrival of NEC SX-6, One of the Worlds Fastest Supercomputers
2003
Changes in Met Office Computing
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Changes in Met Office Computing
Ferranti Mercury - ‘Meteor’ 3000 calculations per second
The ‘Cray twins’ 160,000 million calculations per second
The NEC SX-6 computer installed Exeter 2004, 6 times more powerful
2005, 2 million, million calculations per second
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0
2
4
6
8
10
Numerical Model Accuracy
Area: North Atlantic
New modelintroduced
RM
S M
SLP
New modelintroduced
New modelintroduced
24-hr forecast
48-hr forecast
72-hr forecast
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Myth 1
Our climate has always changed, this is just another natural change and nothing to do with humans.
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Grape vines
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Three Cranes Wharf near Blackfriars in the City
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CLIMATE 1000 - 2000AD Source: IPCC 2000
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How much climate change has there really been?
GLOBAL TEMPERATURES have risen by about 0.7ºC between 1861 and 2003
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Tem
per
atu
re c
han
ge
ºC
1.0
0.5
0.0
-0.51850 1900 1950 2000
observed
model simulation
+
Observed and simulated change
Natural factors
observedmodel simulation
SUN
Sunlightpasses
through the atmosphere..
..and warms the earth.
..most escapes to outer spaceand cools the earth...
Infra-red radiationis given off by the earth...
…but some IR is trapped by some gases in the air, thus reducing the cooling.
THE GREENHOUSE EFFECT
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The most important greenhouse gases are:-
carbon dioxidemethanenitrous oxide hydrofluorocarbons Perfluorocarbonssulphur hexafluoride. These are the gases that are covered by the Kyoto Protocol.
Chlorofluorocarbons (CFCs) and hydrochlorofluorocarbons (HCFCs) are also powerful greenhouse gases but they are being progressively phased out under the Montreal Protocol as they also damage the stratospheric ozone layer.
GREENHOUSE GASES
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HUMAN ACTIVITIES HAVE CHANGED THE ATMOSPHERE
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Current (2005)
CO
2 C
on
cen
trat
ion
(p
pm
v)
Projected (2100)
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Myth 2
Carbon dioxide is not driving our current warming.
Carbon Dioxide only makes up a small part of the atmosphere therefore it cannot be responsible for this
current Global Warming.
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EARTH’S ORBIT
Orbit for Northern Hemisphere
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Current (2007)
CO
2 C
on
cen
trat
ion
(p
pm
v)
Projected levels of atmospheric CO2 during the next 100 years would be higher than at anytime in the last 440,000 yrs
Projected (2100)
CO2 concentrations have risen by over 30% due to human activities
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CO
2 C
on
cen
trat
ion
(p
pm
v)
Projected levels of atmospheric CO2 during the next 100 years would be higher than at anytime in the last 440,000 yrs
Projected (2100)
CO2 concentrations have risen by over 30% due to human activities
Current (2005)
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Observed and simulated change
Natural & man-made factors
Tem
per
atu
re c
han
ge
ºC
1.0
0.5
0.0
-0.51850 1900 1950 2000
observed
model simulation
+
+
observedmodel simulation
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RELATIVE WARMING OF GREENHOUSE GASES current emissions, effect over next 100 years
Methane24%
Carbondioxide
63%Nitrous
oxide 10%
Others3%
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ATMOSPHERIC CONSTITUENTS which affect climate; sources and lifetimes
Carbon dioxide Fossil fuels, deforestation 100 years
Methane Agriculture, natural gas 10 years
Other gases
(nitrous oxide, CFCs, ground-level ozone..)
Aerosols Power generation, transport 2 weeks
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CARBON DIOXIDE (CO2)
The most important man-made greenhouse gas
About half of the CO2 emitted by Man remains in the
atmosphere; remainder absorbed by vegetation and
oceans
CO2 risen by 1/3 since the industrial revolution
CO2 emissions would have to be reduced by about 70%
to stabilise climate change
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Myth 3
Computer models are unreliable.
How can you predict 100 years ahead when you can’t predict the weather for the next 5 days?
THE CLIMATE SYSTEM
OCEAN
PrecipitationSea-ice
LAND
Ice- sheetssnow
Biomass
Clouds
Solarradiation
Terrestrialradiation
Greenhouse gases and aerosol
ATMOSPHERE
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ATMOSPHEREATMOSPHERE LANDLAND OCEANOCEAN ICEICE SULPHURSULPHUR CARBON CARBON CHEMISTRYCHEMISTRY
ATMOSPHEREATMOSPHERE LANDLAND OCEANOCEAN ICEICE SULPHURSULPHUR CARBON CARBON
ATMOSPHEREATMOSPHERE LANDLAND OCEANOCEAN ICEICE SULPHURSULPHUR
ATMOSPHEREATMOSPHERE LANDLAND OCEANOCEAN ICEICE
ATMOSPHEREATMOSPHERE LANDLAND OCEANOCEAN
ATMOSPHEREATMOSPHERE LANDLAND
ATMOSPHEREATMOSPHERE
19991999
19971997
19921992
19851985
Development of Hadley Centre Climate Models
1960s1960s
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Projections of Climate Change
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Model Projections – Global temperature riseG
lob
al t
emp
erat
ure
ris
e, d
egre
es C
High emissionsMedium-high emissionsMedium-low emissionsLow emissions
Start to diverge from mid-century
Other climatemodels:1.5 - 6°C
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Myth 4
It’s all to do with the sun-
There’s a strong link between increasing temperatures on earth and the number of sunspots on the sun.
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Solar influence
Temperature anomaly relative to late 19 th century.
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1374
1372
1370
1368
1850 1900 1950 2000
So
lar
rad
iati
on
/
W m
–2
CHANGES IN SOLAR ENERGYGJJ1999
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Myth 6
The NAD will be cut off and we’ll be heading for another ice age
GLOBAL OCEAN CIRCULATION
COOLING
WARMSURFACECURRENT
INTERMEDIATEWATERS
WARM AND LESS SALINE ANTARCTIC CIRCUMPOLAR CURRENT
GJ J1999
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The Gulf Stream
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NORTH ATLANTIC OCEAN CIRCULATIONC
ircu
lati
on
str
en
gth
No changeSRES A1FISRES B2SRES B1SRES A2
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The Day After Tomorrow? Very unlikely!
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Myth 5
Everyone jumps on the negative effects of Climate Change there’s no need for urgent action.
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Global-average temperature and sea level are projected to rise under all scenarios
Global-average surface temperature projected to increase by 1.4 ºC (~2.5 °F) to 5.8 ºC (~10.5 °F) by 2100 Rate of warming likely unprecedented in at least last 10,000 yrs Land areas will warm more than the global average
Global average precipitation will increase over 21st century
Very likely to be more intense precipitation events
Snow cover and sea-ice extent projected to decrease further
Glaciers and icecaps projected to continue widespread retreat
Global mean sea-level projected to increase by 9 cm (~3.5 in) to 88 cm (~34.5 in) by 2100
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COASTAL POPULATIONS AT RISKChange from the present day to the 2080s
University of Middlesex
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Coastal flooding from sea-level rise
River flooding from more heavy rain events
Health risks
Water supply threatened by droughts
Increased storminess?
IMPACTS ON THE UK
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HOW QUICKLY WILL THE CLIMATE CHANGE IN FUTURE
Depends on…………
How much greenhouse gas emissions grow this depends on population growth, energy use, new
technologies, etc
How sensitive the climate system is to emissionshow clouds, ice, oceans etc respond to the extra heating;
we build a mathematical model of the earth’s climate system to calculate this
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WHAT CAN BE DONE?
Adaptationcoping with the effects of climate change
Mitigationreducing emissions of greenhouse gasessoaking up CO2 by forests, etcreducing sensitivities
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•Turn off lights when you leave a room •Only boil the amount of water you need in your kettle •Turn off televisions, videos, stereos and computers when they are not in use - they can use between 10 and 60% of the power they use when on •Don't leave fridge doors open for longer than necessary, let food cool down fully before putting in the fridge or freezer, defrost regularly and keep at the right temperature •Close curtains at dusk to keep in heat •Let your clothes dry naturally rather than using a tumble drier •Turning down the thermostat for your heating by 1 degree could cut your heating bill by 10% •Set your water thermostat for 60 degrees - this is plenty warm enough for bathing and washing and will save money too •Use economy programmes on dishwashers or washing machines •Where possible don't stand cookers and fridges/freezers next to each other
Things you can do today at no cost:
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Things you could do in the future
•Put foil behind radiators fitted on external walls •Use energy saving lightbulbs - they use a quarter of the electricity and last much longer •Insulate your hot water tank and pipes •Speak to your energy provider about their 'green tariff' - they may be able to match your energy consumption with an equivalent amount of energy from renewable sources •Fit seals to externals doors, skirting boards and floor boards to reduce heat loss - 15% of heat is lost through draughts and 15% through the floor •Make your windows draught proof or fit double glazing - this cuts heat loss in half - up to 10% of heat is lost through uninsulated windows•Fit loft insulation - which should be at least 200mm thick to be most effective - 25% of heat is lost through an uninsulated roof •Fit wall insulation - up to 33% of heat is lost through uninsulated walls •Replace old inefficient boilers •Fit solar panels or solar tiles to your roof
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Links: www.metoffice.gov.ukwww.bbc.co.uk/climate
www.royalsoc.ac.ukwww.ipcc.ch