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Your energy our future |
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Climate change is a real issue we can all help to resolve! |
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The exchange of 'man-made' carbon dioxide between man-made emissions, atmosphere, ocean and land, is about 7 GtC/year (billion tons of carbon, in the form of carbon dioxide, per year), which also shows much larger natural exchanges between atmosphere and ocean (about 90 GtC/yr) and atmosphere and land (about 60 GtC/yr). However, these natural exchanges have been in balance for many thousands of years, leading to the pre-industrial concentration of CO2 remaining steady at about 280 ppm. |
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Global Warming |
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§ Coastal flooding special report |
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1. Climate Change: the world in 2055 2. Natural phenomena captured from space |
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Climate Change is a real problem - Global Warming - useful links Global Warming hot map of the World
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Climate projections Because we can't know the future for certain, our climate change scientists use computer-based climate models to project plausible scenarios, or projections, for coming centuries. It is important to be aware that projections from climate models are always subject to uncertainty because of limitations on our knowledge of how the climate system works and on the computing resources available. Different climate models can give different projections. The projections are also based on emissions scenarios, such as the level of CO2 emissions increasing or decreasing. Many different scenarios are used, based on estimates of economic and social growth, and this is one of the major sources of uncertainty in climate prediction. But even if greenhouse gas emissions are substantially reduced, the long lifespan of CO2 in the atmosphere means that we cannot avoid further climate change due to CO2 already in the atmosphere. Despite the uncertainties, all models show that the Earth will warm in the next century, with a consistent geographical pattern. Some of the diagrams below are maps of differences between the current climate, conventionally defined as 1960-1990, and the climate of the end of the 21st century, taken to be 2070-2100. For most quantities, changes are shown both for the annual average and for each of the four seasons December-February (Winter), March-May (Spring), June-August (Summer) and September-November (Autumn). The other diagrams are time-series, showing changes which occur as time passes. |
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What can climate scientists tell us about the future? Dr Vicky Pope Like any 'expert' trying to project into the future, scientists cannot give precise predictions of what will happen in 100 years, or even in the next 10 years. However, we are able to give a range of possible outcomes of the world's actions and to assign probabilities to these, and climate projections should be treated as an assessment of risk. You wouldn't drive a car if you knew you had a 10% chance of causing an accident. Yet we continue to increase emissions, despite the fact that even if we could stabilise greenhouse gases at, or close to, today's levels there would still be only a 80% chance of keeping global temperature rises somewhere between 2 and 3 °C above pre-industrial levels. If we carry on increasing emissions at present rates then global average temperature rise will be 2 °C by the middle of this century. The difficulty is that the projections do not agree on how big the changes will be. Over the next few years, better models and the use of multiple model techniques should help us to understand and reduce the uncertainties in our predictions.
Impacts our models are already predicting for Europe and the UK Average European rainfall. In northern Europe (including UK) average summer rainfall for 2070-2100 is likely to decrease by between 5 and 20%. Average winter rainfall is very likely to increase. The number and intensity of extreme rainfall events will increase in winter. Summer floods in the UK Heatwaves
Global impacts our models are already predicting
Drought
Amazon rainforest
Greenland ice sheet
Tackling the science Climate scientists tend to gravitate towards two approaches when it comes to describing their projections of climate change. All scientists are trained to consider all the possible problems with their results and will always point out the caveats and areas that could be improved. This can give rise to a very confused view of what results mean and leads the public dismissing to some results as too uncertain. Some scientists react against this by taking the most pessimistic view of what the future holds, to try to make it clear how serious the problem is. These results tend to be dismissed as unrealistic. By quantifying the risks of climate change, the Met Office Hadley Centre hopes to give a balanced view of the future and provide useful information that can be used to make important decisions about all our futures. There is already a very large body of evidence that can be used to make decisions about climate change. The strengths and weaknesses of this evidence have been tested and are understood. Climate scientists use evidence from observations of the past climate, and from computer models of the climate, to produce projections of the future. Projections are made using climate models derived from the laws of physics. A well-established set of equations result from the physical laws governing the climate and these are solved for a three-dimensional grid that spans the globe. The observations are then used to make an independent check on whether the models are good enough. The accuracy of the results depends on a detailed understanding of the physical processes and the fineness of the grid that can be represented on the computer being used. Climate models currently have a grid spacing of 150 km, and this is likely to improve to 90 km with the next generation of models. A finer grid means more detail and more accuracy. The grid spacing and the science are the two aspects that are being continually improved, and the reason why scientists will always place caveats on their projections.
Analysing the risks of climate change In order to generate the full range of possible futures, scientists generate model projections that take account of uncertainties in the following:
AdaptationIf we plan ahead, we should be able to adapt to some aspects of climate change, provided that change is not too great or occurs too quickly. If emissions continue to grow at present rates, the changes will be so large and so rapid that the adverse effects will quickly outweigh any local benefits and come to dominate in all regions of the world. Adaptation will also become increasingly difficult, and in some cases impossible. We also need to consider that the UK does not exist in isolation, but is affected by what happens elsewhere. For example, world food prices and migration are already significant issues today and will be adversely affected by global warming. About Dr Vicky Pope
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Urgency of Climate Change |
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