Questions from category Climate Change:
The term Global Warming refers to the observation that the atmosphere near the Earth's surface is warming. This warming is one of many kinds of climate change that the Earth has gone through in the past and will continue to go through in the future. It is reasonable to expect that the Earth should warm as the amount of greenhouse gases in the atmosphere increases. It is known for certain that atmospheric concentrations of greenhouse gases are rising dramatically due to human activity. It is less well known exactly how the increases in these greenhouse gases factor in the observed changes of the Earth's climate and global temperatures.
The Earth's climate changes when the amount of energy stored by the climate system is varied. The most significant changes occur when the global energy balance between incoming energy from the Sun and outgoing heat from the Earth is upset. There are a number of natural mechanisms that can upset this balance, for example fluctuations in the Earth's orbit, variations in ocean circulation and changes in the composition of the Earth's atmosphere. In recent times, the latter has been evident as a consequence not of natural processes but of man-made pollution, through emissions of greenhouse gases and aerosols. By altering the global energy balance, such mechanisms "force" the climate to change. Consequently, scientists call them "climate forcing" mechanisms.
Global, annual-mean radiative forcings (Wm-2) due to a number of agents from the period from pre-industrial (1750) to present (2000). (IPCC 2001)
The major components of the climate system that are important for climatic change and its consequences, such as sea level rise, during the next century are: the atmosphere, oceans, terrestrial biosphere, glaciers and ice sheets and land surface. In order to project the impact of human perturbations on the climate system, it is necessary to calculate the effects of all the key processes operating in these climate system components and the interactions between them. These climate processes can be represented in mathematical terms based on physical laws such as the conservation of mass, momentum, and energy. However, the complexity of the system means that the calculations from these mathematical equations can be performed in practice only by using a computer. The mathematical formulation is therefore implemented in a computer program, which we refer to as a 'model'. If the model includes enough of the components of the climate system to be useful for simulating the climate, it is commonly called a 'climate model'."
Basic physics tells us that greenhouse gases trap Earth's heat and cause warming. But Earth's climate is very complex, involving interactions among the air, land and oceans. That's why scientists use computer models to project the effects of global warming. Though the models are far from exact, they do a reasonable job of simulating our current climate and reproducing known changes from past climates. Scientists are confident about the models' abilities to simulate large-scale effects of global warming, such as global temperature increase and average sea level rise. The models are less reliable when it comes to simulating changes in other weather variables such as changes in rainfall. Also, current models are still ill-equipped to predict with any confidence what will happen in local areas.
Weather and climate are different. The methods used to forecast changes in weather and climate differ as well. Because the weather changes from day to day, current weather forecasts are reliable for roughly ten days. Climate, on the other hand, can be thought of as average weather, including weather's variability over much longer time horizons (e.g., from year to year). Natural changes in our planet's climate happen over the course of years, centuries and many millennia. Long-term climate forecasts are possible because scientists understand many of the factors that influence climate over such long periods, such as changes in the sun's energy and the level of greenhouse gases in the atmosphere. Climate scientists do not claim to know how to predict day-to-day fluctuations (weather) over the 21st century. Rather, they are predicting how they think average temperature and precipitation (climate) will change due to human activities.
Separating out the impact of human activity from natural climate variation is extremely difficult. Nonetheless, the IPCC concluded there is a 'discernible human influence' on climate. This means the observed global warming is unlikely to be the result of natural variability alone and that human activities are at least partially responsible.
Many greenhouse gases occur naturally, but human activities are adding gases to the natural mix at an unprecedented rate. Water vapor is the most abundant greenhouse gas; it occurs naturally and makes upabout two thirds of the natural greenhouse effect. Fuel burning and other human activities, however, are adding large amounts of greenhouse gases to the atmosphere - the most important ones being carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), hydrofluorocarbons(HFCs), perfluorocarbons (PFCs) and sulfur hexafluoride (SF6). Since pre-industrial times atmospheric concentrations of CO2, CH4 and N2O have climbed by over 30%, 145% and 15%, respectively. Scientists have confirmed this is primarily due to human activity. Burning coal, oil and gas, and cutting down forests are largely responsible.
Because human emissions of CO2 and other greenhouse gases continue to climb, and because they remain in the atmosphere for decades to centuries (depending on the gas), we're committing ourselves to a warmer climate in the future. The IPCC projects an average global temperature increase of 2-6°F by 2100, and greater warming there after. Temperatures in some parts of the globe (e.g., the polar regions) are expected to rise even faster. Even the low end of the IPCC's projected range represents a rate of climate change unprecedented in the past 10,000 years.
Our health, agriculture, water resources, forests, wildlife and coastal areas are vulnerable to global warming and the climatic changes it will bring. The IPCC concluded that 'climate change is likely to have wide-ranging and mostly adverse impacts on human health, with significant loss of life.' A few degrees of warming increases the chances of more frequent and severe heat waves, which can cause more heat-related death and illness. Greater heat can also mean worsened air pollution, as well as damaged crops and depleted water resources. Warming is likely to allow tropical diseases, such as malaria, to spread northward in some areas of the world. It will also intensify the Earth's hydrological cycle. This means that both evaporation and precipitation will increase. Some areas will receive more rain, while other areas will be drier. At the same time, extreme events like floods and droughts are likely to become more frequent. Warming will cause glaciers to melt and oceans to expand. The IPCC projects that sea level will rise one half foot to three feet over the next century. This threatens low-lying coastal areas. Scientists are also concerned that warming could lead to more intense storms.
A warming of 1°F over the past century and a further 2-6°F over the 21st century, as projected by the IPCC, may appear minor compared to short-term weather changes from night to day and winter to summer. But in global climate terms, a warming at this rate would be much larger and faster than any of the climatic changes over the past 10,000 years. Global temperatures during the last ice age (about 20,000 years ago) were 'only' 9°F cooler than today, but that was enough to allow massive ice sheets to reach as far south as the Great Lakes and New York City. The warming that humans are causing will change Earth's climate in the opposite direction, but tens or possibly a hundred times faster than natural rates of climate change. Warming of a few degrees would lead to more frequent droughts and heat waves, cause greater rainfall, and possibly change the strength of storms. It is possible that some areas would benefit from global warming even as other areas were harmed. Certain farming areas, for example, could enjoy a longer growing season, while others suffer from more frequent droughts. Local effects, however, are the most difficult to predict, making it difficult to know who will benefit and who will not, and for how long these conditions will persist, as the warming continues and the climate keeps changing.
Natural and human factors affect the average temperature of our planet. Natural variability in the Earth's climate system can cause small changes over decades to centuries. Gradual changes in Earth's orbit around the sun (which in turn change how sunlight hits our planet) are thought to be the key pacemaker for the comings and goings of past ice ages over many millennia. The sun's energy can also vary slightly over time. Large volcanic eruptions can cool the planet for a few years by spewing out particles that block some sunlight. Even some of our own pollutants, like the sulfur dioxide released from power plants and heavy industry that contributes to acid rain, have a similar cooling effect. Depletion of the ozone layer caused by our release of chlorofluorocarbons has led to cooling of the upper atmosphere. Scientists think these temporary cooling effects have been masking some of the long-term warming being caused by human emissions of greenhouse gases. Over the 21st century, the ongoing buildup of greenhouse gases in the atmosphere is likely to be the most dominant influence on our planet's climate.
Polar ice caps are some of the largest surface features on our planet and any changes to them, however small, could have far reaching effects. Melting due to global warming is expected to reduce the size and extent of the polar ice caps, even after taking into account the potential for more snow and ice accumulation atop the ice sheets due to increased precipitation. Melting of polar ice and land based glaciers is expected to contribute to the one half foot to three feet sea level rise projected by the IPCC for the 21st century. Shrinking ice caps may also cause changes in ocean circulation and even storm tracks. To be sure, not all of the melting currently occurring is due to global warming, and the melting of floating sea ice does not affect sea level. Further warming will likely accelerate the shrinkage of ice caps and glaciers, however. Of particular concern is the stability of the West Antarctic Ice Sheet. A sudden collapse would raise sea levels 16-20 feet, but the IPCC considers the likelihood of such a collapse before the year 2100 low.
Until recently, conflicting studies suggested that temperatures measured by satellites revealed a slight cooling trend, whereas the surface temperature record showed a warming trend. This confounded the global warming issue. Satellites began measurements in 1979 and the surface temperature record, which reveals global warming of about 1°F, dates back to about 1860. Satellites take temperatures through vertical slices of the atmosphere, not at the surface. Satellite measurements are also known to be influenced by ozone layer depletion, which has caused cooling of the upper atmosphere. For these and other reasons, satellite and surface data are not expected to be a perfect match. Nevertheless, the discrepancy between the two data sets was too large to be ignored. Then scientists discovered they neglected some measurement and calibration problems with the satellites, including the fact that satellites were falling from their orbits, which produced an artificial cooling trend. Correcting the satellite data for these problems revealed a small warming trend. These corrections - though not the last word on the satellite vs. surface discrepancy - bring the satellite record into better agreement with surface measurements. Any remaining discrepancies do not invalidate the fact that surface temperatures are rising.
The Earth has a natural CO2 cycle that moves massive amounts of CO2 into and out of the atmosphere. The oceans and land vegetation release and absorb over 200 billion metric tons of carbon into and out of the atmosphere each year. When the cycle is balanced, atmospheric levels of CO2 remain relatively stable. Human activities are now adding about 7 billion metric tons of carbon into the atmosphere every year, which is only about 3-4% of the amount exchanged naturally. But that's enough to knock the system out of balance, surpassing nature's ability to take our CO2 emissions out of the atmosphere. The oceans and land vegetation are absorbing about half of our emissions; the other half remains airborne for 100 years or longer. This is what is causing the rapid buildup of CO2, a buildup that dwarfs natural fluctuations.
Given our knowledge of global warming and our changing climate, we can expect more extreme weather, including more frequent hot days and droughts, less frequent cold days, and more precipitation (including more snowfall in cold areas). But attributing any particular extreme weather event to global warming remains beyond the current limits of scientific capability.
El Nino is a natural phenomenon that has been occurring throughout the centuries, though not always with the same regularity; it now occurs about every two to seven years. El Nino is the strong warming of the equatorial Pacific ocean. Its effects are felt worldwide, which demonstrates the interconnected nature of the Earth's climate. Recent El Nino events have been very strong and have contributed to the record-setting temperatures of the 1990s', evidence that El Nino events can warm parts of the Earth. But now scientists are examining how human-induced global warming could affect El Nino. Scientists are concerned that the accumulation of greenhouse gases in our atmosphere may inject enough heat into the Pacific Ocean to make El Nino events more frequent and fierce.
Exactly how global warming will impact individual locations, let alone individuals, is uncertain. But because global temperatures, rainfall, sea levels and the frequency of extreme weather are expected to increase, you could be affected in many ways. Your health and comfort could be affected if your region experiences more frequent heat waves and worse air pollution. These health concerns are especially serious if you are or care for the very young, very old, or if you have heart and respiratory problems. In the winter time you may feel milder temperatures. You may pay higher energy bills for air conditioning in summer, and lower bills for heating in winter. If you live in the country's interior, particularly in dry areas, water shortages may be more frequent, leading to more restrictions on your water usage. If you live along the coast, your home may be threatened by sea level rise and an increase in storm intensity. The cost of food may change as farmers and the food industry adapt to new climate patterns. And the outdoor activities that you and your family enjoy could be affected by increased beach erosion, decreased snow fall and retreating glaciers, and loss of forests and wildlife, where species are unable to adapt to the changing climate.
As a business owner, your costs, competition, and planning decisions may be affected. Your health care costs could increase if the public health sector is burdened by increases in heat and climate related mortality and illness. Like homeowners, your business's energy costs will reflect the need for greater cooling in the summer and less heating in the winter. Your property insurance premiums could go up due to more droughts and floods and possibly more intense storms. If your business is located along the coast, sea level rise may also affect property insurance, not to mention how rising seas may directly impact your business. If your business depends on waterways for transportation, those shipping costs could increase in some areas due to reduced river flow and lower lake levels, though in northern areas shipping could be eased by a longer ice-free season. If you're in the agricultural or food industry, changing climatic and growing season conditions will require adaptations. Your competitors in this sector may experience either more or less favorable climatic changes than you. The same is true if you're in a forestry related business. Some of global warming's impacts may be most severe in other nations less capable of adapting. This may create social and economic disruptions that ripple across the globe to affect your business. For all of these reasons, long-term business planning will increasingly have to consider the changing nature of our planet's climate.
Energy or solar radiation enters the atmosphere as sunshine. The sky reflects a portion of this radiation, the rest is absorbed by the Earth and is eventually released again as thermal radiation. Both man-made and naturally occurring events can limit the amount of solar radiation at the earth's surface. Urban air pollution, smoke from forest fires, and airborne ash resulting from volcanic activity reduce the solar resource by increasing the scattering and absorption of solar radiation. Some scientists think of the radiation budget in terms of a balance. If the Earth gets more energy from the Sun, the Earth heats up and emits more thermal energy. This brings the radiation budget into balance. If the Earth emits more of this thermal energy than it absorbs from solar radiation, the Earth cools off. As it cools off, the Earth emits less energy. This change also brings the radiation budget back into balance.