conclusion greenhouse effect essay

Essay on Greenhouse Effect for Students and Children

500 words essay on greenhouse effect.

The past month, July of 2019, has been the hottest month in the records of human history. This means on a global scale, the average climate and temperatures are now seen a steady rise year-on-year. The culprits of this climate change phenomenon are mainly pollution , overpopulation and general disregard for the environment by the human race. However, we can specifically point to two phenomenons that contribute to the rising temperatures – global warming and the greenhouse effect. Let us see more about them in this essay on the greenhouse effect.

The earth’s surface is surrounded by an envelope of the air we call the atmosphere. Gasses in this atmosphere trap the infrared radiation of the sun which generates heat on the surface of the earth. In an ideal scenario, this effect causes the temperature on the earth to be around 15c. And without such a phenomenon life could not sustain on earth.

However, due to rapid industrialization and rising pollution, the emission of greenhouse gases has increased multifold over the last few centuries. This, in turn, causes more radiation to be trapped in the earth’s atmosphere. And as a consequence, the temperature on the surface of the planet steadily rises. This is what we refer to when we talk about the man-made greenhouse effect.

Causes of Greenhouse Effect

As we saw earlier in this essay on the greenhouse effect, the phenomenon itself is naturally occurring and an important one to sustain life on our planet. However, there is an anthropogenic part of this effect. This is caused due to the activities of man.

The most prominent among this is the burning of fossil fuels . Our industries, vehicles, factories, etc are overly reliant on fossil fuels for their energy and power. This has caused an immense increase in emissions of harmful greenhouse gasses such as carbon dioxide, carbon monoxide, sulfides, etc. This has multiplied the greenhouse effect and we have seen a steady rise in surface temperatures.

Other harmful activities such as deforestation, excessive urbanization, harmful agricultural practices, etc. have also led to the release of excess carbon dioxide and made the greenhouse effect more prominent. Another harmful element that causes harm to the environment is CFC (chlorofluorocarbon).

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Some Effects of Greenhouse Effect

Even after overwhelming proof, there are still people who deny the existence of climate change and its devastating pitfalls. However, there are so many effects and pieces of evidence of climate change it is now undeniable. The surface temperature of the planet has risen by 1c since the 19th century. This change is largely due to the increased emissions of carbon dioxide. The most harm has been seen in the past 35 years in particular.

The oceans and the seas have absorbed a lot of this increased heat. The surfaces of these oceans have seen a rise in temperatures of 0.4c. The ice sheets and glaciers are also rapidly shrinking. The rate at which the ice caps melt in Antartica has tripled in the last decade itself. These alarming statistics and facts are proof of the major disaster we face in the form of climate change.

600 Words Essay on Greenhouse Effect

A Greenhouse , as the term suggests, is a structure made of glass which is designed to trap heat inside. Thus, even on cold chilling winter days, there is warmth inside it. Similarly, Earth also traps energy from the Sun and prevents it from escaping back. The greenhouse gases or the molecules present in the atmosphere of the Earth trap the heat of the Sun. This is what we know as the Greenhouse effect.

Greenhouse Gases

These gases or molecules are naturally present in the atmosphere of the Earth. However, they are also released due to human activities. These gases play a vital role in trapping the heat of the Sun and thereby gradually warming the temperature of Earth. The Earth is habitable for humans due to the equilibrium of the energy it receives and the energy that it reflects back to space.

Global Warming and the Greenhouse Effect

The trapping and emission of radiation by the greenhouse gases present in the atmosphere is known as the Greenhouse effect. Without this process, Earth will either be very cold or very hot, which will make life impossible on Earth.

The greenhouse effect is a natural phenomenon. Due to wrong human activities such as clearing forests, burning fossil fuels, releasing industrial gas in the atmosphere, etc., the emission of greenhouse gases is increasing.

Thus, this has, in turn, resulted in global warming . We can see the effects due to these like extreme droughts, floods, hurricanes, landslides, rise in sea levels, etc. Global warming is adversely affecting our biodiversity, ecosystem and the life of the people. Also, the Himalayan glaciers are melting due to this.

There are broadly two causes of the greenhouse effect:

I. Natural Causes

• Some components that are present on the Earth naturally produce greenhouse gases. For example, carbon dioxide is present in the oceans, decaying of plants due to forest fires and the manure of some animals produces methane , and nitrogen oxide is present in water and soil.
• Water Vapour raises the temperature by absorbing energy when there is a rise in the humidity.
• Humans and animals breathe oxygen and release carbon dioxide in the atmosphere.

II. Man-made Causes

• Burning of fossil fuels such as oil and coal emits carbon dioxide in the atmosphere which causes an excessive greenhouse effect. Also, while digging a coal mine or an oil well, methane is released from the Earth, which pollutes it.
• Trees with the help of the process of photosynthesis absorb the carbon dioxide and release oxygen. Due to deforestation the carbon dioxide level is continuously increasing. This is also a major cause of the increase in the greenhouse effect.
• In order to get maximum yield, the farmers use artificial nitrogen in their fields. This releases nitrogen oxide in the atmosphere.
• Industries release harmful gases in the atmosphere like methane, carbon dioxide , and fluorine gas. These also enhance global warming.

All the countries of the world are facing the ill effects of global warming. The Government and non-governmental organizations need to take appropriate and concrete measures to control the emission of toxic greenhouse gases. They need to promote the greater use of renewable energy and forestation. Also, it is the duty of every individual to protect the environment and not use such means that harm the atmosphere. It is the need of the hour to protect our environment else that day is not far away when life on Earth will also become difficult.

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Greenhouse Effect

Global warming describes the current rise in the average temperature of Earth’s air and oceans. Global warming is often described as the most recent example of climate change.

Earth Science, Meteorology, Geography

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Global warming describes the current rise in the average temperature of Earth’s air and oceans. Global warming is often described as the most recent example of climate change . Earth’s climate has changed many times. Our planet has gone through multiple ice ages , in which ice sheets and glaciers covered large portions of Earth. It has also gone through warm periods when temperatures were higher than they are today. Past changes in Earth’s temperature happened very slowly, over hundreds of thousands of years. However, the recent warming trend is happening much faster than it ever has. Natural cycles of warming and cooling are not enough to explain the amount of warming we have experienced in such a short time—only human activities can account for it. Scientists worry that the climate is changing faster than some living things can adapt to it. In 1988, the World Meteorological Organization and the United Nations Environment Programme established a committee of climatologists , meteorologists , geographers , and other scientists from around the world. This Intergovernmental Panel on Climate Change (IPCC) includes thousands of scientists who review the most up-to-date research available related to global warming and climate change. The IPCC evaluates the risk of climate change caused by human activities. According to the IPCC’s most recent report (in 2007), Earth’s average surface temperatures have risen about 0.74 degrees Celsius (1.33 degrees Fahrenheit) during the past 100 years. The increase is greater in northern latitudes . The IPCC also found that land regions are warming faster than oceans. The IPCC states that most of the temperature increase since the mid-20th century is likely due to human activities. The Greenhouse Effect Human activities contribute to global warming by increasing the greenhouse effect. The greenhouse effect happens when certain gases—known as greenhouse gases —collect in Earth’s atmosphere . These gases, which occur naturally in the atmosphere, include carbon dioxide , methane , nitrogen oxide, and fluorinated gases sometimes known as chlorofluorocarbons (CFCs). Greenhouse gases let the sun’s light shine onto Earth’s surface, but they trap the heat that reflects back up into the atmosphere. In this way, they act like the insulating glass walls of a greenhouse. The greenhouse effect keeps Earth’s climate comfortable. Without it, surface temperatures would be cooler by about 33 degrees Celsius (60 degrees Fahrenheit), and many life forms would freeze . Since the Industrial Revolution in the late 1700s and early 1800s, people have been releasing large quantities of greenhouse gases into the atmosphere. That amount has skyrocketed in the past century. Greenhouse gas emissions increased 70 percent between 1970 and 2004. Emissions of carbon dioxide, the most important greenhouse gas, rose by about 80 percent during that time. The amount of carbon dioxide in the atmosphere today far exceeds the natural range seen over the last 650,000 years. Most of the carbon dioxide that people put into the atmosphere comes from burning fossil fuels such as oil , coal , and natural gas . Cars, trucks, trains, and planes all burn fossil fuels. Many electric power plants also burn fossil fuels. Another way people release carbon dioxide into the atmosphere is by cutting down forests . This happens for two reasons. Decaying plant material, including trees, releases tons of carbon dioxide into the atmosphere. Living trees absorb carbon dioxide. By diminishing the number of trees to absorb carbon dioxide, the gas remains in the atmosphere. Most methane in the atmosphere comes from livestock farming , landfills , and fossil fuel production such as coal mining and natural gas processing. Nitrous oxide comes from agricultural technology and fossil fuel burning. Fluorinated gases include chlorofluorocarbons, hydrochlorofluorocarbons , and hydrofluorocarbons. These greenhouse gases are used in aerosol cans and refrigeration. All of these human activities add greenhouse gases to the atmosphere, trapping more heat than usual and contributing to global warming. Effects of Global Warming Even slight rises in average global temperatures can have huge effects. Perhaps the biggest, most obvious effect is that glaciers and ice caps melt faster than usual. The meltwater drains into the oceans, causing sea levels to rise and oceans to become less salty. Ice sheets and glaciers advance and retreat naturally. As Earth’s temperature has changed, the ice sheets have grown and shrunk, and sea levels have fallen and risen. Ancient corals found on land in Florida, Bermuda, and the Bahamas show that the sea level must have been five to six meters (16-20 feet) higher 130,000 years ago than it is today. Earth doesn’t need to become oven-hot to melt the glaciers. Northern summers were just three to five degrees Celsius (five to nine degrees Fahrenheit) warmer during the time of those ancient fossils than they are today. However, the speed at which global warming is taking place is unprecedented . The effects are unknown. Glaciers and ice caps cover about 10 percent of the world’s landmass today. They hold about 75 percent of the world’s fresh water. If all of this ice melted, sea levels would rise by about 70 meters (230 feet). The IPCC reported that the global sea level rose about 1.8 millimeters (0.07 inches) per year from 1961 to 1993, and 3.1 millimeters (0.12 inches) per year since 1993. Rising sea levels could flood coastal communities, displacing millions of people in areas such as Bangladesh, the Netherlands, and the U.S. state of Florida. Forced migration would impact not only those areas, but the regions to which the “ climate refugees ” flee . Millions more people in countries like Bolivia, Peru, and India depend on glacial meltwater for drinking, irrigation , and hydroelectric power . Rapid loss of these glaciers would devastate those countries. Glacial melt has already raised the global sea level slightly. However, scientists are discovering ways the sea level could increase even faster. For example, the melting of the Chacaltaya Glacier in Bolivia has exposed dark rocks beneath it. The rocks absorb heat from the sun, speeding up the melting process. Many scientists use the term “climate change” instead of “global warming.” This is because greenhouse gas emissions affect more than just temperature. Another effect involves changes in precipitation like rain and snow . Patterns in precipitation may change or become more extreme. Over the course of the 20th century, precipitation increased in eastern parts of North and South America, northern Europe, and northern and central Asia. However, it has decreased in parts of Africa, the Mediterranean, and parts of southern Asia. Future Changes Nobody can look into a crystal ball and predict the future with certainty. However, scientists can make estimates about future population growth, greenhouse gas emissions, and other factors that affect climate. They can enter those estimates into computer models to find out the most likely effects of global warming. The IPCC predicts that greenhouse gas emissions will continue to increase over the next few decades . As a result, they predict the average global temperature will increase by about 0.2 degrees Celsius (0.36 degrees Fahrenheit) per decade. Even if we reduce greenhouse gas and aerosol emissions to their 2000 levels, we can still expect a warming of about 0.1 degree Celsius (0.18 degrees Fahrenheit) per decade. The panel also predicts global warming will contribute to some serious changes in water supplies around the world. By the middle of the 21st century, the IPCC predicts, river runoff and water availability will most likely increase at high latitudes and in some tropical areas. However, many dry regions in the mid-latitudes and tropics will experience a decrease in water resources. As a result, millions of people may be exposed to water shortages . Water shortages decrease the amount of water available for drinking, electricity , and hygiene . Shortages also reduce water used for irrigation. Agricultural output would slow and food prices would climb. Consistent years of drought in the Great Plains of the United States and Canada would have this effect. IPCC data also suggest that the frequency of heat waves and extreme precipitation will increase. Weather patterns such as storms and tropical cyclones will become more intense. Storms themselves may be stronger, more frequent, and longer-lasting. They would be followed by stronger storm surges , the immediate rise in sea level following storms. Storm surges are particularly damaging to coastal areas because their effects (flooding, erosion , damage to buildings and crops) are lasting. What We Can Do Reducing our greenhouse gas emissions is a critical step in slowing the global warming trend. Many governments around the world are working toward this goal. The biggest effort so far has been the Kyoto Protocol , which was adopted in 1997 and went into effect in 2005. By the end of 2009, 187 countries had signed and ratified the agreement. Under the protocol , 37 industrialized countries and the European Union have committed to reducing their greenhouse gas emissions. There are several ways that governments, industries, and individuals can reduce greenhouse gases. We can improve energy efficiency in homes and businesses. We can improve the fuel efficiency of cars and other vehicles. We can also support development of alternative energy sources, such as solar power and biofuels , that don’t involve burning fossil fuels. Some scientists are working to capture carbon dioxide and store it underground, rather than let it go into the atmosphere. This process is called carbon sequestration . Trees and other plants absorb carbon dioxide as they grow. Protecting existing forests and planting new ones can help balance greenhouse gases in the atmosphere. Changes in farming practices could also reduce greenhouse gas emissions. For example, farms use large amounts of nitrogen-based fertilizers , which increase nitrogen oxide emissions from the soil. Reducing the use of these fertilizers would reduce the amount of this greenhouse gas in the atmosphere. The way farmers handle animal manure can also have an effect on global warming. When manure is stored as liquid or slurry in ponds or tanks, it releases methane. When it dries as a solid, however, it does not. Reducing greenhouse gas emissions is vitally important. However, the global temperature has already changed and will most likely continue to change for years to come. The IPCC suggests that people explore ways to adapt to global warming as well as try to slow or stop it. Some of the suggestions for adapting include:

• Expanding water supplies through rain catchment , conservation , reuse, and desalination .
• Adjusting crop locations, variety, and planting dates.
• Building seawalls and storm surge barriers and creating marshes and wetlands as buffers against rising sea levels .
• Creating heat-health action plans , boosting emergency medical services, and improving disease surveillance and control.
• Diversifying tourism attractions, because existing attractions like ski resorts and coral reefs may disappear.
• Planning for roads and rail lines to cope with warming and/or flooding.
• Strengthening energy infrastructure , improving energy efficiency, and reducing dependence on single sources of energy.

Barking up the Wrong Tree Spruce bark beetles in the U.S. state of Alaska have had a population boom thanks to 20 years of warmer-than-average summers. The insects have managed to chew their way through 1.6 million hectares (four million acres) of spruce trees.

Disappearing Penguins Emperor penguins ( Aptenodytes forsteri ) made a showbiz splash in the 2005 film March of the Penguins . Sadly, their encore might include a disappearing act. In the 1970s, an abnormally long warm spell caused these Antarctic birds' population to drop by 50 percent. Some scientists worry that continued global warming will push the creatures to extinction by changing their habitat and food supply.

Shell Shock A sudden increase in the amount of carbon dioxide in the atmosphere does more than change Earth's temperature. A lot of the carbon dioxide in the air dissolves into seawater. There, it forms carbonic acid in a process called ocean acidification. Ocean acidification is making it hard for some sea creatures to build shells and skeletal structures. This could alter the ecological balance in the oceans and cause problems for fishing and tourism industries.

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Related Resources

Essay on Greenhouse Effect: Causes, Problems, Effects and Prevention

The process by which radiation from a planet’s atmosphere warms its surface to a temperature which exceeds the normal temperature of the planet is called greenhouse effect. If a planet’s atmosphere contains greenhouse gases, the atmosphere will radiate the energy in various directions. Some part of this radiation will be towards the surface, making it warm. The downward component of the radiation, which is the strength of the greenhouse effect will depend on the atmosphere’s temperature and amount of greenhouse gases present in the atmosphere.

The earth’s atmosphere is warmed by absorbing infrared thermal radiation from the sun. The greenhouse gases which are present in the atmosphere radiate energy, some of which is directed to the surface and lower atmosphere. The mechanism which produces this difference between the actual surface temperature and effective temperature is due to the temperature, knows as greenhouse effect.

The natural greenhouse effect of the earth is critical to support life. Human activities such as burning the fossil fuels and clearing the forests have made an intense impact on natural greenhouse effect, leading to global warming.

History of Greenhouse Effect

The term greenhouse effect was first used by atmospheric scientists in early 1800s. The existence of greenhouse effect was brought up by Joseph Fourier in 1824. In 1896, the effect was fully qualified by Svante Arrhenius, who made the first quantitative prediction of global warming because of a hypothetical doubling of atmospheric carbon dioxide. At the time, it was used to describe the naturally occurring functions of greenhouse gases present in the atmosphere, and did not have any negative subtexts. It was not until the mid 1950s that greenhouse effect was teamed with concern for climate change.

Greenhouse gases that cause Greenhouse Effect

The major gases which contribute to the greenhouse effect on earth are as follows:-

• Water vapor 36-70%
• Carbon dioxide 9-26%
• Methane 4-9%

The below mentioned activities release gases which prove to be harmful for the planet. Following are the six major greenhouses which play a lead role in the greenhouse effect and global warming:-

1. Carbon dioxide (CO2)

It is a naturally occurring gas, produced by living organisms and fermentation. Carbon dioxide which is emitted from fuel burning is responsible for approx 87% of global warming, and has alarmingly increased by 27% since the industrial revolution.

2. Methane (CH4)

Methane is a naturally occurring inflammable gas which is produced by decomposition of organic matters and geological coal formations. The landfills hole the major credit to release methane, which adds up into the atmosphere and leads the global warming.

3. Nitrogen oxides (NOx)

Nitrogen oxides are naturally occurring from microbial action present in the soil. It is also produced by burning of fuels. Due to the increased use of nitrogen based fertilizers and catalytic converters in automobiles, the production of nitrogen oxides has raised, thus disturbing the ecosystem balance.

4. Hydrofluorocarbon gases (HFCs)

Chlorofluorocarbons (CFCs), coolant, cleaning and propellant gases were blacklisted internationally due to its harmful effect on the ozone layer. HFCs also play a crucial part in global warming, and are 4,000 to 10,000 times more harmful than carbon dioxide.

5. Sulphur hexafluoride (SF6)

Very low atmospheric concentration can make it a good test gas for gas concentration monitors. SF6 is a man-made gas used in water leakage detection for cable cooling systems and insulating materials for high voltage equipment.

6. Perfluorocrbons (PFCs)

PFCs are man-made replacement gases for CFCs, but they also result as a by-product of aluminum smelting. They are also used as a purging agent for semi conductor manufacturing. They cause severe damage to the atmosphere too.

What does increased greenhouse gases indicate?

The increase in greenhouse gases directly increases the heat on the planet’s surface and lower atmosphere. It has a dangerous effect as it can reduce or even create holes in the ozone layer. Due to this, harmful rays such as ultra violet rays can seep in though the thin areas and cause damage on earth.

What are the causes of greenhouse effect?

1. burning the fossil fuels.

Fossil fuels such as coal, natural gas and oil are an integral part of our lives, the elements which play a vital role in daily routines. The most important use of fossil fuels occurs in producing electricity and transportation. On burning the fossil fuels, the carbon dioxide stored inside them is released, which combines with oxygen in the air, resulting in production of carbon dioxide. As the population is increasing, the numbers of vehicles have made a high leap too. Due to this, the pollution has increased in the atmosphere. As these vehicles run, carbon dioxide is released, which is one of the main gases responsible for increase in greenhouse effect.

Electricity related emissions are high because we are still dependant on coal for generating electricity, which releases a huge amount of carbon dioxide into the atmosphere. Since it is the primary source of generating electricity, the loss of fossil fuels is massive, due to which the global warming has increased.

2. Deforestation

A major section of the land on our earth is covered by the forests. They are very important for a sustainable life on earth, as plants give out oxygen and inhale the carbon dioxide. Thus, the ecosystem is balanced due to the presence of trees. Sadly, large scale development of the urban landscapes has resulted in depletion of green cover of the earth. Forests are now being burnt down or chopped off to build concrete buildings instead. On burning the wood, the stored carbon is converted back to carbon dioxide, which adds up into the atmosphere, increasing the pollution.

3. Industrial waste and landfills

Various industries which are involved in cement production, fertilizers, extraction of oil, coal mining activities etc produce harmful greenhouse gases. Also, landfills filled with garbage produce carbon dioxide and methane, which play a major role in the greenhouse effect.

4. Population rise

Increase in population over the decades has led to high demand for food, clothing and shelter. Machines used in our daily lives such as air conditioners also exhale harmful gases, which contribute to the greenhouse effect. Also, more number of people means more usage of fossil fuels, which has made the situations much worse.

What are the harmful effects of greenhouse effect?

The adverse effects of greenhouse effect are alarming. They are already being experienced on the earth now, and can go much adverse changes in the near future. The major harmful effects of greenhouse effect are listed below:

• The sea levels will rise. There is more than 5,773,000 cubic miles of water present in form of ice caps, glaciers and permanent snow. According to the National Snow and Ice Data Center, if all of the glaciers met, the sea level would rise by 230 feet! This will not happen all at once, but the levels will rise certainly, submerging the low-lying areas.
• The balance of the global ecosystem will be affected. The fresh water stored in the ice caps will desalinate the ocean as they melt. The desalination in the gulf current will play a negative impact on the ocean currents, which regulate temperatures. It will be difficult to draw a pattern of warming and cooling in some areas.
• Warmer water and stronger hurricanes will be more frequent than now. Due to the rise in oceans’ temperature, the probability of frequent and stronger hurricanes may also become a threat.
• Weather patterns will continue to change. Most of the regions that are currently subjected to droughts will face much challenging conditions. The wet region will get wetter too. Mountain glaciers and snow caps will further shrink which will jeopardize many water supply systems. These negative changes have already begun to show their impact in some parts of the world.
• Ecosystems will be stressed due the impact of greenhouse effect and global warming. Flora and fauna will be massively affected. The animals which cannot adapt to the climatic changes will extinct over the time, thus misbalancing the ecosystem balance. A variety of pests and tropical diseases are expected to sprout in the warmer regions. Valuable species especially in the arctic will be the worst affected.

Evidence to the changes in earth’s climate: Global Warming

The effects of greenhouse effect and global warming have already started showing up in some parts of the world. Situations are predicted to get much worse. Some of the observations recorded by the Intergovernmental Panel on Climate Change (IPCC) are as follows: -

• Eleven out of twelve warmest years since 1850 occurred between 1996 and 2006. Average global temperatures have risen by approximately 0.74C between 1906 and 2005. This rise in temperature is widespread throughout the world, but higher at the northern latitudes.
• Sea levels have increased during the same period. Since 1961, the average rate has been 1.8 mm per year, but has now further increased to 3.1 mm per year since 1993.
• Some of the climate changes agencies from the United States have reported that the oceans all over the world are getting warmer at a rate much higher than predicted. The warming has occurred approximately 50% faster over that last century, than it was calculated previously.

A number of human activities contribute to the greenhouse effect, which has brought us to the alarming situations today. If continued without taking precautions to save the earth, the situations are going to be worse. Some of the human activities which produce greenhouse gases are as follows: -

• Fuel combustion
• Vehicle transport and automobiles
• Energy industries
• Use of oil and natural gas
• Metal production manufacturing industries and construction
• Fugitive emissions from fuels
• Mineral products
• Chemical industries
• Production of halocarbons
• Solvent and other product use
• Consumption of halocarbons and sulphur hexafluoride
• Production of halocarbons and sulphur hexafluoride
• Enteric fermentation
• Rice cultivation
• Agricultural soils
• Prescribes burning of savannas
• Solid waste disposal on land
• Wastewater handling
• Waste incineration
• Field burning of agricultural residues

What preventive should be taken against greenhouse effect?

It would not be late today if we take an initiative to make the earth a reliable place to live in. to reduce the harmful effects of greenhouse gases on the earth and atmosphere, change must be brought in our daily routine and lifestyles. Here are some of the best suggestive steps to keep in mind to reduce greenhouse gas emissions:-

• Reduce, Reuse, Recycle Following the three Rs in your daily life can make a difference too. Buying products with minimal packaging will help in reducing waste. Through recycling half of your household waste, 2,400 pounds of carbon dioxide can be saved from adding up in the atmosphere.
• By adding insulation to the walls, installing caulking or weather stripping around doors and windows.
• Lower the heat while sleeping and keep the temperature moderate all the time.
• Installing a programmable thermostat can save a large amount of carbon dioxide from being released. By setting it just 2 degrees lower during winter and higher in summer can save approx. 2,000 pounds of carbon dioxide each year.
• Replace the light bulbs with Compact Fluorescent Lights It is better to use compact fluorescent light (CFL) than the usual light bulbs. By replacing just one 60-watt incandescent light bulb with a CFL, over $30 will be saved over the life of the bulb. Also, the CFL gives off 70 percent less heat than the light bulbs and lasts 10 times longer than them too.
• Drive less and drive smart Walking and biking are a great form of exercise. Not only they will keep you fit, but also make your contribution towards saving the planet, since less driving means lesser emissions. Every gallon of gas saved will keep 20 pounds of carbon dioxide away from the atmosphere.
• Use less hot water Set your water heater at 120 degrees and wrap it in an insulating blanket if it is 15 years old. Also, use low flow showerheads to save hot water and approx 350 pounds of carbon dioxide every year.
• Buy energy efficient products Home appliances now come in a wide range of energy efficient models, and compact fluorescent bulbs are designed to use much lesser amount of energy than the regular light bulbs.
• Plant a tree Trees are the best solution to fight against the greenhouse effect and global warming. Not only they inhale carbon dioxide and release oxygen for us, plantation will also help in restoring the disturbed ecological balance.
• Use the ‘off’ switch Save electricity and reduce global warming by using power only when you need it. Make a habit to switch off lights, television, computer and other electronic devices when they are not in use. Turn off the water tap when you do not need the water. These simple steps will help you in reducing the energy usage and burning of fossil fuels. Less energy usage means less dependence on fossil fuels, which on burning contribute to the harmful greenhouse effect.

Greenhouse effect Essay Conclusion

Greenhouse effect and global warming are the biggest threat to human race and the biggest environmental challenge of 21st century that we need to tackle. It is important for all citizens to become fully aware of the causes and harmful consequences of greenhouse effect and global warming. The main culprits of greenhouse effect and global warming is the growing emission of harmful gases such as Methane, carbon dioxide and carbon monoxide resulting from emissions of industrial activities, incomplete combustion of petrol and diesel from vehicles as well as growing emissions of CFCs from air conditioners. It is important for individuals to choose greener alternatives such as cycling, hybrid clean fuels and for industries and governments to choose environmental friendly production methods and energy sources. Immediate action on this greenhouse effect and global warming is necessary to tackle this environmental problem.

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21.1: The Greenhouse Effect and Climate Change

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• Page ID 47008

• Melissa Ha and Rachel Schleiger
• Yuba College & Butte College via ASCCC Open Educational Resources Initiative

Earth’s Temperature is a Balancing Act

Earth’s temperature depends on the balance between energy entering and leaving the planet. When incoming energy from the sun is absorbed, Earth warms. When the sun’s energy is reflected back into space, Earth avoids warming. When energy is released from Earth into space, the planet cools. Many factors, both natural and human, can cause changes in Earth’s energy balance, including:

• Changes in the greenhouse effect, which affects the amount of heat retained by Earth’s atmosphere;
• Variations in the sun’s energy reaching Earth;
• Changes in the reflectivity of Earth’s atmosphere and surface.

Scientists have pieced together a picture of Earth’s climate, dating back hundreds of thousands of years, by analyzing a number of indirect measures of climate such as ice cores, tree rings, glacier size, pollen counts, and ocean sediments. Scientists have also studied changes in Earth’s orbit around the sun and the activity of the sun itself.

The historical record shows that the climate varies naturally over a wide range of time scales. In general, climate changes prior to the Industrial Revolution in the 1700s can be explained by natural causes, such as changes in solar energy, volcanic eruptions, and natural changes in greenhouse gas (GHG) concentrations. Recent changes in climate , however, cannot be explained by natural causes alone. Research indicates that natural causes are very unlikely to explain most observed warming, especially warming since the mid-20th century. Rather, human activities, especially our combustion of fossil fuels, explains the current warming (figure \(\PageIndex{a}\)). The scientific consensus is clear: through alterations of the carbon cycle, humans are changing the global climate by increasing the effects of something known as the greenhouse effect.

The Greenhouse Effect Causes the Atmosphere to Retain Heat

Gardeners that live in moderate or cool environments use greenhouses because they trap heat and create an environment that is warmer than outside temperatures. This is great for plants that like heat, or are sensitive to cold temperatures, such as tomato and pepper plants. Greenhouses contain glass or plastic that allow visible light from the sun to pass. This light, which is a form of energy, is absorbed by plants, soil, and surfaces and heats them. Some of that heat energy is then radiated outwards in the form of infrared radiation, a different form of energy. Unlike with visible light, the glass of the greenhouse blocks the infrared radiation, thereby trapping the heat energy, causing the temperature within the greenhouse to increase.

The same phenomenon happens inside a car on a sunny day. Have you ever noticed how much hotter a car can get compared to the outside temperature? Light energy from the sun passes through the windows and is absorbed by the surfaces in the car such as seats and the dashboard. Those warm surfaces then radiate infrared radiation, which cannot pass through the glass. This trapped infrared energy causes the air temperatures in the car to increase. This process is commonly known as the greenhouse effect .

The video below made for kids, but provides a clear and simple introduction to the greenhouse effect.

The greenhouse effect also happens with the entire Earth. Of course, our planet is not surrounded by glass windows. Instead, the Earth is wrapped with an atmosphere that contains greenhouse gases (GHGs). Much like the glass in a greenhouse, GHGs allow incoming visible light energy from the sun to pass, but they block infrared radiation that is radiated from the Earth towards space (figure \(\PageIndex{b}\)). In this way, they help trap heat energy that subsequently raises air temperature. Being a greenhouse gas is a physical property of certain types of gases; because of their molecular structure they absorb wavelengths of infrared radiation, but are transparent to visible light. Some notable greenhouse gases are water vapor (H 2 O), carbon dioxide (CO 2 ), and methane (CH 4 ). GHGs act like a blanket, making Earth significantly warmer than it would otherwise be. Scientists estimate that average temperature on Earth would be -18º C without naturally-occurring GHGs.

What is Global Warming?

Global warming refers to the recent and ongoing rise in global average temperature near Earth’s surface. It is caused mostly by increasing concentrations of greenhouse gases in the atmosphere. Global warming is causing climate patterns to change. However, global warming itself represents only one aspect of climate change.

What is Climate Change?

Climate change refers to any significant change in the measures of climate lasting for an extended period of time. In other words, climate change includes major changes in temperature, precipitation, or wind patterns, among other effects, that occur over several decades or longer.

The Main Greenhouse Gasses

The most important GHGs directly emitted by humans include CO 2 and methane. Carbon dioxide  (CO 2 ) is the primary greenhouse gas that is contributing to recent global climate change. CO 2 is a natural component of the carbon cycle, involved in such activities as photosynthesis, respiration, volcanic eruptions, and ocean-atmosphere exchange. Human activities, primarily the burning of fossil fuels and changes in land use, release very large amounts of CO 2 to the atmosphere, causing its concentration in the atmosphere to rise.

Atmospheric CO 2 concentrations have increased by 45% since pre-industrial times, from approximately 280 parts per million (ppm) in the 18th century to 409.8 ppm in 2019 (figure \(\PageIndex{c}\)). The current CO 2 level is higher than it has been in at least 800,000 years, based on evidence from ice cores that preserve ancient atmospheric gases (figure \(\PageIndex{d-f}\)). Human activities currently release over 30 billion tons of CO 2 into the atmosphere every year. While some volcanic eruptions released large quantities of CO 2 in the distant past, the U.S. Geological Survey (USGS) reports that human activities now emit more than 135 times as much CO 2 as volcanoes each year. This human-caused build-up of CO 2 in the atmosphere is like a tub filling with water, where more water flows from the faucet than the drain can take away.

Other Greenhouse Gasses

Although this concentration is far less than that of CO 2 , methane (CH 4 ) is 28 times as potent a greenhouse gas. Methane is produced when bacteria break down organic matter under anaerobic conditions and can be released due to natural or anthropogenic processes. Anaerobic conditions can happen when organic matter is trapped underwater (such as in rice paddies) or in the intestines of herbivores. Anthropogenic causes now account for 60% of total methane release. Examples include agriculture, fossil fuel extraction and transport, mining, landfill use, and burning of forests. Specifically, raising cattle releases methane due to fermentation in their rumens produces methane that is expelled from their GI tract. Methane is more abundant in Earth’s atmosphere now than at any time in at least the past 650,000 years, and CH 4 concentrations increased sharply during most of the 20th century. They are now more than two and-a-half times pre-industrial levels (1.9 ppm), but the rate of increase has slowed considerably in recent decades.

Water vapor is the most abundant greenhouse gas and also the most important in terms of its contribution to the natural greenhouse effect, despite having a short atmospheric lifetime. Some human activities can influence local water vapor levels. However, on a global scale, the concentration of water vapor is controlled by temperature, which influences overall rates of evaporation and precipitation. Therefore, the global concentration of water vapor is not substantially affected by direct human emissions.

Ground-level ozone (O 3 ), which also has a short atmospheric lifetime, is a potent greenhouse gas. Chemical reactions create ozone from emissions of nitrogen oxides and volatile organic compounds from automobiles, power plants, and other industrial and commercial sources in the presence of sunlight (as discussed in section 10.1). In addition to trapping heat, ozone is a pollutant that can cause respiratory health problems and damage crops and ecosystems.

Changes in the Sun’s Energy Affect how Much Energy Reaches Earth

Climate can be influenced by natural changes that affect how much solar energy reaches Earth. These changes include changes within the sun and changes in Earth’s orbit. Changes occurring in the sun itself can affect the intensity of the sunlight that reaches Earth’s surface. The intensity of the sunlight can cause either warming (during periods of stronger solar intensity) or cooling (during periods of weaker solar intensity). The sun follows a natural 11-year cycle of small ups and downs in intensity, but the effect on Earth’s climate is small. Changes in the shape of Earth’s orbit as well as the tilt and position of Earth’s axis can also affect the amount of sunlight reaching Earth’s surface.

Changes in the sun’s intensity have influenced Earth’s climate in the past. For example, the so-called “ Little Ice Age ” between the 17th and 19th centuries may have been partially caused by a low solar activity phase from 1645 to 1715, which coincided with cooler temperatures. The Little Ice Age refers to a slight cooling of North America, Europe, and probably other areas around the globe. Changes in Earth’s orbit have had a big impact on climate over tens of thousands of years. These changes appear to be the primary cause of past cycles of ice ages, in which Earth has experienced long periods of cold temperatures (ice ages), as well as shorter interglacial periods (periods between ice ages) of relatively warmer temperatures.

Changes in solar energy continue to affect climate. However, solar activity has been relatively constant, aside from the 11-year cycle, since the mid-20th century and therefore does not explain the recent warming of Earth. Similarly, changes in the shape of Earth’s orbit as well as the tilt and position of Earth’s axis affect temperature on relatively long timescales (tens of thousands of years), and therefore cannot explain the recent warming.

Changes in Reflectivity Affect How Much Energy Enters Earth’s System

When sunlight energy reaches Earth it can be reflected or absorbed. The amount that is reflected or absorbed depends on Earth’s surface and atmosphere. Light-colored objects and surfaces, like snow and clouds, tend to reflect most sunlight, while darker objects and surfaces, like the ocean and forests, tend to absorb more sunlight. The term albedo refers to the amount of solar radiation reflected from an object or surface, often expressed as a percentage. Earth as a whole has an albedo of about 30%, meaning that 70% of the sunlight that reaches the planet is absorbed. Sunlight that is absorbed warms Earth’s land, water, and atmosphere.

Albedo is also affected by aerosols. Aerosols are small particles or liquid droplets in the atmosphere that can absorb or reflect sunlight. Unlike greenhouse gases (GHGs), the climate effects of aerosols vary depending on what they are made of and where they are emitted. Those aerosols that reflect sunlight, such as particles from volcanic eruptions or sulfur emissions from burning coal, have a cooling effect. Those that absorb sunlight, such as black carbon (a part of soot), have a warming effect.

Natural changes in albedo, like the melting of sea ice or increases in cloud cover, have contributed to climate change in the past, often acting as feedbacks to other processes. Volcanoes have played a noticeable role in climate. Volcanic particles that reach the upper atmosphere can reflect enough sunlight back to space to cool the surface of the planet by a few tenths of a degree for several years. Volcanic particles from a single eruption do not produce long-term change because they remain in the atmosphere for a much shorter time than GHGs.

Human changes in land use and land cover have changed Earth’s albedo. Processes such as deforestation, reforestation, desertification, and urbanization often contribute to changes in climate in the places they occur. These effects may be significant regionally, but are smaller when averaged over the entire globe.

Scientific Consensus: Global Climate Change is Real

The Intergovernmental Panel on Climate Change (IPCC) was created in 1988 by the United Nations Environment Programme and the World Meteorological Organization. It is charged with the task of evaluating and synthesizing the scientific evidence surrounding global climate change. The IPCC uses this information to evaluate current impacts and future risks, in addition to providing policymakers with assessments. These assessments are released about once every every six years. The most recent report, the 5th Assessment, was released in 2013. Hundreds of leading scientists from around the world are chosen to author these reports. Over the history of the IPCC, these scientists have reviewed thousands of peer-reviewed, publicly available studies. The scientific consensus is clear: global climate change is real and humans are very likely the cause for this change.

Additionally, the major scientific agencies of the United States, including the National Aeronautics and Space Administration (NASA) and the National Oceanic and Atmospheric Administration (NOAA), also agree that climate change is occurring and that humans are driving it. In 2010, the US National Research Council concluded that “Climate change is occurring, is very likely caused by human activities, and poses significant risks for a broad range of human and natural systems”. Many independent scientific organizations have released similar statements, both in the United States and abroad. This doesn’t necessarily mean that every scientist sees eye to eye on each component of the climate change problem, but broad agreement exists that climate change is happening and is primarily caused by excess greenhouse gases from human activities. Critics of climate change, driven by ideology instead of evidence, try to suggest to the public that there is no scientific consensus on global climate change. Such an assertion is patently false.

Current Status of Global Climate Change and Future Changes

Greenhouse gas concentrations in the atmosphere will continue to increase unless the billions of tons of anthropogenic emissions each year decrease substantially. Increased concentrations are expected to do the following:

• Increase Earth’s average temperature (figure \(\PageIndex{g}\)),
• Influence the patterns and amounts of precipitation,
• Reduce ice and snow cover, as well as permafrost,
• Raise sea level (figure \(\PageIndex{h}\)),
• Increase the acidity of the oceans.

Figure \(\PageIndex{h}\):  Sea height variation (mm) over time. Sea height has increased about 3.3 millimeters per year on average since 1993. Data is from satellite sea level observations by the NASA Goddard Space Flight Center. Image by NASA (public domain).

These changes will impact our food supply, water resources, infrastructure, ecosystems, and even our own health. The magnitude and rate of future climate change will primarily depend on the following factors:

• The rate at which levels of greenhouse gas concentrations in our atmosphere continue to increase,
• How strongly features of the climate (e.g., temperature, precipitation, and sea level) respond to the expected increase in greenhouse gas concentrations,
• Natural influences on climate (e.g., from volcanic activity and changes in the sun’s intensity) and natural processes within the climate system (e.g., changes in ocean circulation patterns).

Past and Present-day GHG Emissions Will Affect Climate Far into the Future

Many greenhouse gases stay in the atmosphere for long periods of time. As a result, even if emissions stopped increasing, atmospheric greenhouse gas concentrations would continue to remain elevated for hundreds of years. Moreover, if we stabilized concentrations and the composition of today’s atmosphere remained steady (which would require a dramatic reduction in current greenhouse gas emissions), surface air temperatures would continue to warm. This is because the oceans, which store heat, take many decades to fully respond to higher greenhouse gas concentrations. The ocean’s response to higher greenhouse gas concentrations and higher temperatures will continue to impact climate over the next several decades to hundreds of years.

Future Temperature Changes

Climate models project the following key temperature-related changes:

• Average global temperatures are expected to increase by 2°F to 11.5°F by 2100, depending on the level of future greenhouse gas emissions, and the outcomes from various climate models.
• By 2100, global average temperature is expected to warm at least twice as much as it has during the last 100 years.
• Ground-level air temperatures are expected to continue to warm more rapidly over land than oceans.
• Some parts of the world are projected to see larger temperature increases than the global average.

Future Precipitation and Storm Events

Patterns of precipitation and storm events, including both rain and snowfall are likely to change. However, some of these changes are less certain than the changes associated with temperature. Projections show that future precipitation and storm changes will vary by season and region. Some regions may have less precipitation, some may have more precipitation, and some may have little or no change. The amount of rain falling in heavy precipitation events is likely to increase in most regions, while storm tracks are projected to shift towards the poles. Climate models project the following precipitation and storm changes:

• Global average annual precipitation through the end of the century is expected to increase, although changes in the amount and intensity of precipitation will vary by region.
• The intensity of precipitation events will likely increase on average. This will be particularly pronounced in tropical and high-latitude regions, which are also expected to experience overall increases in precipitation.
• The strength of the winds associated with tropical storms is likely to increase. The amount of precipitation falling in tropical storms is also likely to increase.
• Annual average precipitation is projected to increase in some areas and decrease in others.

Future Ice, Snowpack, and Permafrost

Arctic sea ice is already declining drastically. The area of snow cover in the Northern Hemisphere has decreased since 1970. Permafrost temperature has increased over the last century, making it more susceptible to thawing. Over the next century, it is expected that sea ice will continue to decline, glaciers will continue to shrink, snow cover will continue to decrease, and permafrost will continue to thaw.

For every 2°F of warming, models project about a 15% decrease in the extent of annually averaged sea ice and a 25% decrease in September Arctic sea ice. The coastal sections of the Greenland and Antarctic ice sheets are expected to continue to melt or slide into the ocean. If the rate of this ice melting increases in the 21st century, the ice sheets could add significantly to global sea level rise. Glaciers are expected to continue to decrease in size. The rate of melting is expected to continue to increase, which will contribute to sea level rise.

Future Sea Level Change

Warming temperatures contribute to sea level rise by expanding ocean water, melting mountain glaciers and ice caps, and causing portions of the Greenland and Antarctic ice sheets to melt or flow into the ocean. Since 1870, global sea level has risen by about 8 inches. Estimates of future sea level rise vary for different regions, but global sea level for the next century is expected to rise at a greater rate than during the past 50 years. The contribution of thermal expansion, ice caps, and small glaciers to sea level rise is relatively well-studied, but the impacts of climate change on ice sheets are less understood and represent an active area of research. Thus, it is more difficult to predict how much changes in ice sheets will contribute to sea level rise. Greenland and Antarctic ice sheets could contribute an additional 1 foot of sea level rise, depending on how the ice sheets respond.

Regional and local factors will influence future relative sea level rise for specific coastlines around the world (figure \(\PageIndex{i}\)). For example, relative sea level rise depends on land elevation changes that occur as a result of subsidence (sinking) or uplift (rising), in addition to things such as local currents, winds, salinity, water temperatures, and proximity to thinning ice sheets. Assuming that these historical geological forces continue, a 2-foot rise in global sea level by 2100 would result in the following relative sea level rise:

• 2.3 feet at New York City
• 2.9 feet at Hampton Roads, Virginia
• 3.5 feet at Galveston, Texas
• 1 foot at Neah Bay in Washington state

Future Ocean Acidification

Ocean acidification is the process of ocean waters decreasing in pH. Oceans become more acidic as carbon dioxide (CO 2 ) emissions in the atmosphere dissolve in the ocean. This change is measured on the pH scale, with lower values being more acidic. The pH level of the oceans has decreased by approximately 0.1 pH units since pre-industrial times, which is equivalent to a 25% increase in acidity. The pH level of the oceans is projected to decrease even more by the end of the century as CO 2 concentrations are expected to increase for the foreseeable future. Ocean acidification adversely affects many marine species, including plankton, mollusks, shellfish, and corals. As ocean acidification increases, the availability of calcium carbonate will decline. Calcium carbonate is a key building block for the shells and skeletons of many marine organisms. If atmospheric CO 2 concentrations double, coral calcification rates are projected to decline by more than 30%. If CO 2 concentrations continue to rise at their current rate, corals could become rare on tropical and subtropical reefs by 2050.

Mismatched Interactions

Climate change also affects phenology, the study of the effects of climatic conditions on the timing of periodic lifecycle events, such as flowering in plants or migration in birds. Researchers have shown that 385 plant species in Great Britain are flowering 4.5 days sooner than was recorded earlier during the previous 40 years. In addition, insect-pollinated species were more likely to flower earlier than wind-pollinated species. The impact of changes in flowering date would be mitigated if the insect pollinators emerged earlier. This mismatched timing of plants and pollinators could result in injurious ecosystem effects because, for continued survival, insect-pollinated plants must flower when their pollinators are present.

Likewise, migratory birds rely on daylength cues, which are not influenced by climate change. Their insect food sources, however, emerge earlier in the year in response to warmer temperatures. As a result, climate change decreases food availability for migratory bird species.

Spread of Disease

This rise in global temperatures will increase the range of disease-carrying insects and the viruses and pathogenic parasites they harbor. Thus, diseases will spread to new regions of the globe. This spread has already been documented with dengue fever, a disease the affects hundreds of millions per year, according to the World Health Organization. Colder temperatures typically limit the distribution of certain species, such as the mosquitoes that transmit malaria, because freezing temperatures destroy their eggs.

Not only will the range of some disease-causing insects expand, the increasing temperatures will also accelerate their lifecycles, which allows them to breed and multiply quicker, and perhaps evolve pesticide resistance faster. In addition to dengue fever, other diseases are expected to spread to new portions of the world as the global climate warms. These include malaria, yellow fever, West Nile virus, zika virus, and chikungunya.

Climate change does not only increase the spread of diseases in humans. Rising temperatures are associated with greater amphibian mortality due to chytridiomycosis (see Invasive Species ). Similarly, warmer temperatures have exacerbated bark beetle infestations of coniferous trees, such as pine an spruce.

Climate Change Affects Everyone

Our lives are connected to the climate . Human societies have adapted to the relatively stable climate we have enjoyed since the last ice age which ended several thousand years ago. A warming climate will bring changes that can affect our water supplies, agriculture, power and transportation systems, the natural environment, and even our own health and safety.

Carbon dioxide can stay in the atmosphere for nearly a century, on average, so Earth will continue to warm in the coming decades. The warmer it gets, the greater the risk for more severe changes to the climate and Earth’s system. Although it’s difficult to predict the exact impacts of climate change, what’s clear is that the climate we are accustomed to is no longer a reliable guide for what to expect in the future.

We can reduce the risks we will face from climate change . By making choices that reduce greenhouse gas pollution, and preparing for the changes that are already underway, we can reduce risks from climate change. Our decisions today will shape the world our children and grandchildren will live in.

You can take steps at home, on the road, and in your office to reduce greenhouse gas emissions and the risks associated with climate change. Many of these steps can save you money. Some, such as walking or biking to work, can even improve your health! You can also get involved on a local or state level to support energy efficiency, clean energy programs, or other climate programs.

Suggested Supplementary Reading

Intergovernmental Panel on Climate Change. 2013. 5th Assessment: Summary for Policymakers .

NASA. 2018. Global Climate Change: Vital Signs of the Planet . This website by NASA provides a multi-media smorgasbord of engaging content. Learn about climate change using data collected by NASA satellites and more.

Attributions

Modified by Melissa Ha from the following sources:

• Climate and the Effects of Global Climate Change  from  General Biology  by OpenStax (licensed under  CC-BY )
• Climate Change  from  Environmental Biology  by Matthew R. Fisher (licensed under  CC-BY )
• Carbon Cycle from  Biology  by John W. Kimball (licensed under  CC-BY )

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Can We Engineer Our Way Out of the Climate Crisis?

Mammoth, a giant machine in Iceland that will pull planet-warming carbon dioxide out of the air. Credit... Francesca Jones for The New York Times

Supported by

By David Gelles

David Gelles reported from Reykjavik, Iceland, and Midland, Texas.

• March 31, 2024

On a windswept Icelandic plateau, an international team of engineers and executives is powering up an innovative machine designed to alter the very composition of Earth’s atmosphere.

If all goes as planned, the enormous vacuum will soon be sucking up vast quantities of air, stripping out carbon dioxide and then locking away those greenhouse gases deep underground in ancient stone — greenhouse gases that would otherwise continue heating up the globe.

Just a few years ago, technologies like these, that attempt to re-engineer the natural environment, were on the scientific fringe. They were too expensive, too impractical, too sci-fi. But with the dangers from climate change worsening, and the world failing to meet its goals of slashing greenhouse gas emissions, they are quickly moving to the mainstream among both scientists and investors, despite questions about their effectiveness and safety.

First in a series on the risky ways humans are starting to manipulate nature to fight climate change. Once science fiction, today these ideas are becoming reality.

Researchers are studying ways to block some of the sun’s radiation. They are testing whether adding iron to the ocean could carry carbon dioxide to the sea floor. They are hatching plans to build giant parasols in space . And with massive facilities like the one in Iceland, they are seeking to reduce the concentration of carbon dioxide in the air.

As the scale and urgency of the climate crisis has crystallized, “people have woken up and are looking to see if there’s any miraculous, deus ex machina that can help,” said Al Gore, the former vice president.

Since the dawn of the industrial age, humans have pumped huge volumes of heat-trapping gases into the atmosphere in pursuit of industry and advancement. It amounted to a remaking of the planet’s delicately balanced atmosphere that today has transformed the world, intensifying heat, worsening droughts and storms and threatening human progress.

As the risks became clearer, political and corporate leaders pledged to keep global average temperatures to no more than 1.5 degrees Celsius higher than before the Industrial Revolution . But for several months last year, the world briefly passed that symbolic threshold, sooner than many scientists expected.

Global temperatures are now expected to rise as much as 4 degrees Celsius, or more than 7 degrees Fahrenheit, by the end of the century. That has given new weight to what some people call geoengineering, though that term has become so contentious its proponents now prefer the term “climate interventions.” The hope is that taking steps like these might buy some time at a moment when energy consumption is on the rise, and the world isn’t quitting fossil fuels fast enough.

Many of the projects are controversial. A plant similar to the one in Iceland, but far larger, is being built in Texas by Occidental Petroleum, the giant oil company. Occidental intends to use some of the carbon dioxide it captures to extract even more oil, the burning of which is one of the main causes of the climate crisis in the first place.

Some critics say that other types of interventions could open up a Pandora’s box of new problems by scrambling weather patterns or amplifying human suffering through unintended consequences. In effect they are asking: Should humans be experimenting with the environment in this way? Do we know enough to understand the risks?

“We need more information so we can make these decisions in the future,” said Alan Robock, a professor of atmospheric science at Rutgers University. “Which is riskier: to do it, or not to do it?”

Others argue that fanciful or costly technologies will simply waste resources and time, or lull people with the false idea that it will be possible to slow global warming without phasing out fossil fuels.

There is also the risk of rogue actors barreling ahead with their own efforts to change the climate. Already, Mexico has banned what’s known as solar radiation modification after a start-up from California released sulfur dioxide into the atmosphere without permission.

And then there is the fact that, because these technologies are so new, there is relatively little regulation governing them.

“There are these much bigger questions around who decides how is this is all coordinated over time,” said Marion Hourdequin, a professor of environmental philosophy at Colorado College. “We don’t have a great track record of sustained global cooperation.”

With a subzero wind whipping down from the fjords, Edda Aradottir trudged through fresh snow to inspect the direct air capture plant in Iceland.

Ms. Aradottir is the chief executive of Carbfix, an Icelandic company that is working with the Swiss start-up that built the plant, Climeworks. Known as Mammoth, the project is a technological accomplishment, powered by clean geothermal energy and capable of capturing up to 36,000 metric tons of carbon dioxide per year and pumping it down into the bedrock.

That is just one one-millionth of annual global emissions. But unlike trees, which can be cut down or catch fire, Climeworks promises to store that carbon dioxide forever.

Inside a series of bunkerlike buildings, dozens of huge fans suck air into bins that contain chemical pellets that absorb carbon dioxide, then release the gas when they are heated up. The carbon dioxide is then mixed with water and pumped more than a mile below the surface, where extreme pressure turns it into a solid in a matter of years, a process known as “mineralization.” In effect, the gas becomes part of the rock.

“Over 99 percent of the carbon on Earth is already stored in rocks in the form of minerals,” Ms. Aradottir said. “Naturally, it happens over geologic time scales. We’re speeding it up.”

When Mammoth is turned on in the coming weeks, it will be the largest such facility in the world, even though the amount of carbon it can absorb is still just a drop in the bucket. Global carbon dioxide emissions hit an all-time high of 36 billion metric tons last year.

The Occidental plant, being built near Odessa, Texas, and known as Stratos, will be more than 10 times more powerful than Mammoth, powered by solar energy, and have the potential to capture and sequester 500,000 metric tons of carbon dioxide per year.

It uses a different process to extract carbon dioxide from the air, though the goal is the same: Most of it will be locked away deep underground. But at least some of the carbon dioxide, Occidental says, will also be used to extract more oil.

In that process, carbon dioxide is pumped into the ground to force out oil that might otherwise be too difficult to reach. Techniques like this have made Occidental a company worth more than $50 billion and helped send American crude production to a new high in recent years.

Of course, it is the world’s reliance on the burning of oil and other fossil fuels that has so dangerously sent carbon dioxide levels soaring. In the atmosphere, carbon dioxide acts as a blanket, trapping the sun’s heat and warming the world.

Today, Occidental says it is trying to become a “carbon management” company as well as an oil producer. Last year, it paid $1.1 billion for a start-up called Carbon Engineering that had developed a way to soak up carbon dioxide from the air, and began building the Stratos project. Today, what was a barren plot of dirt less than 12 months ago is a bustling construction site.

“It’s like the Apollo missions at NASA,” said Richard Jackson, who oversees carbon management and domestic oil operations at Occidental. “We’re trying to move as quickly as we can.”

In coming years, Occidental said it planned to build 100 facilities, each capable of capturing 1 million metric tons of carbon dioxide a year. It has struck up a financial partnership with BlackRock, the world’s largest asset manager, and made a deal to develop direct air capture plants with Adnoc, the United Arab Emirates’ state oil company.

In South Texas, it is planning to build 30 of the plants on the King Ranch, funded in part by $1.2 billion the Biden administration last year awarded to direct air capture projects .

Climeworks also has aggressive expansion plans. It secured a portion of the White House funds for a direct air capture plant in Louisiana, is working with a group of Kenyan entrepreneurs to build a large facility outside Nairobi and has plans to construct plants in Canada and other countries in Europe.

Driving the construction boom is the desire of many corporations to reduce their effect on global warming. Over the past decade, hundreds of multinational corporations have pledged to become carbon neutral by 2040. Rather than phasing out fossil fuels to meet those goals, most companies are finding that they have to pay for carbon credits, which can be acquired by preserving forests, supporting renewable energy projects or paying for carbon sequestration.

Microsoft, JPMorgan and UBS are some of the big companies that have signed long term agreements to buy credits from Climeworks. Amazon, AT&T and the Houston Astros are among those signed up with Occidental.

Bill Gates, the Microsoft co-founder, said last year that he was the largest individual customer of Climeworks, paying the company $10 million each year to offset his sizable carbon footprint.

Yet the grand plans envisioned by direct air capture companies, with hundreds of plants built in the years ahead, are predicated on a market that does not yet exist. Only a handful of big companies have so far proved willing to voluntarily spend millions of dollars on direct air capture credits, and there is no guarantee that the rest of the corporate world will follow suit anytime soon.

Even if more companies do decide to start offsetting their emissions, there are cheaper ways to do so, including by preserving forests and paying for renewable energy. For example, it currently costs between $500 and $1,000 to capture a metric ton of carbon dioxide with direct air capture, compared with just $10 to $30 per ton for most carbon credits today .

“ It’s very expensive,” said Mr. Robock. “And so it’s not going to be a solution in the short term or the long term.”

Still, the business world is bullish. Boston Consulting Group expects more companies to begin buying credits to pay for carbon dioxide removal, and more governments to encourage that buying. In the United States and Europe, governments have started subsidizing the construction of the plants. By 2040, BCG expects the market for carbon dioxide removal technologies could grow from less than $10 billion today to as much as $135 billion.

“Companies will face a rising price on carbon and regulatory pressures that will make them feel compelled to do this,” said Rich Lesser, the global chair of BCG.

Although the direct air capture market is still in its infancy, it already has vociferous detractors in academia, activist circles and beyond.

Some say it is little more than a ploy by oil and gas companies to prolong the very industries that are responsible for creating global warming. They point to the extensive evidence that fossil fuel interests for years worked to play down public awareness of climate change, and the fact that some of the captured carbon will be used for additional oil production.

Those concerns were magnified when Vicki Hollub, Occidental’s chief executive, last year said direct air capture could “preserve our industry.” She added, “This gives our industry a license to continue to operate for the 60, 70, 80 years that I think it’s going to be very much needed.”

Scientists say an urgent transition away from fossil fuels is necessary to avoid extreme global temperature increases. Last year, nearly 200 countries agreed to begin phasing out oil, coal and gas.

“This is a new wave of denial, deception and delay,” said Lili Fuhr, director of the fossil economy program at the Center for International Environmental Law. “You have the fossil fuel industry trying to say we can engineer our way out of this without any major changes to business as usual.”

A related line of reasoning holds that the enormous amounts of clean energy needed to power direct air capture plants would be better used powering homes and businesses, thereby displacing fossil fuels such as natural gas and coal that still provide much of the world’s electricity.

Ms. Fuhr added that the costs remained high in spite of a growing raft of government support, including a tax credit in the United States worth $180 for every metric ton of carbon dioxide that is captured and stored, a subsidy that is likely to significantly lower Occidental’s tax bill in the years ahead. “The industry has been successful in capturing subsidies, just not carbon,” she said.

And then there is the fact that even if Occidental and Climeworks make good on their ambitions to build hundreds of new plants in the coming years, they would still not come close to capturing even 1 percent of current annual global emissions.

Mark Z. Jacobson, a professor of civil and environmental engineering at Stanford University, said climate interventions in general, and carbon capture in particular, were dangerous distractions from the more urgent work of rapidly reducing the use of fossil fuels.

“There are many solutions that are just not helpful at all, that do not help an iota for climate and don’t help an iota for air pollution,” he said. “Among these are direct air capture.”

Proponents of the technology say that with fossil fuel emissions continuing to rise, the world is fast approaching the moment when any and all solutions to abate global warming should be on the table.

At the least, direct air capture has a role to play, they say, because there might always be at least some greenhouse gases being produced in the future, even if the vast majority of emissions are successfully eliminated. Sucking that carbon dioxide out of the air will be valuable, the argument goes.

But in the longer term, many scientists believe it will be necessary to go further and actually try to remove some of the excess carbon dioxide that has dangerously accumulated over the centuries. Proponents of direct air capture say their technology is suited for such a herculean task.

“No one is arguing you could solve all our carbon emissions with this,” Mr. Lesser said. “But it could be a meaningful part of solving a huge problem.”

The past year’s record temperatures, warming oceans and megafires are all evidence of a deeply uncomfortable reality: We’ve already been manipulating the planet for the past couple hundred years. In less time than it takes a redwood tree to reach its full height, humans have added enough carbon dioxide to the atmosphere to scramble weather patterns, melt glaciers and wipe out coral reefs.

Viewed this way, today’s attempts to slow down or even reverse the warming can be seen as efforts to undo the changes that have already taken place. Whether or not humans can succeed in this most ambitious feat is unclear. It is among the most consequential problems our species has faced.

Yet as people begin to deliberately tinker with the climate in new ways, there are profound questions that are only beginning to be contemplated. If the current extreme weather and temperature rise came about inadvertently, as the unintentional consequence of human development, what might happen when we begin actively trying to control the planet’s atmosphere?

“It’s true that we have been altering the climate through greenhouse gas emissions for centuries now,” said Ms. Hourdequin of Colorado College. “But trying to intentionally manage the climate through geoengineering would be a distinctive endeavor, quite different than the kind of haphazard interference that we’ve engaged in thus far.”

David Gelles reports on climate change and leads The Times’s Climate Forward newsletter and events series . More about David Gelles

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Decades of buried trash in landfills is releasing methane , a powerful greenhouse gas, at higher rates than previously estimated, a study says.

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Global warming conclusion.

Global warming is not something to take lightly. The oceans are warming, the polar ice caps are melting, and greenhouse gas levels are at an all-time high. These are just some of the things that the claims-makers for the global warming cause have said. The science has proven them right. So, the ultimate claim is that humans are a large factor in the increased rate of global warming. There are claims-makers of all kinds fighting about whether that is true or not. The solutions proposed deal with a cleaner world, while the deniers will opt to do nothing.  This issue has turned political, and it seems like nothing gets done until someone who believes in global warming is in charge. Right now, that is not the case. This issue will continue to get worse until there is no turning back. Hopefully society can come to a consensus to try and inhibit global warming. This is the only way to keep the place we live healthy.

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Climate Change: Evidence and Causes (2014)

Chapter: conclusion.

Below is the uncorrected machine-read text of this chapter, intended to provide our own search engines and external engines with highly rich, chapter-representative searchable text of each book. Because it is UNCORRECTED material, please consider the following text as a useful but insufficient proxy for the authoritative book pages.

Conclusion This document explains that there are well-understood physical mechanisms by which changes in the amounts of greenhouse gases cause climate changes. It discusses the evidence that the concentrations of these gases in the atmosphere have increased and are still increasing rapidly, that climate change is occurring, and that most of the recent change is almost certainly due to emissions of greenhouse gases caused by human activities. Further climate change is inevitable; if emissions of greenhouse gases continue unabated, future changes will substantially exceed those that have occurred so far. There remains a range of estimates of the magnitude and regional expression of future change, but increases in the extremes of climate that can adversely affect natural ecosystems and human activities and infrastructure are expected. Citizens and governments can choose among several options (or a mixture of those options) in response to this information: they can change their pattern of energy production and usage in order to limit emissions of greenhouse gases and hence the magnitude of climate changes; they can wait for changes to occur and accept the losses, damage and suffering that arise; they can adapt to actual and expected changes as much as possible; or they can seek as yet unproven ‘geoengineering’ solutions to counteract some of the climate changes that would otherwise occur. Each of these options has risks, attractions and costs, and what is actually done may be a mixture of these different options. Different nations and communities will vary in their vulnerability and their capacity to adapt. There is an important debate to be had about choices among these options, to decide what is best for each group or nation, and most importantly for the global population as a whole. The options have to be discussed at a global scale, because in many cases those communities that are most vulnerable control few of the emissions, either past or future. Our description of the science of climate change, with both its facts and its uncertainties, is offered as a basis to inform that policy debate. E v i de n c e & C a u se s B9 

Climate Change: Evidence and Causes is a jointly produced publication of The US National Academy of Sciences and The Royal Society. Written by a UK-US team of leading climate scientists and reviewed by climate scientists and others, the publication is intended as a brief, readable reference document for decision makers, policy makers, educators, and other individuals seeking authoritative information on the some of the questions that continue to be asked.

Climate Change makes clear what is well-established and where understanding is still developing. It echoes and builds upon the long history of climate-related work from both national academies, as well as on the newest climate-change assessment from the United Nations' Intergovernmental Panel on Climate Change. It touches on current areas of active debate and ongoing research, such as the link between ocean heat content and the rate of warming.

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Electrical properties of the Ge 2 Sb 2 Te 5 thin films for phase change memory application

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P. I. Lazarenko , A. A. Sherchenkov , S. A. Kozyukhin , A. V. Babich , S. P. Timoshenkov , D. G. Gromov , A. S. Shuliatyev , E. N. Redichev; Electrical properties of the Ge 2 Sb 2 Te 5 thin films for phase change memory application. AIP Conf. Proc. 21 April 2016; 1727 (1): 020013. https://doi.org/10.1063/1.4945968

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In this study I-V characteristic, temperature dependence of resistivity, thermopower, switching and memory effect were investigated for GST225 thin films. Resistivities, ratio of the resistivities of amorphous and crystalline states, activation energies of conductivity, temperature of phase transition, Seebeck coefficient, transition time due to the transformation from OFF to ON states and full recording time were estimated. It was shown that transport mechanism based on the two-channel model has a good correlation with experimental results for Ohmic region of I-V characteristic, while space-charge limited current mechanism for power region.

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