“Each one of us is a cause of global warming, but each one of us can make choices to change that with the things we buy, the electricity we use, the cars we drive; we can make choices to bring our individual carbon emissions to zero.” (Al Gore Nobel Peace Prize Winner)Global Warming is the expected slow, gradual warming of the lower layers of the Earth’s lower atmosphere by the slowly increasing concentrations of man-made greenhouse gases, primarily carbon dioxide, and to a lesser extent methane. These gases trap infrared radiation, which is the “heat radiation” that cools the Earth. The burning of fossil fuels, mainly petroleum and coal, produces carbon dioxide as one of the by-products. As of 2003, the concentration of carbon dioxide is over 50% higher than it was before the start of the industrial revolution in the late 1800's. To bring all this information together, the United Nations formed a group of scientists called the International Panel on Climate Change, or IPCC. The IPCC meets every few years to review the latest scientific findings and write a report summarizing all that is known about global warming. Climate model projections summarized in the latest IPCC report indicate that the global surface temperature will probably rise a further 1.1 to 6.4 °C (2.0 to 11.5 °F) during the twenty-first century. The uncertainty in this estimate arises from the use of models with differing sensitivity to greenhouse gas concentrations and the use of differing estimates of future greenhouse gas emissions. Al Gore, Nobel Peace Prize Winner 2007, underlined the possibility of the collapse of a major ice sheet in Greenland or in West Antarctica, either of which could raise global sea levels by approximately 20 feet (6 m), flooding coastal areas and producing 100 million refugees. Melting water from Greenland, because of its lower salinity, could then halt the currents that keep northern Europe warm and quickly trigger dramatic local cooling there. It also contains various short animated projections of what could happen to different animals more vulnerable to climate change. Major Causes Greenhouse Gases One of the first things scientists learned is that there are several greenhouse gases responsible for warming, and humans emit them in a variety of ways. Most come from the combustion of fossil fuels in cars, factories and electricity production. The gas responsible for the most warming is carbon dioxide, also called CO2. Other contributors include methane released from landfills and agriculture (especially from the digestive systems of grazing animals), nitrous oxide from fertilizers, gases used for refrigeration and industrial processes, and the loss of forests that would otherwise store CO2. Naturally occurring greenhouse gases have a mean warming effect of about 33 °C (59 °F). The major greenhouse gases are water vapor, which causes about 36–70 percent of the greenhouse effect; carbon dioxide (CO2), which causes 9–26 percent; methane (CH4), which causes 4–9 percent, and ozone (O3), which causes 3–7 percent.
Al Gore, Nobel Peace Prize Winner 2007, underlined the possibility of the collapse of a major ice sheet in Greenland or in West Antarctica, either of which could raise global sea levels by approximately 20 feet (6 m), flooding coastal areas and producing 100 million refugees.
Plate Tectonics
Over the course of millions of years, the motion of tectonic plates reconfigures global land and ocean areas and generates topography. This can affect both global and local patterns of climate and atmosphere-ocean circulation. The topography can influence climate. The existence of mountains (as a product of plate tectonics through mountain-building) can cause orographic precipitation. Humidity generally decreases and diurnal temperature swings generally increase with increasing elevation. Mean temperature and the length of the growing season also decrease with increasing elevation. Solar Energy Over the following approximately 4 billion years, the energy output of the sun increased and atmospheric composition changed, with the oxygenation of the atmosphere being the most notable alteration. The luminosity of the sun will continue to increase as it follows the main sequence. These changes in luminosity, and the sun's ultimate death as it becomes a red giant and then a white dwarf, will have large effects on climate, with the red giant phase possibly ending life on Earth. Orbital Variations Slight variations in Earth's orbit lead to changes in the amount of sunlight reaching the Earth's surface and how it is distributed across the globe. The former is similar to solar variations in that there is a change to the power input from the sun to the Earth system. The latter is due to how the orbital variations affect when and where sunlight is received by the Earth. The three types of orbital variations are variations in Earth's eccentricity, changes in the tilt angle of Earth's axis of rotation, and precession of Earth's axis. Volcanism Volcanism is a process of conveying material from the crust and mantle of the Earth to its surface. Volcanic eruptions, geysers, and hot springs, are examples of volcanic processes which release gases and particulates into the atmosphere. Eruptions large enough to affect climate occur on average several times per century, and cause cooling for a period of a few years. The eruption of Mount Pinatubo in 1991, the second largest terrestrial eruption of the 20th century affected the climate substantially. Human Influences Presently the scientific consensus on climate change is that human activity is very likely the cause for the rapid increase in global average temperatures over the past several decades. Consequently, the debate has largely shifted onto ways to reduce further human impact and to find ways to adapt to change that has already occurred. Of most concern in these anthropogenic factors is the increase in CO2 levels due to emissions from fossil fuel combustion, followed by aerosols (particulate matter in the atmosphere) and cement manufacture. Other factors, including land use, ozone depletion, animal agriculture and deforestation, are also of concern in the roles they play - both separately and in conjunction with other factors - in affecting climate. Effects of Global Warming “We face a true planetary emergency. The climate crisis is not a political issue, it is a moral and spiritual challenge to all of humanity." (Al Gore Nobel Peace Prize Winner 2007) Following are the effects: • Global temperatures will increase between 2 and 11.5 degrees Fahrenheit (1.1 and 6.4 degrees Celsius) by the end of this century over pre-industrial levels. • A best-guess temperature rise is between 3.2 and 7.1 degrees Fahrenheit (1.8 and 4 degrees Celsius), though the high end remains possible. • Sea levels are projected to rise between 7 and 23 inches (18 and 59 centimeters) by the end of the century. • If recent melting in Greenland and Antarctica continues, sea levels could rise an additional 4 to 8 inches (10 to 20 centimeters). • Temperatures and sea levels will continue to rise for centuries even if greenhouse gas emissions are stabilized today. • Eleven of the last 12 years rank among the 12 warmest years in the instrumental record, which stretches back to 1850. • Observational evidence suggests an increase in hurricane strength in the North Atlantic since 1970 that correlates with an increase in sea surface temperatures. • In some projections, Arctic sea ice will disappear in the late summer by the later part of this century. • It is very likely that hot extremes, heat waves, and heavy rains will continue to become more frequent. • The Gulf Stream, which brings warm waters to the North Atlantic, may slow. • Higher air temperatures will also be felt in the soil, where warmer conditions are likely to speed the natural decomposition of organic matter and to increase the rates of other soil processes that affect fertility. • Conditions are more favorable for the proliferation of insect pests in warmer climates. Longer growing seasons will enable insects such as grasshoppers to complete a greater number of reproductive cycles during the spring, summer, and autumn. Meetings for combating Global Warming Earth Summit 1992 The United Nations Conference on Environment and Development was held in 1992. 172 governments participated, with 108 sending their heads of state or government. The issues addressed included: • Systematic scrutiny of patterns of production — particularly the production of toxic components, such as lead in gasoline, or poisonous waste including radioactive chemicals. • Alternative sources of energy to replace the use of fossil fuels which are linked to global climate change. • New reliance on public transportation systems in order to reduce vehicle emissions, congestion in cities and the health problems caused by polluted air and smog. • The growing scarcity of water. An important achievement was an agreement on the Climate Change Convention which in turn led to the Kyoto Protocol. Kyoto Protocol 1997 Under the Protocol, 37 industrialized countries (called "Annex I countries") commit themselves to a reduction of four greenhouse gases (GHG) (carbon dioxide, methane, nitrous oxide, sulphur hexafluoride) and two groups of gases (hydrofluorocarbons and perfluorocarbons) produced by them, and all member countries give general commitments. Annex I countries agreed to reduce their collective greenhouse gas emissions by 5.2% from the 1990 level. Emission limits do not include emissions by international aviation and shipping, but are in addition to the industrial gases, chlorofluorocarbons, or CFCs, which are dealt with under the 1987 Montreal Protocol on Substances that Deplete the Ozone Layer. Bali Summit 2007 The 2007 United Nations Climate Change Conference took place in Bali, Indonesia, 2007. Initial EU proposals called for global emissions to peak in 10 to 15 years and decline "well below half" of the 2000 level by 2050 for developing countries and for developed countries to achieve emissions levels 20-40% below 1990 levels by 2020. The United States strongly opposed these numbers. The conference culminated in the adoption of the Bali Road Map. The Bali Road Map includes the Bali Action Plan, which charts the course for a new negotiating process designed to tackle climate change, with the aim of completing this by 2009. It also includes the AWG-KP negotiations and their 2009 deadline, the launch of the Adaptation Fund, the scope and content of the Article 9 review of the Kyoto Protocol.
One of the first things scientists learned is that there are several greenhouse gases responsible for warming, and humans emit them in a variety of ways. Most come from the combustion of fossil fuels in cars, factories and electricity production. The gas responsible for the most warming is carbon dioxide, also called CO2.
Copenhagen Summit 2009
The United Nations Climate Change Conference will take place at the Bella Center in Copenhagen, Denmark, between December 7 and December 18, 2009. According to the Bali Road Map, a framework for climate change mitigation beyond 2012 is to be agreed there. The conference was preceded by the Climate Change: Global Risks, Challenges and Decisions. Suggestions how to tackle Global Warming Biofuel Biofuels have been around as long as cars have. At the start of the 20th century, Henry Ford planned to fuel his Model Ts with ethanol, and early diesel engines were shown to run on peanut oil. But discoveries of huge petroleum deposits kept gasoline and diesel cheap for decades, and biofuels were largely forgotten. However, with the recent rise in oil prices, along with growing concern about global warming caused by carbon dioxide emissions, biofuels are the best solutions. Cell Charge According to many experts, we may soon find ourselves using fuel cells to generate electrical power for all sorts of devices we use every day. A fuel cell is a device that uses a source of fuel, such as hydrogen, and an oxidant to create electricity from an electrochemical process. Much like the batteries that are found under the hoods of automobiles or in flashlights, a fuel cell converts chemical energy to electrical energy. Geothermal Energy Geothermal energy has been used for thousands of years in some countries for cooking and heating. It is simply power derived from the Earth's internal heat. This thermal energy is contained in the rock and fluids beneath Earth's crust. It can be found from shallow ground to several miles below the surface, and even farther down to the extremely hot molten rock called magma.These underground reservoirs of steam and hot water can be tapped to generate electricity or to heat and cool buildings directly. Solar Energy Every hour the sun beams onto Earth more than enough energy to satisfy global energy needs for an entire year. Solar energy is the technology used to harness the sun's energy and make it useable. Today, the technology produces less than one tenth of one percent of global energy demand. Latest Technology Clean technologies mean a cleaner world for all. Not only do modern technologies reduce carbon pollution, they reduce other harmful pollutants that poison our lakes, make our land infertile, and harm human health. By reducing global warming pollution, we help to make our energy and transportation systems more efficient, protect our forest ecosystems, wildlife and biodiversity, and improve our air quality and protect peoples’ health. Clean Technology Clean car technology can produce more efficient, less polluting cars that get better mileage and create needed manufacturing jobs. We have the technology to clean up dirty diesel trucks and use cleaner fuels – but we can only achieve success by avoiding roadblocks and creating policies that reduce pollution. Control GHG Concentrations A commonly cited goal is to stabilize GHG concentrations around 450-550 parts per million (ppm), or about twice pre-industrial levels. This is the point at which many believe the most damaging impacts of climate change can be avoided. Current concentrations are about 380 ppm, which means there isn't much time to lose. According to the IPCC, we'd have to reduce GHG emissions by 50% to 80% of what they're on track to be in the next century to reach this level. |
Sunday, 5 January 2014
Global Warming
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