abil- fh?rl. . .03 nz?mg SEAN: Q03 mym: 33? Q0 $55 an CONTENTS CLIMATE CHANGE - WHAT IS 2 A CAUSE FOR CONCERN 3 WHAT SHELL THINKS ABOUT CLIMATE CHANGE AND WHY 4 WHAT SHAPES OUR THINKING 5 ROLE OF GOVERNMENT 7 WHAT IS SHELL DOING ABOUT CLIMATE 8 REDUCING EMISSIONS OF GREENHOUSE GASES IO Each of the companies within the Royal Dutch/Shell Group of companies is a separate and distinct entity. in this report, the expressions Group and Royal Dutch/Shell Group are used to refer to the companies of the Royal Dutch/Shell Group as a Whole. The words ?She/i?, ?We? and ?us? are used in some places to refer to the Group and in others to an individual She/l company or companies Where no useful purpose is served by identifying it or one of them more particularly. CLIMATE CHANGE -WHAT IS Some solar radiation is reflected by the earth and the atmosphere Solar radiation passes through the clear atmosphere . Most radiation is absorbed by the EARTH earth's surface and warms it ases present in the atmosphere, such as water vapour, carbon dioxide and methane, keep the earth warmer than it would otherwise be by acting as an insulating blanket and trapping some of the sun?s rays - the natural ?greenhouse effect?. The burning of fossil fuels such as coal, oil and natural gas, together with other human activities such as deforestation, releases greenhouse gases, especially carbon dioxide (C02) into the air. Their concentration in the atmosphere has been rising since the industrial revolution. This has led ATMOSPHERE Infra-red radiation is emitted from the earth's surface to an increase in the greenhouse effect. There is concern that an enhanced greenhouse effect will cause the world to warm up. This could cause a change in climate and local weather patterns, possibly with increased droughts, floods, storms and sea level rise. The average temperature of the earth has risen by about half a degree Celsius over the last century, possibly due in part to human greenhouse gas emissions. Some of the infra?red radiation is absorbed and re-emitted by the greenhouse gases. The effect of this is to warm the surface and the lower atmosphere WHAT THE WORLD HAS DECIDED TO DO. ost of the world?s nations were sufficiently concerned to sign a United Nations agreement, the Framework Convention on Climate Change in 1992. Industrial countries agreed to reduce emissions of greenhouse gases to the' level they were in 1990, by the year 2000. Very few countries will meet this target. At a conference in Kyoto (December 1997), stronger commitments under the Convention were agreed. Rich countries will be legally bound to reduce their greenhouse gas emissions by at least 5% on average relative to 1990 levels by the years 2008 to 2012. This is the first real step in what will likely be a series of further international negotiations to tackle the issue globally. Combined global land and sea surface temperatures A CAUSE FOR ONC ERN 1860?1997 (relative to 1961?90 average) 0.50 0.40 trend 3 0.30? The temperature of the Earth has 0 20_ . . . 0 been rISIng over the last century. 010? II 8 'tlill'vnll II The causes are not clear but TE 030? I. I II I I 040? II I Atmospheric carbon dioxide concentrations and fossil fuel emissions '0-50 - 380 ?0'60 I I I I 1840 1860 1880 1900 1920 1940 1960 1980 2000 A 360 6 emISSIons of greenhouse gases, 5 - 4 555) especially carbon dioxide, from 340 - 2 human activities have caused their 0 . . - 53 8: concentrations In the atmosphere Increase. I I I I I 1850 1900 1950 2000 ii 300 Year 0 280 . . Atmospheric carbon diox1de concentrations and 260 global temperatures over the last 150 thousand years 800 1000 1200 1400 1600 1800 2000 Projection Year Present We don?t know what the 360