Global warming is the temperature of Earth's surface, oceans and atmosphere going up over tens of years. Average temperatures today are about 1 °C (1.8 °F) higher than 150 years ago, but in some parts of the world it is less than this and some more. Many scientists say that in the next 100–200 years, temperatures might be up to 6 °C (11 °F) higher than they were before the effects of global warming were discovered. The most noticeable changes because of this increase in temperature is the melting of ice caps all around the world. Sea level is rising steadily because of continental ice melting into the sea. Many cities will be partly flooded by the ocean in the 21st century.
Among the greenhouse gases, the increase of carbon dioxide in the atmosphere is the main cause of global warming, as predicted by Svante Arrhenius a hundred years ago, confirming the work of Joseph Fourier more than 200 years ago. When people burn fossil fuels like coal, oil and natural gas this adds carbon dioxide into the air. This is because fossil fuels contain lots of carbon and burning means joining most of the atoms in the fuel with oxygen. When people cut down many trees (deforestation), this means less carbon dioxide is taken out of the atmosphere by those plants.
As the Earth's surface temperature becomes hotter the sea level becomes higher. This is partly because water expands when it gets warmer. It is also partly because warm temperatures make glaciers and ice caps melt. The sea level rise causes coastal areas to flood. Weather patterns, including where and how much rain or snow there is, are changing. Deserts will probably increase in size. Colder areas will warm up faster than warm areas. Strong storms may become more likely and farming may not make as much food. These effects will not be the same everywhere. The changes from one area to another are not well known.
People in government and the Intergovernmental Panel on Climate Change (IPCC) are talking about global warming. But governments, companies and other people do not agree on what to do about it. Some things that could reduce warming are to burn less fossil fuels, eat less meat, grow more trees, and put some carbon dioxide back in the ground. Shading the Earth from some sunlight (this is called geoengineering) could also reduce warming but we don't understand how it might change weather in other ways. Also people could adapt to any temperature changes. The Kyoto Protocol and Paris Agreement try to reduce pollution from the burning of fossil fuels. Most governments have agreed to them but some people in government think nothing should change. The gas produced by cows digestion also causes global warming, because it contains a greenhouse gas called methane.
Since the 1800s, people have recorded the daily temperature. By about 1850, there were enough places measuring temperature so that scientists could know the global average temperature. From 1920 to 1940, the temperature got warmer. From 1940 to 1970, the temperature got slightly cooler. From 1970 to today, the average temperature for the world has increased by about 1 °C (1.8 ± 0.4 °F). Starting in 1979, satellites started measuring the temperature of the Earth.
Before 1850, there were not enough temperature measurements for us to know how warm or cold it was. Climatologists use proxy measurements to try to figure out past temperatures before there were thermometers. This means measuring things that change when it gets colder or warmer. One way is to cut into a tree and measure how far apart the growth rings are. Trees that live a long time can give us an idea of how temperature and rain changed while it was alive.
For most of the past 2000 years the temperature didn't change much. There were some times where the temperatures were a little warmer or cooler. One of the most famous warm times was the Medieval Warm Period and one of the most famous cool times was the Little Ice Age. Other proxy measurements like the temperature measured in deep holes mostly agree with the tree rings. Tree rings and bore holes can only help scientists work out the temperature until about 1000 years ago. Ice cores are also used to find out the temperature back to about half a million years ago.
The greenhouse effectEdit
Coal-burning power plants, car exhausts, factory smokestacks, and other man-made waste gas vents give off about 23 billion tons of carbon dioxide and other greenhouse gases into the Earth's atmosphere each year. The amount of CO2 in the air is about 31% more than it was around 1750. About three-quarters of the CO2 that people have put in the air during the past 20 years are due to burning fossil fuel like coal or oil. The rest mostly comes from changes in how land is used, like cutting down trees.
The sun gets a little bit hotter and colder every 11 years. This is called the 11-year sunspot cycle. The change is so small that scientists can barely measure how it affects the temperature of the Earth. If the sun was causing the Earth to warm up, it would warm both the surface and high up in the air. But the air in the upper stratosphere is actually getting colder, so scientists don't think changes in the sun have much effect
Dust and dirtEdit
Dust and dirt in the air may come from natural sources such as volcanos, erosion and meteoric dust. Some of this dirt falls out within a few hours. Some is aerosol, so small that it could stay in the air for years. The aerosol particles in the atmosphere make the earth colder. The effect of dust therefore cancels out some of the effects of greenhouse gases. Even though humans also put aerosols in the air when they burn coal or oil this only cancels out the greenhouse effect of the fuel burning for less than 20 years: the carbon dioxide stays in the atmosphere much longer and keeps on warming the earth.
Some people try to stop global warming, usually by burning less fossil fuel. Many people have tried to get countries to emit less greenhouse gases. The Kyoto Protocol was signed in 1997. It was meant to reduce the amount of greenhouse gases in the atmosphere to below their levels in 1990. However, carbon dioxide levels have continued to rise.
Energy conservation is used to burn less fossil fuel. People can also use energy sources that don't burn fossil fuel, like hydrogen, solar panels or electricity from nuclear power or wind power. Or they can prevent the carbon dioxide from getting out into the atmosphere, which is called carbon capture and storage (CCS).
People can also change how they live because of any changes that global warming will bring. For example, they can go to places where the weather is better, or build walls around cities to keep flood water out. Like the preventive measures, these things cost money, and rich people and rich countries will be able to change more easily than the poor. Geoengineering is also seen by some as one climate change mitigation response. For example, a process using nanotechnology has been found to remove carbon dioxide from the air to create ethanol.
The term global warmingEdit
The English used in this article may not be easy for everybody to understand.
The term global warming was first used in its modern sense on 8 August 1975 in a science paper by Wally Broecker in the journal Science called "Climate Change: Are We on the Brink of a Pronounced Global Warming?". Broecker's choice of words was new and represented a significant recognition that the climate was warming; previously the phrasing used by scientists was "inadvertent climate modification," because while it was recognized humans could change the climate, no one was sure which direction it was going. The National Academy of Sciences first used global warming in a 1979 paper called the Charney Report, it said: "if carbon dioxide continues to increase, we find no reason to doubt that climate changes will result and no reason to believe that these changes will be negligible." The report made a distinction between referring to surface temperature changes as global warming, while referring to other changes caused by increased CO2 as climate change.
Global warming became more widely popular after 1988 when NASA climate scientist James Hansen used the term in a testimony to Congress. He said: "global warming has reached a level such that we can ascribe with a high degree of confidence a cause and effect relationship between the greenhouse effect and the observed warming." His testimony was widely reported and afterward global warming was commonly used by the press and in public discourse.
Effects of global warming on sea levelsEdit
Global warming means that Antarctica and Greenland ice sheets are melting and the oceans are expanding. The term "global warming" was created by Wallace Smith Broecker. Recent climate change would still cause a 6 meters (20 ft) sea-level rise even if greenhouse gas emissions were reduced in 2015 per a scientific paper in Science.
Cities affected by current sea level riseEdit
Many cities are sea ports and under threat of flooding if the present sea level rises.
- London 
- New York City
- Norfolk, Virginia, in Hampton Roads area of United States 
- Southampton 
- Crisfield, Maryland, United States 
- Charleston, South Carolina 
- Miami, Florida, has been listed as "the number-one most vulnerable city worldwide" in terms of potential damage to property from storm-related flooding and sea-level rise.
- Saint Petersburg 
- Sydney, Australia 
- Jakarta 
- Thatta and Badin, in Sindh, Pakistan 
- Malé, Maldives
- Mumbai, Buenos Aires, Los Angeles, Rio de Janeiro 
OECD 2007 REPORTEdit
From a 2007 OECD report
- Miami, USA
- Guangzhou, P.R. of China
- New York-Newark, USA
- Kolkata, India
- Shanghai, P.R. of China
- Mumbai, India
- Tianjin, P.R. of China
- Tokyo, Japan
- Hong Kong, P.R. of China
- Bangkok, Thailand
- Ningbo, P.R. of China
- New Orleans, USA
- Osaka-Kobe, Japan
- Amsterdam, The Netherlands
- Rotterdam, The Netherlands
- Ho Chi Minh City, Vietnam
- Nagoya, Japan
- Qingdao, China
- Virginia Beach, USA
- Alexandria, Egypt
Another seven cities that are exposed to coastal flooding:
- Rangoon, Myanmar
- Hai Phòng, Vietnam
- Khulna, Bangladesh
- Lagos, Nigeria
- Abidjan, Côte d'Ivoire
- Chittagong, Bangladesh
- Jakarta, Indonesia
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- IPCC (2018). "IPCC SR15 Summary for Policymakers 2018" (PDF). p. 6.
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- "Aerosols: Tiny Particles, Big Impact". earthobservatory.nasa.gov. 2010-11-02. Retrieved 2019-05-02.
- Harrison, Anna. "'No sudden jump in warming' from emissions cuts". www.leeds.ac.uk. Retrieved 2019-10-11.
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- McKie, Robin; editor, science (7 March 2009). "Scientists to issue stark warning over dramatic new sea level figures". Retrieved 23 January 2017 – via The Guardian.
- President Trump, Military Split on Climate Change at YouTube
- Floods in London.  Royal Geographical Society
- "Sea Level Rise - NYS Dept. of Environmental Conservation". New York State Department of Environmental Conservation. Retrieved 23 January 2017.
- interactive map from Climate Central
- "Mapping Sea Level Rise to Help Recovery after Hurricane Sandy". U.S. Global Change Research Program. Retrieved 23 January 2017.
- World Bank, World Development Report 2010, 91.
- Climate change in New York City
- Noguchi, Yuki (2014-06-24). "As Sea Levels Rise, Norfolk Is Sinking And Planning". NPR. Retrieved 2014-11-25.
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- Montgomery, David (2013-10-24). "Crisfield, Md., beats back a rising Chesapeake Bay". Washington Post. Retrieved 2013-10-27.
- Two cities, two very different responses to rising sea levels July 2, 2015 PBS NewsHour
- Jeff Goodell (June 20, 2013). "Goodbye, Miami". Rolling Stone. Retrieved June 21, 2013.
The Organization for Economic Co-operation and Development lists Miami as the number-one most vulnerable city worldwide in terms of property damage, with more than $416 billion in assets at risk to storm-related flooding and sea-level rise.
- Climate Change Economics February 2015 National Geographic
- "Coastal floods in Russia". Retrieved 23 January 2017.
- "Most at risk: Study reveals Sydney's climate change 'hotspots'". 29 April 2008. Retrieved 23 January 2017.
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