Bangladesh Floods:20 Million people are at Risk

New research shows a bleak future for Bangladesh, claiming up to 20 million people are at risk from rising sea levels and monsoon floods.

The research by the Centre for Environmental and Geographic Information Services in Bangladesh predicts that sea water could reach far inland, as many rivers are surrounded by low lying flood plains. As well as displacing those living in these areas, it would make it hard to cultivate such basic foods as rice.

The research comes as the Bangladesh Government appeals for £3 billion in aid over the next five years to combat climate change in the region. The study suggest that a surprisingly small amount of land will be permanently lost to rising sea levels, but perhaps the bigger threat is repeated Bangladesh floods every monsoon season, especially in the south west region.

A senior scientist on the study claims sea water could cause havoc for rice production in Bangladesh’s poorest regions.

“These are very poor people, and vulnerable. For four months they’ll have nowhere to work, So people will migrate to the cities for jobs, because of the uncomfortable situation with sea level rise. We are talking about 20 million people.”

According to Bangladesh monitoring stations, there has been an average of 5mm sea level rise per year for the past 30 years. Nearly half of the rice produced in Bangladesh is so call “monsoon” rice, much of which is grown in the areas most vulnerable to Bangladesh floods.

Bangladesh has been listed as one of the countries vulnerable to “extreme risk” from climate change over the next 100 years.

What is climate change?

Climate change can be defined as “statistically significant variation in either the mean state of the climate or in its variability, persisting for an extended period (Houghton et al, 2001)”. It is extremely important to define what can be labelled as climate change, and what cannot. 

The United Nations Framework Convention on Climate (UNFCC) states that climate change is variation in the climate, which can be attributed to human activity, either directly or indirectly, and stresses that it must be in addition to natural variation being experienced during the same time period. It is essential to distinguish between “climate change” due to human activities and “climate variability” due to natural causes. Only when we have a comprehensive understanding of these factors can we understand what effect humans are having on the composition of the atmosphere (UNFCC, 2002).

The potential problem of global warming was officially recognised in 1988 when the World Meteorological Organization (WMO) and the United Nations Environment Programme (UNEP) established the Intergovernmental Panel on Climate Change (IPCC). 

The IPCC was created with the intention of being an objective assessor of peer reviewed published scientific literature. It’s fundamental objective to provide a comprehensive, and impartial view, regarding the science and potential impact of climate change due to anthropogenic factors, then to use this information to look at options for potential adaptation and mitigation. This lead to the creation of the United Nation Framework Convention on Climate Change (UNFCCC) in 1992, a result of the first IPCC Assessment Report, which was completed in 1990. 

The second IPCC assessment was published in 1995, and provided the basis for the Kyoto Agreement, which aims to reduce carbon dioxide emissions. A third IPCC report was completed in 2001, providing a comprehensive source of reference, which has been used internationally as the basis for the science and impact of global climate change. A fourth report is planned for 2007, and its scope and outline are currently under discussion (http://www.ipcc.ch).

 

Climate change is one of the most serious environmental challenges facing the world. Call for action. The need to address climate change is urgent.  

Climate change is a change or variability in the average weather of a region. It may be a positive change in some locations which may enhance the productivity of a region, however, the rapidity of the change will cause major disruption and there will be many more losers than gains if climate change advances as predicted and as initial indications are now beginning to show.

To become fully engaged with the issue of climate change, it is important to understand the science. Understanding how the circulation of the Earth's carbon atoms drives climate change. Climate change is caused by the persistent build-up of greenhouse gases such as Carbon Dioxide (CO2) in the Earth's atmosphere. Climate change will also alter the availability of freshwater and potable water resources. There are a handful of other, mainly industrial, chemicals that also contribute to climate change. The scientific opinion on climate change at the moment is that 'the warming that has occurred in the past 50 years can be directly attributed to anthropogenic emissions.  

Many people confuse the hole in the ozone layer with climate change. In fact, the hole in the ozone layer, which is now beginning to mend itself due to the efforts, and agreements, made worldwide for industry to limit and reduce ozone depleting emissions, has nothing to do with climate change.

The Kyoto Protocol is the international plan to reduce climate change pollution. But climate change is about much more than perceptions of scientific certainty or uncertainty.

For example, water vapor is not typically considered part of the climate change problem, although larger amounts of water vapour are known to be present now than in the past, and this will also have an effect on climate.  

Climate change is a change in the 'average weather' that a given region experiences, and average weather changes will be unevenly dispersed around the world, with some places experiencing much greater rises than others. Climate change in the Arctic will be greater than in most other regions, and is expected to move the permafrost boundary north by several hundred kilometers.  

The issue of climate change is closely linked to other environmental issues, and to the challenge of sustainable development itself. The impacts of climate change once thought of as unimaginable and farfetched are now occurring. Climate change, sometimes called “global warming”, is the most serious and most complex environmental issue ever to confront the international community.  

Climate change isn't a problem for the future, it's affecting people around the world today. A vast amount of research has been done on climate change, its causes and implications. Many positive feedbacks also exist where the effects of climate change accelerate global warming. However, developing countries in particular are becoming more and more concerned about how climate change will affect them, and they do not possess the wealth to protect their populations from the effects of natural disasters such as flooding.  

Read on throughout this web site for more information on climate change, and how you can be part of the solution.

Top Ten Things You Need to Know about Global Warming

There are a number of widely held misconceptions about climate change, and unfortunately, these are reflected in some of the educational materials available on the web. It is therefore crucial for teachers to educate themselves and their students with accurate information and be careful not to reinforce common but incorrect notions. The following primer is a good place to begin.
#1 Global warming is caused primarily by carbon dioxide from burning coal, oil and gas.
Certain gases that trap heat are building up in Earth's atmosphere. The primary culprit is carbon dioxide, released from burning coal, oil and natural gas in power plants, cars, factories, etc. (and to a lesser extent when forests are cleared). The second is methane, released from rice paddies, both ends of cows, rotting garbage in landfills, mining operations, and gas pipelines. Third are chlorofluorocarbons (CFCs) and similar chemicals, which are also implicated in the separate problem of ozone depletion (see #5 below). Nitrous oxide (from fertilizers and other chemicals) is fourth.


#2 Earth's average temperature has risen about 1 degree F in the past 100 years and is projected to rise another 3 to 10 degrees F in the next 100 years.
While Earth's climate has changed naturally throughout time, the current rate of change due to human activity is unprecedented during at least the last 10,000 years. The projected range of temperature rise is wide because it includes a variety of possible future conditions, such as whether or not we control greenhouse gas emissions and different ways the climate system might respond. Temperatures over the US are expected to rise more than over the globe as a whole because land areas closer to the poles are projected to warm faster than those nearer the equator.

#3 There is scientific consensus that global warming is real, is caused by human activities, and presents serious challenges.
Scientists working on this issue report that the observed global warming cannot be explained by natural variations such as changes in the sun's output or volcanic eruptions. The most authoritative source of information is the UN Intergovernmental Panel on Climate Change (IPCC) which draws upon the collective wisdom of many hundreds of scientists from around the world. The IPCC projects global temperature increases of 3 to 10 degrees F in the next 100 years and says that human activity is the cause of most of the observed and projected warming.

#4 There's a difference between weather and climate.
Weather refers to the conditions at one particular time and place, and can change from hour to hour, day to day, and season to season. Climate, on the other hand, refers to the long-term average pattern of weather in a place. For example, we might say that the climate of South Florida is warm, moist and sunny, although the weather on a particular day could be quite different than that. Long-term data are needed to determine changes in climate, and such data indicate that Earth's climate has been warming at a rapid rate since the start of intensive use of coal and oil in the late 1800s.

#5 The ozone hole does not cause global warming.
Ozone depletion is a different problem, caused mainly by CFCs (like Freon) once used in refrigerators and air conditioners. In the past, CFCs were also used in aerosol spray cans, but that use was banned in the US in 1978. CFCs deplete the stratospheric ozone layer that protects life on Earth from excess ultraviolet light that can cause skin cancer and cataracts in humans and other damage to plants and animals. An international agreement has phased out most uses of CFCs but the ozone layer is only just beginning to recover, partly because these chemicals remain in the atmosphere for a long time. (Although ozone depletion is not the cause of global warming, there are a number of connections between the two. For example, many ozone-depleting compounds are also greenhouse gases. Some of the compounds now replacing CFCs in order to protect ozone are also greenhouse gases. And ozone itself is a greenhouse gas. In addition, while greenhouse gas build-up causes temperatures close to Earth's surface to rise, it cause temperatures higher up, in the stratosphere, to fall. This stratospheric cooling speeds ozone depletion, delaying the recovery of the ozone hole.)

#6 Global warming will have significant impacts on people and nature.
As temperatures continue to rise, precipitation is projected to come more frequently in the form of heavy downpours. We can probably expect more extreme wet and dry conditions. In the western US, where snowpack provides free storage of most of the water supply, reduced snowpack will make less water available in summer. Coastal areas will become more vulnerable to storm surges as sea level rises. Plant and animal species will migrate or disappear in response to changes in climate; New England may lose its lobsters and maple trees as they move north into Canada. Natural ecosystems such as coral reefs, mangrove swamps, arctic tundra, and alpine meadows are especially vulnerable and may disappear entirely in some areas. While global warming will have impacts on natural and human systems all around the world, the largest impacts will be on many natural ecosystems and on people who live in developing countries and have few resources and little ability to adapt. On the positive side, warmer winters will reduce cold-related stresses and growing seasons will lengthen. And there will be tradeoffs in some areas, such as less skiing but more hiking; and fewer killing frosts but more bugs.

#7 Sea level has already risen due to warming and is projected to rise much more.
Many people are under the mistaken impression that only if the polar ice caps melt will sea level rise. In fact, average sea level around the world has already risen 4 to 8 inches in the past 100 years due to global warming and is expected to rise another 4 to 35 inches (with a best guess of around 19 inches) by 2100. The primary reason for this rise is that water expands as it warms. The second reason is that glaciers all over the world are melting, and when land-based ice melts, the water runs to the sea and increases its level. Thousands of small islands are threatened by the projected sea-level rise for the 21st century, as are low-lying coastal areas such as southern Florida. Of course, if there is any significant melting of the polar ice sheets, the additional rise in sea level would be enormous (measured in feet not inches). This is projected to occur on a time scale of millennia rather than centuries.

#8 Saving energy and developing alternative energy sources would help.
Each of us can reduce our contribution to global warming by using less greenhouse-gas-producing energy: driving less, choosing fuel efficient cars and appliances (like refrigerators and water heaters), and using solar energy where feasible for water and space heat. We can encourage our political and business leaders to institute policies that will save energy and develop alternative energy sources that do not release carbon dioxide. We can preserve existing forests and plant new ones. But even if we take aggressive action now, we cannot completely prevent climate change because once carbon dioxide is in the atmosphere, it remains there for about a century, and the climate system takes a long time to respond to changes. But our actions now and in the coming decades will have enormous implications for future generations.

#9 An international agreement known as the Kyoto Protocol has been negotiated to reduce greenhouse gas emissions, but the US is not participating in it.
Because of its high energy consumption, the US has long emitted more carbon dioxide than any other country. Because carbon dioxide remains in the atmosphere for about 120 years, it accumulates, becomes equally distributed around the world, and has global effects. Thus, while using large amounts of energy to achieve economic growth, the US and other wealthy nations have unintentionally burdened the rest of the world with a long-term problem. And many negative impacts of climate change are likely to be more severe for poorer countries that lack the resources to adapt. The US has more technological and financial resources than other nations. The role of the US in reducing its own emissions and sharing its technologies with other nations will thus be critical to the success of international efforts to limit climate change. Meanwhile, we do not have to wait for the government to take action. Some companies, governments and individuals have already committed to reducing their emissions of greenhouse gases without laws or treaties requiring them to do so.

#10 Protecting the world's climate by stabilizing atmospheric concentrations of greenhouse gases will require enormous reductions in current emissions.
Even if ratified, the Kyoto Protocol in its present form is only a start and would not be nearly enough to stabilize climate. It is estimated that greenhouse gas emissions would have to be reduced to less than one third of current levels to stabilize atmospheric concentrations. This would require a major transformation of the energy sector. A mix of new and existing energy technologies will be needed to achieve this, including large increases in energy efficiency and renewable energy. Researchers are also developing technology to capture and bury carbon dioxide thousands of feet underground. Major increases in public and private research and development are needed to make the necessary technologies available as rapidly and economically as possible.

Carbon Dioxide (CO2)

Carbon Dioxide (CO2) is a colorless, odorless non-flammable gas and is the most prominent Greenhouse gas in Earth's atmosphere. It is recycled through the atmosphere by the process photosynthesis, which makes human life possible. Photosynthesis is the process of green plants and other organisms transforming light energy into chemical energy. Light Energy is trapped and used to convert carbon dioxide, water, and other minerals into oxygen and energy rich organic compounds. (Encyclopaedia Britannica Volume 25) Carbon Dioxide is emitted into the air as humans exhale, burn fossil fuels for energy, and deforest the planet. Every year humans add over 30 billion tons of carbon dioxide in the atmosphere by these processes, and it is up thirty percent since 1750 (www.envirolink.org/orgs/edf/sitemap.html). An isolated test at Mauna Loa in Hawaii revealed more than a 12% (316 ppm in 1959 to 360 ppm in 1996) increase in mean annual concentration of carbon dioxide. Mauna Loa, located in Hawaii, is the worlds largest volcano at 40,000 cubic km and 4,170 meters above sea level. (Encyclopedia Britannica Volume 27) . Ice core samples have also shown a dramatic increase in carbon dioxide levels. Drilling deep into glaciers and polar ice caps and taking out samples of ice, then melting the ice and capturing the gas has shown an increase in carbon dioxide concentrations over the past 100 years. Ice core samples are essentially "drilling through time", because the deeper the ice is, the older the ice is.
In 1996, carbon dioxide world emissions increased by 2.8%. The U.S. reported a 3.3% increase in CO2
concentrations. The U.S. continues to emit more than any other country in the world, accounting for 25% of all emissions. The European Union had an increase of 2.2%, much larger than a small increase of 1.1% in 1995. Eastern Europe had a decreasing rate of -2.4%. China's increase in 1996 was 4.7%.(http://infoweb.magi.com/~dwalsh/wfsesr.html)
Fossil Fuels were created chiefly by the decay of plants from millions of years ago. We use coal, oil and natural gas to generate electricity, heat our homes, power our factories and run our cars. These fossil fuels contain carbon, and when they are burned, they combine with oxygen, forming carbon dioxide. The two atoms of oxygen add to the total weight. The World Energy Council reported that global carbon dioxide emissions from buring fossil fuels rose 12% between 1990 and 1995. (www.eb.com:180) The increase from developing countries was three times that from developed countries. Middle East carbon dioxide emissions from burning of fossil fuels increased 35%, Africa increased 12%, and Eastern Europe increased rates by 75% from 1990-1995.
Deforestation is another main producer of carbon dioxide. The causes of deforestation are logging for lumber, pulpwood, and fuel wood. Also contributing to deforestation are clearing new land for farming and pastures used for animals such as cows. Forests and wooded areas are natural carbon sinks. This means that as trees absorb carbon dioxide, and release oxygen, carbon is being put into trees. This process occurs naturally by photosynthesis, which occurs less and less as we cut and burn down trees. As the abundance of trees declines, less carbon dioxide can be recycled. As we burn them down, carbon is released into the air and the carbon bonds with oxygen to form carbon dioxide, adding to the greenhouse effect. About 860 acres, the size of Central Park in New York, is destroyed every 15 minutes in the tropics.

The Greenhouse Effect


The "greenhouse effect" is the heating of the Earth due to the presence of greenhouse gases. It is named this way because of a similar effect produced by the glass panes of a greenhouse. Shorter-wavelength solar radiation from the sun passes through Earth's atmosphere, then is absorbed by the surface of the Earth, causing it to warm. Part of the absorbed energy is then reradiated back to the atmosphere as long wave infared radiation. Little of this long wave radiation escapes back into space; the radiation cannot pass through the greenhouse gases in the atmosphere. The greenhouse gases selectively transmit the infared waves, trapping some and allowing some to pass through into space. The greenhouse gases absorb these waves and reemits the waves downward, causing the lower atmosphere to warm.(www.eb.com:180)

What are Greenhouse Gases?


Many greenhouse gases occur naturally, such as water vapor, carbon dioxide, methane, nitrous oxide, and ozone. Others such as hydrofluorocarbons (HFCs), perfluorocarbons (PFCs), and sulfur hexafluoride (SF6) result exclusively from human industrial processes.

Human Activities and Greenhouse Gases

Human Activities also add significantly to the level of naturally occurring greenhouse gases:

  • Carbon dioxide is released into the atmosphere by the burning of solid waste, wood and wood products, and fossil fuels (oil, natural gas, and coal).
  • Nitrous oxide emissions occur during various agricultural and industrial processes, and when solid waste or fossil fuels are burned.
  • Methane is emitted when organic waste decomposes, whether in landfills or in connection with livestock farming. Methane emissions also occur during the production and transport of fossil fuels.

National and International Programs :

  • Atmosphere, Climate & Environment Information Programme
    (Disseminates information, effects of, and controls on air pollution and climate change, within the framework of national legislation and international discussion.)
  • Carbon Sequestration Web site
    (Offers information on carbon management efforts supported by the DOE Office of Science.)
  • Climate Change Information Kit
    (Detailed summary of climate change issues from the United Nations Environment Programme's Information Unit for Conventions.)
  • Climate Prediction Center at NOAA's National Centers for Environmental Prediction
    (The Center's mission is to maintain a continuous watch on short-term climate fluctuations and to diagnose and predict them.)
  • Climate Research Division in the United Kingdom
    (Comprehensive climate links for the UK Meteorological Office's Hadley Center for Climate Prediction and Research.)
  • Climate Resources page of NOAA's National Climatic Data Center
    (Expert and authoritative source for many types of climate data and documentation.)
  • Common Questions About Climate Change
    (Compiled by the United Nations Environment Programme and the World Meteorological Organization.)
  • Encyclopedia of Sustainable Development
    (A one-stop source of information on sustainable development.)
  • Encyclopedia of the Atmospheric Environment
    (A one-stop source of information on a range of atmospheric issues, including air quality, acid rain, global warming and ozone depletionsustainable development.)
  • Environment Canada's Global Climate Change Site
    (Informative and entertaining site; especially good for educators and students.)
  • Global Change Data and Information Service
    (A collection of distributed information systems operated by agencies participating in the U.S. Global Change Research Program.)
  • GREENGRASS
    (Offers information on sources and sinks of greenhouse gases from managed European grasslands and mitigation strategies.)
  • Intergovernmental Panel on Climate Change
    (The IPCC was formed by the World Meteorological Organization and the United Nations Environment Programme in 1988 and is the vehicle through which scientists around the world are working jointly on climate change assessments.)
  • NASA's Land Cover Land Use Change Program
    (An interdisciplinary programme aimed at improving the understanding of land use and land cover change dynamics and their relationships with global environmental change.)
  • NOAA-CIRES Climate Diagnostics Center
    (Focuses on advancing our understanding of and ability to predict climate variability. A great ENSO site.)
  • Regional and Global Data for Global Change Research from ORNL DAAC
    (Comprehensive metadata database of data and models on the biogeochemical dynamics of terrestrial ecosystems. Metadata contain links to data and models held by other data centers.)
  • Synthesis and Upscaling of Sea-level Rise Vulnerability Assessment Studies (SURVAS)
    (To enhance the understanding of the implications of sea-level rise at the regional and global scale.)
  • U.S. Environmental Protection Agency Global Warming Site
    (EPA's site describes the climate system, climate change impacts, and actions being taken from the global level down to the local level.)
  • U.S. Global Change Research Program (USGCRP)
    (Umbrella agency site covers anything having to do with U.S. government climate change research. A great source for 100s of additional links.)
  • World Bank Group
    (Provides loans, policy advice, technical assistance, and knowledge-sharing services in assistance to developing economies.)
  • World Data Centre for Greenhouse Gases
    (Collects, archives, and provides greenhouse gas data and data from related gases in the atmosphere and ocean that are measured under the Global Atmosphere Watch (GAW) programme.)
  • What is Global warming ?

    Global warming -- a gradual increase in planet-wide temperatures -- is now well documented and accepted by scientists as fact. A panel convened by the U.S National Research Council, the nation's premier science policy body, in June 2006 voiced a "high level of confidence" that Earth is the hottest it has been in at least 400 years, and possibly even the last 2,000 years. Studies indicate that the average global surface temperature has increased by approximately 0.5-1.0°F (0.3-0.6°C) over the last century. This is the largest increase in surface temperature in the last 1,000 years and scientists are predicting an even greater increase over this century. This warming is largely attributed to the increase of greenhouse gases (primarily carbon dioxide and methane) in the Earth's upper atmosphere caused by human burning of fossil fuels, industrial, farming, and deforestation activities.

    Average global temperatures may increase by 1.4-5.8ºC (that's 2.5 - 10.4º F) by the end of the 21st century. Although the numbers sound small, they can trigger significant changes in climate. (The difference between global temperatures during an Ice Age and an ice-free period is only about 5ºC.) Besides resulting in more hot days, many scientists believe an increase in temperatures may lead to changes in precipitation and weather patterns. Warmer ocean water may result in more intense and frequent tropical storms and hurricanes. Sea levels are also expected to increase by 0.09 - 0.88 m. in the next century, mainly from melting glaciers and expanding seawater . Global warming may also affect wildlife and species that cannot survive in warmer environments may become extinct. Finally, human health is also at stake, as global warming may result in the spreading of certain diseases such as malaria, the flooding of major cities, a greater risk of heat stroke for individuals, and poor air quality.

    Climate change is very likely having an impact now on our planet and its life, according to the latest installment of a report published by the Intergovernmental Panel on Climate Change (IPCC). And the future problems caused by rising seas, growing deserts, and more frequent droughts all look set to affect the developing world more than rich countries, they add. The report is the second chapter of the IPCC's Fourth Assessment -- the most comprehensive summary yet of research into the causes and effects of climate change

    Why does the climate change ?

    The global mean climate changes because the amount of net energy that enters the climate system changes in time. The Earth receives energy from the sun. Part of this energy is transformed into heat. The total amount of solar energy that is transformed into heat is not always the same because:

    • The amount of energy that the Sun radiates is not always the same
    • The orbit of the Earth around the Sun is not always the same
    • The composition of the atmosphere is not always the same
    • The reflection of sunlight at the Earth's surface (albedo) is not always the same
    • The amount of cloud cover is not always the same

    The Earth also receives energy from the atmosphere in the form of infrared radiation. Without the atmosphere, the Earth would only receive solar radiation and the temperature on Earth would be much lower. The warming of the Earth as a result of the infrared radiation of the atmoshere to the Earth is called the greenhouse effect. This greenhouse effect does not always have the same intensity because:

    • The amount of cloud cover is not always the same
    • The concentration of greenhouse gases in the atmosphere is not always the same

    Furthermore the Earth loses energy to space in the form of infrared radiation. This amount of radiation depends on the temperature. The global mean temperature adjusts in such a way that the mean amount of energy that enters the Earth-atmosphere system (in the form of solar radiation) balances to the amount that leaves the atmosphere (in the form of infrared radiation).

    These processes mentioned above do not operate independent of each other but can strengthen or weaken each other. If the temperature of the atmosphere rises, the amount of watervapor in the atmosphere increases which results in an increase of the amount of infrared radiation to the Earth (the greenhouse effect is strengthened). This will reinforce the initial temperature rise. Such a reinforcement is called a positive feedback. In this example one speaks of the watervapor feedback. Another important feedback is the snow albedo-feedback. When the temperature of the atmosphere falls, more snow remains on the Earth's surface. More sunlight is reflected and the initial temperature drop will be reinforced. This last feedback is an essential link in the onset of ice ages. A rather uncertain feedback is the cloud feedback. Clouds reflect the sunlight and thus have a cooling effect on the climate. Night clouds however diminish the amount of infrared radiation to space and thus have a warming effect on the climate. Moreover this effect on the infrared radiation strongly depends on the temperature and thus the height at which the cloud is situated. Because it is by no means clear how the cloud distribution responds to temperature changes, there is a lot of uncertainty about the nature and strength of the cloud feedback and it behaves very different in the different climate models.

    Because of atmospheric and ocean currents there is a constant redistribution of heat over the Earth's surface. Changes in these currents can cause large climate fluctuations in certain regions. The variations in the mean temperature of a certain region are generally much bigger than the variations of the global mean temperature.

    In the climate simulations of this project we prescribe the following so called climate forcings:

    • the amount of energy that the sun radiated from 1940 to 2000
    • the amount of volcanic dust in the atmosphere between 1940 and 2000
    • the amount of sulfate aerosoles in the atmosphere between 1940 and 2000
    • the concentration of greenhouse gases between 1940 and 2080
    For the first three forcings we set the values for the years after 2000 to the year 2000 values. For the concentration of greenhouse gases in the years after 2000, of which CO2 is the most important, we use the 'business as usual' scenario, in which the world continues to burn fossil fuels undiminished and as a result, the concentration of CO2 continuously increases.

    The plots below show the prescribed solar constant (the first climate forcing) and the concentration of CO2 (part of the fourth climate forcing).

    .