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Greenhouse Effect

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    Introduction

    The greenhouse effect is a natural process that regulates global warming. But as the number of greenhouse gases increases in the atmosphere, it results in what is known as global warming, which is one of the major problems facing the world today. We will discuss it briefly in the article below.

    The greenhouse effect is a natural substance that warms the surface of the earth. The atmosphere exists on earthworks as the surface of the glasshouse. When the sun’s rays reach the surface of the earth, 30% of the sun’s energy appears to return to the atmosphere. 21 per cent of this energy is absorbed by the atmosphere. The rest of the sun’s energy is absorbed by the oceans, vegetation, and other structures of our planet. This energy is absorbed into the earth by means of infrared waves that heat the Earth. Some gases in space are called ‘thermal gases’ because of their thermal conductivity. These gases absorb heat and return it to earth. The greenhouse gases are carbon dioxide, methane, water vapour, etc. These gases help keep the greenhouse temperature at about 30 ℃ higher than it would otherwise. Without the greenhouse effect, the earth would be too cold for life to thrive.

    Step 1: The sun’s rays reach the earth’s atmosphere. Some of this energy is also reflected in the atmosphere.

    Step 2: The remainder of the sun’s energy is absorbed by the oceans, plants, land, and other structures found on Earth.

    Step 3: Heat from Earth to the atmosphere.

    Step 4: Some of this heat is trapped by greenhouse gases in the atmosphere.

    Step 5: This keeps the earth warm enough to support life.

    Humans have increased levels of greenhouse gases through the use of fossil fuels such as coal and petroleum. This violates the balance maintained by the greenhouse effect, which results in an increase in the temperature of our earth’s atmosphere. Simply put, global warming refers to an increase in global warming. Global warming is a major problem facing the world today.

    Global Warming

    Greenhouse Gas

    Formula

    % on Earth

    Water vapour

    H2O

    35-70%

    Carbon Dioxide

    CO2

    9-25%

    Methane

    CH4

    4-9%

    Nitrous Oxide

    N2O

    3-7%

    We have always had greenhouse gases in the atmosphere. We take in oxygen and release carbon dioxide from our respiratory system. Plants take in carbon dioxide to make food through a process called photosynthesis. Once the forests have been cleared for human use, they no longer absorb carbon dioxide, and the gas begins to fill the air instead of accelerating crop growth. Thus, by cutting down trees, more carbon dioxide is added to the atmosphere. We have cut down forests for large parts of the planet that is to increase the number of greenhouse gases, and as a result, we have changed the temperature of the planet.

    We have burned a lot of fossil fuels. Thermal gases are also released when living things (including fuels that are still used such as oil or gas) are burned. These gases trap heat, trap heat in the Earth’s atmosphere.

    Effects of Global Warming

    Human activities such as the burning of minerals and deforestation increase the level of greenhouse gases that cause long-term global warming. This increase in man-made temperatures is often called global warming.

    Scientists are using the earth’s atmosphere, atmosphere, and atmosphere to monitor and evaluate climate change. The graph presented shows the change in global temperature.

    The effects of global warming are given below:

    • Year after year, recordings of the longest heatwaves affecting the stability of humans and other life forms on earth have been shattered.
    • Increased temperatures of melting glaciers and ice. This melting ice increases sea levels, leading to rising sea levels.
    • Extreme weather events such as hurricanes, droughts, and floods are becoming more frequent and more severe due to global warming.
    • Oceans have absorbed much of the extra heat and carbon dioxide so far. In addition to air, global warming contributes to the warming and acidity of the oceans. This poses a threat to marine ecosystems.
    • Extreme rainfall and extreme drought can cause water shortages.
    • Heat can lead to death and illness, especially for the elderly.
    • High temperatures and humidity can cause mosquito-borne diseases.

    Steps to Reduce Global Warming

    As we know, global warming is a major problem that poses a threat and a threat to all living systems. At the international level, various treaties, treaties and agreements have been signed to combat global warming by increasing international cooperation. But in addition to governments trying to solve this problem, man must also learn to take responsibility for his actions and need to take small steps on a personal level to reduce the total emissions of greenhouse gases to make the planet better and healthier.

    As individuals, we can do the following:

    • Use bicycles instead of short-distance vehicles.
    • Plant more trees by organizing community events and planting trips.

    A greenhouse effect is a process that occurs when energy from the sun’s rays passes through its atmosphere and warms the surface of the planet, but the atmosphere prevents heat from returning directly to the atmosphere, resulting in a warm planet.

    FAQ’s

    How Much of global warming is responsible for sea-level rise?

    As the earth's atmosphere warms, ice in the cooler climate melts rapidly. Glaciers can recede. This melting factor contributes to rising sea levels. The upper layer of the sea will also be warm. Water grows when heated. This increase contributes to rising sea levels, which can lead to drowning and submerging coastal areas.

    Do All Greenhouse Gases Have the Same Capacity of Heat?

    No, greenhouse gases differ in their heat-holding capacity. Each gas has different radioactive properties, normal life span and atmospheric concentration, etc. For various thermal gases, the heat of a home heater is calculated depending on its concentration in the atmosphere and how long it is likely to stay there. High-pressure greenhouse gases will have the ability to trap heat and vice versa.

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