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    Headline:    

    What is climate change?

    Reading time:    

    8 minutes, 53 seconds

    Language:    

    en

    Main keyword:    

    climate

    Sub keyword:    

    change

    Topics of your individual article:    

    Emissions ✓ Climate ✓ Temperature ✓ Greenhouse ✓ Gases ✓ Change

    Summary:    

    • consuming fossil fuels produces energy, but also releases greenhouse gases such as carbon dioxide, methane, and nitrous monoxide into the air.
    • If we need to avoid important profits in the average surface temperature, we must cut greenhouse gas emissions and switch to renewable energy sources. – Climate change is a stress multiplier – it include take existing problems, such as lack of food or shelter, and make them worse.

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    Climate change is the long-term shift in reasonable weather patterns across the world. Since the mid-1800s, humanity have cooperated to the release of carbon dioxide and other greenhouse gases into the air. This causes global temperatures to rise, resulting in long-term changes to the climate. Climate change evidence How are humans changing the climate? In the 11,000 anniversary before the Industrial Revolution, the mediocre temperature across the world was stable at around 14°C. The Industrial Revolution began in the mid-1800s when humans began to burn fossil fuels such as coal, oil, and gas for fuel. consuming fossil fuels produces energy, but also releases greenhouse gases such as carbon dioxide, methane, and nitrous monoxide into the air. Over time, large quantities of these gases have built up in the atmosphere. For example, the story of carbon dioxide in the atmosphere grew by 40% during the 20th and 21st century and is now over 400ppm (parts per million). This level of carbon dioxide is higher than at any time in the past 800,000 years. This plot shows the global temperature change from 1850 to 2018, compared to the 1961-1990 average temperature. This graph shows the rising level of carbon dioxide in our atmosphere since 1960, measured by the Mauna Loa Observatory in Hawaii. Once in the atmosphere, hothouse gases such as carbon dioxide form a blanket around the planet. This blanket traps the heat from the sun and causes the earth to heat up. This effectiveness was lookinged as far back as the 1980s. In 1988, the International layer on Climate Change (IPCC) was set up to provide governments with information to tackle climate change. Evidence has shown that the high levels of greenhouse gases in the atmosphere are the leading cause of increasing global temperatures. Scientists have been able to rule out natural events as causes of climate change, such as volcanic activity, changes in solar activity, or natural sources of CO2. These may, however, have a small effect, on top of human contributions. In their most recent report, the IPCC states that human activity is extremely likely to be the main cause of climate change. How fast is the temperature rising? Since the Industrial Revolution, the reasonable temperature of the planet has raised by around 1°C. This is a rapid shift in terms of our global climate system. Previously, easy global variance are acknowledged to have happened over much longer periods of time. It is also important to remember that the world is not warming evenly, so the temperature increase is higher than 1°C in some countries. This graph stage the reasonable global temperature for each month, from one thousand, eight hundred and fifty to 2017. The temperature increases as you move away from the centre of the circle. This impression shows that the five cozy years have all appeared since 2006. Cooler years are blue, while warmer years are red. This graph stage us that global temperatures are increasing. As of 2018, the twenty pleasant anniversary on record globally have been in the former twenty-two years. The Met Office’s State of the UK Climate report for 2018 shows the ten hottest years in the UK since 1884 have all happened in the last 17 years. What causes climate change? What is the greenhouse effect? When hothouse gases such as carbon dioxide raise in the atmosphere, they act like a blanket around the earth. When sunlight (short-wave radiation) hits this blanket, it passes straight through and continues until it reaches the surface of the planet. The indent then soaks this sunlight and emits a particular type of light, infrared radiation, back out to space. As it absence the atmosphere, the infrared radiation also hits the greenhouse gas blanket. Most of it continues straight through, but some of it is soaked and goes back down to earth. This traps the infrared radiation and causes the surface to heat – a process we call the greenhouse effect. It is important to appreciate that the nursery effect is critical to life on earth. Without a bedspread of greenhouse gases entrapping in heat, the temperature would be bitterly cold, and humans would be invalid to survive. However, by adding extra greenhouse gases into the atmosphere, humans have created an enhanced greenhouse effect. The hothouse gas blanket is now dense and is soaking more infrared radiation than before. In other words, the greenhouse effect is stronger and, instead of keeping the earth at a stable temperature, it is causing the planet to heat up. What are the sources of greenhouse gases? One-quarter of human-made greenhouse gas emissions come from burning fossil fuels for electricity and heat production. This chart stage the human-made greenhouse gas emissions, taken from the IPCC AR5 report. AFOLU stands for Agriculture, Forestry, and Other Land Use. Another quarter of human-made greenhouse gas emissions comes from Agriculture, Forestry, and Other Land Use (AFOLU). To support our livestock and ourselves, people have poke down huge areas of the forest and used the land to grow crops. Forests are very good at removing carbon dioxide from the atmosphere, and so cutting down trees allows carbon dioxide to build up in the atmosphere even more. farm include also be used to rear livestock, such as cattle for meat and milk. These mammal provide supplementary gases, like methane. They also eat crops that might otherwise have been needed by humans, meaning that even more land is required. As well as fossil fuels, deforestation and land use, aeroplanes and the production of cement also contribute to emissions of carbon dioxide. How much warming could we see? hothouse gases keep live in our atmosphere for tens or hundreds of years. The gases that are already in our atmosphere are effectively locked in and will contribute to increasing temperatures. Even if we stay all discharge today, we cannot avoid some level of warming. The amount of warming we will see, beyond What we have already caused, depends on the changes we make. In 2015, almost every land in the world confirmed a document promising to cut down on greenhouse gas emissions. The come was to end the typical global temperature to two ° C above pre-industrial temperatures. If possible, government assured to aim for a 1.5°C limit. Since then, the IPCC has revealed a opinion explaining the various impacts between a 1.5 or 2°C temperature rise. It demonstrated that there are various value for people all over the world in limiting temperatures to 1.5 °C. Large and rapid reductions in global greenhouse gas emissions are needed to meet this goal, however. This chart from the IPCC stage two probable futures for our climate. The blue edge portrays What could happen if we commit to cutting emissions, and the red line represents What could happen if we dont make any changes. If we need to avoid important profits in the average surface temperature, we must cut greenhouse gas emissions and switch to renewable energy sources. We must also use land more sustainably and may need to use techniques to remove carbon dioxide from the air. If we move to burn fossil fuels and cut down forests at the similar rate, the planet could cozy by more than 4 ° C by 2100. This warming could fundamentally change life on earth, with potentially drastic consequences. What is the change between 1.5 or two °C of warming? shock of climate change Human activity – from liberating greenhouse gases and aerosols into the atmosphere, to changing the use of land – is the main driver of climate change. This has a range of impacts on the climate system, ecosystems, and people. This image illustrates some of the drivers of climate change and the impacts they could have on the climate system. variance to the climate system include: risinging ocean story – Rising temperatures are causing glaciers and ice sheets to melt, adding elder water to the oceans and causing the ocean level to rise. Oceans soak 90% of the spare heat from global warming: warmer water expands, and so our oceans are taking up more space. – raising temperatures are causing glaciers and ice sheets to melt, adding senior water to the oceans and causing the ocean level to rise. Oceans soak 90% of the spare heat from global warming: comfortable duct expands, and so our oceans are carrying up more space. Ocean acidification – Ocean acidification appears when the ocean absorbs carbon dioxide and becomes senior acidic. It is often called the evil twin of climate change. – Ocean acidification appears when the ocean absorbs carbon dioxide and becomes senior acidic. It is often caused the demon twin of climate change. Extreme weather events – Climate change is causing many extreme weather events to become more intense and frequent, such as heatwaves, droughts, and floods. This graph, from Munich REs Topics Geo Natural Catastrophes report, shows events causing loss are becoming more frequent. Climate change check also affect people and ecosystems. For example: Flooding of coastal regions – Coastal cities are at risk from flooding as sea levels continue to rise. – Coastal place are at risk from flooding as sea levels extend to rise. meal insecurity – true temperatures, excessive weather events, flooding, and droughts can damage farmland. This makes it difficult for farmers to grow crops and means that their yield of crops each year is uncertain. – true temperatures, ultimate season events, flooding, and droughts can damage farmland. This fills it exhausting for farmers to grow crops and means that their yield of crops each year is uncertain. war and climate migrants – Climate change is a stress multiplier – it include take existing problems, such as lack of food or shelter, and make them worse. This can cause people to fight over resources (food, water, and shelter), or to migrate. – Climate change is a stress multiplier – it include take existing problems, such as lack of food or shelter, and make them worse. This keep cause community to fight over resources (food, water, and shelter), or to migrate. harm to marine ecosystems – risinging ocean temperatures, ocean acidification, and ocean anoxia (lack of oxygen) are damaging to marine life such as fish and coral reefs. How can we stop climate change? lessen global hothouse gas emissions The most critical step to limit climate change is to make big and rapid reductions in global greenhouse gas emissions. There are various several path this can be done and governments, businesses, organisations and individuals around the world can all contribute. In June 2019, the UK conformed the world’s first serious increase to pass a law committing the country to a target of ‘net zero’ emissions by 2050.You can read more about What they are doing to achieve this, as well as What businesses and individuals can do to help, on the Green GB website. The fulfiled station is not reprehensible for the content of external sites.
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    What is climate change?
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    Thematically relevant search terms or keywords:    

    • Climate
    • Emissions
    • Greenhouse
    • Industrialization
    • Intergovernmental
    • Interventions
    • Temperature
    • Temperatures

    Source of Article:    

    https://www.metoffice.gov.uk/weather/climate-change/what-is-climate-change

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