| An animated journey through the Earth's climate history |
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| Written by BBC News | ||||
| Thursday, 03 December 2009 | ||||
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As world leaders prepare to meet in Copenhagen to discuss climate change - how did the Earth's climate arrive at its current state and how do scientists delve into the secrets of our planet's past? The layers of ice laid down each year in Antarctica and Greenland store a record of the Earth's climate. Bubbles of air trapped in the ice as it froze can be analysed to give details on temperature at the time it froze, and on atmospheric concentrations of gases. The oldest ice core so far extracted belongs to the European Project for Ice Coring in Antarctica (Epica). It allows scientists to look back 800,000 years. Over time, the Earth's orbit around the Sun varies slightly.
This changes the amount of solar energy reaching the Earth's surface, alternately warming and cooling the planet's surface. In a warming phase, greenhouse gases such as carbon dioxide are released and amplify the warming - increasing the natural greenhouse effect. They are stored again when an ice age starts. So over this period, we see temperature and carbon dioxide concentrations changing in step, in cycles lasting about 100,000 years. About 10,000 years ago, the Earth emerged from its most recent ice age. Agriculture developed, and the extra food supported a growing global population. The last 1,000 years saw development of international trade - and eventually, in the 1700s, the birth of the Industrial Revolution. This ran largely on coal and later, oil. CLIMATE CHANGE GLOSSARYSelect a term from the dropdown:GlossaryAdaptationAnnex I countriesAnnex II countriesAnthropogenic climate changeAosisAR4Atmospheric aerosolsBali action planBali roadmapBaseline for cutsBiofuelBlack carbonBoxer-Kerry billBusiness as usualCap and tradeCarbon capture and storage (CCS)Carbon dioxide (CO2)Carbon dioxide (CO2) equivalentCarbon footprintCarbon intensityCarbon leakageCarbon neutralCarbon offsettingCarbon sequestrationCarbon sinkCertified Emission Reduction (CER)Clean Coal TechnologyClean Development Mechanism (CDM)Climate changeCFCCO2Commitment periodCOP15Country in transitionDangerous climate changeDeforestationEmission Trading Scheme (ETS)EU Burden-sharing agreementFeedback loopFlexible mechanismFossil_fuelsG77Geological sequestrationGlobal average temperatureGlobal energy budgetGlobal dimmingGlobal warmingGlobal Warming Potential (GWP)Greenhouse gases (GHGs)Greenhouse effectHockey stickIPCCJoint implementationKyoto ProtocolLDCsLULUCFMajor Economies Forum on Energy and ClimateMethaneMitigationNairobi work programNatural greenhouse effectNon-annex I countriesOcean acidificationppm (350/450)Per-capita emissionsPre-industrial levels of carbon dioxideREDDRenewable energyStern reviewTechnology transferTipping pointTwenty-twenty-twenty (20-20-20)UNFCCCWaxman-Markey energy billWeather Climate change - A pattern of change affecting global or regional climate as measured by yardsticks such as average temperature and rainfall, or an alteration in frequency of extreme weather conditions. This variation may be caused by both natural processes and human activity. global warming is one aspect of climate change. The human population was also growing, reaching one billion around the start of the 19th Century. By this time, a growing network of weather stations was taking daily measurements of temperature, a record that increases in precision as time goes on. In the 20th Century, fuel use, industry, land clearance and agriculture all increased atmospheric concentrations of CO2 and other greenhouse gases. The temperature curve for the last 100 years shows two distinct periods of warming with an intervening period of cooling around 1940, probably caused by increased industrial emissions of aerosols, tiny particles that reflect sunlight. In the second half of the century, highly accurate measurements, taken initially in Hawaii and Antarctica, proved that carbon dioxide concentrations were steadily rising in a regular manner. Other greenhouse gases such as methane showed similar trends. The Intergovernmental Panel on Climate Change (IPCC) concludes it is more than 90% probable that the warming seen in the second half of the 20th Century is mainly driven by human emissions of greenhouse gases. Sources and resources
The data, for the animation , on temperature and carbon dioxide for the 800,000 year time period is taken from the European Project for Ice Coring in Antarctica, Epica. The data can be downloaded using the link on the right and was complied by Dr Robert Mulvaney of the British Antarctic Survey. For the time period covering the last 1,500 years the CO2 record is from the Law Dome ice core, again in Antarctica. McFarling Meure et al, 2006 is the source. For the past 60 or so years the CO2 source is the readings taken at Mauna Loa by the NOAA. Temperature for the last 1,500 years is taken from Mann, M.E., Zhang, Z., Hughes, M.K., Bradley, R.S., Miller, S.K., Rutherford, S., Proxy-Based Reconstructions of Hemispheric and Global surface temperature Variations over the Past Two Millennia, Proc. Natl. Acad. Sci., 105, 13252-13257, 2008. For the final time period covered, the temperature data is sourced to the Met Office Hadley Centre and to the Climatic Research Unit at the University of East Anglia. The illustration showing the extent of ice cover over North America 20,000 years ago is credited to Ehlers and Gibbard. Population figures are sourced to the US Census Bureau and the UN. Figures on per capita GDP are from Angus Maddison. More information on the Earth's past climate can be found at the NOAA's palaeoclimatology page and from the IPCC's 2007 report. source: http://news.bbc.co.uk/2/hi/in_depth/sci_tech/2009/copenhagen/8393855.stm |
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