Global Warming Effects
Glaciers are melting, sea level is increasing, cloud forests are dying, and wildlife is scary to maintain the pace. It is being clarified that by releasing heat-trapped gas due to the power of our modern life, humans have made the most hot heat of the past. Called greenhouse gas, their levels are higher than the last 650,000 years.
We call the result of global warming, but it is making a cause for a change in the climate of the Earth, or long-term weather patterns, which vary in place from place to place. As the earth spins every day, new heat goes into it with vapor, the oceans get moisture, rising here, standing there. It’s changing the rhythm of the climate that relies on all living things.
What do we do to reduce this heat? How do we cope with the changes already with the introduction? When we struggle to evacuate it, when we know that the face of the Earth, along with the coastline, the forests, fields and the mountains surrounded by snow – stop in balance.
“Greenhouse effect” occurs when there is some heat in the atmosphere in the Earth’s atmosphere. These gases allow light to come, but like greenhouses glass walls, keep heat from rising.
First of all, sunlight shines on the surface of the Earth, where it absorbs and then spreads back to the atmosphere as heat. In the atmosphere, “greenhouse” gas snatches this heat and survives in the remaining space. More greenhouse gases are in the atmosphere, more heat is not trapped.
Scientists know about the greenhouse effect from 1824, when Joseph Fourier calculated that the Earth would be much cooler if it was not in the atmosphere. This greenhouse effect is those that keep the Earth’s climate alive. Without that, the surface of the Earth will be an average of about 60 degrees Fahrenheit cooling.
In 1895, Swedish chemist Swanette Ernius discovered that humans could increase the greenhouse effect by making carbon dioxide, greenhouse gases. He started climate research for 100 years, which gave us a modern understanding of global warming.
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The level of greenhouse gas (GHG) has increased above and below the history of the Earth, but for the past several thousand years. They have remained steadily stable. The average global temperature has remained steady during that time, until recently. By burning fossil fuels and other GHG emissions, humans are heating the greenhouse effect and the earth.
Scientists often use the term “climate change” rather than global warming. This is because the Earth’s average temperature is high, wind and ocean currents raise heat worldwide, which can cool some areas, others can heat up and the amount of rain and ice can decrease. As a result, the climate varies in different areas in different areas.
Is not the temperature changing?
The average global temperature and concentration of carbon dioxide vary from cycle to hundreds of years because the Earth’s position differs from the Sun. As a result, the ice age has come and gone.
However, for thousands of years, GHG emissions in the atmosphere are done by greenhouse gases that are naturally absorbed. As a result, GHG concentrations and temperatures are fairly stable. This stability has allowed human culture to be developed in constant climates.
Occasionally, other factors influence global temperatures globally. Volcanic eruption, for example, releases particles which temporarily freeze the surface of the Earth. But these have no permanent effect for a few years. Other chakras, such as El Nino, also work on a fairly short and predictable cycle.
After the Industrial Revolution, humans now have increased the amount of carbon dioxide in the atmosphere by a third. These major changes have been taken historically for thousands of years, but now the president of the decade is taking place.
Why Is This A Concern?
The rapid increase in greenhouse gases is a problem because the climate is changing rapidly because some live things may adopt. Besides, a new and more precise environment has unique challenges for all life.
Historically, the climate of the Earth is regularly transmitted forward and backward, as we see today and the temperature is as cold as the large sheet of ice is covered in North America and Europe. The average global temperature is between 5 and 9 degrees Fahrenheit (9 degrees Fahrenheit) during the glacial period, and this swing is gradual, for thousands of years
Now, with the concentration of greenhouse gases. The rest of the earth’s ice content (such as Greenland and Antarctica) also melt. Excess water can potentially increase sea levels significantly
As the mercury grows, the climate may change unexpectedly. With the rise of sea level, the weather can more extreme. This means that a more intense major storm, more rain is followed by a long and dry drought. Changes in the range in which plants and animals can live, and water supply loss, which historically comes from glaciers
Global Warming Solution
The evidence is that humans are the reason for global warming. But the question of what to do about it is controversial. Economics, sociology, and politics are all important factors for future planning.
Even if we stop the emissions of greenhouse gases (GHG) today. The earth will still be warmer than the second degree Fahrenheit. But what we do today makes a big difference. Based on our preferences, scientists predict that the Earth can be warmer than 2.5 degrees or 10 degrees Fahrenheit.
A commonly cited goal is to make the GHG concentration stable about 450-550 parts per million (PPM), or twice of industrial levels. This is an issue in which many believe that the most harmful effects of climate change can avoided. The current concentration is approximately 380 ppm, which means there is not much time to lose. According to IPCC. We have to reduce GHG emissions by 50% to 80% in the next century to reach this level.
Is This Possible?
Researchers Stephen Pekala and Robert Solcollo at Princeton University have suggested that they “stabilization wedges”. This means that instead of relying on the huge change in an area. Reducing GHG emissions by the various technologies available in the next few decades. They suggest that each emission reduction reduces seven shovels. Together they all can catch emissions at the current level for the next 50 years, putting us on a potential path to freeze around 500 ppm.
Energy efficiency and improvements in vehicle fuel economy, wind and solar power increase, hydrogen produced from renewable sources. Biofuels (produced from crops), natural gas and molecular power are many possible electrical holes. There is also the ability to extract carbon dioxide from fossil fuels. And store it in the underground – a process called “carbon alert”.
Apart from reducing the gas, we exit the atmosphere. We can also increase the amount of gas emitted from the atmosphere. Plants and trees absorb CO2 because it grows, increasing the “sequestration” forests of carbon naturally. And the way we change the farm, we can increase the amount of carbon we are storing.
Some of these techniques have defects, and different parts of the world will choose to rely on certain types of energy. But there are different options for putting us on the path towards a stable climate.
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