mis course hero what is global warming?

by John King 4 min read

Whats is global warming?

Global warming is the long-term heating of Earth's climate system observed since the pre-industrial period (between 1850 and 1900) due to human activities, primarily fossil fuel burning, which increases heat-trapping greenhouse gas levels in Earth's atmosphere.

What is global warming in class?

Answer: Global warming is the unnatural rise in the temperature of the earth's surface due to increased amounts of green house gases in the earth's atmosphere.

What is global warming in detail Class 10?

Introduction: Global Warming means gradual increase in world's temperature caused by greenhouse gases. The impact of global warming can be seen in sea level, crops, rainfall, and human health.

What is global warming study com?

Global warming simply means an increase in the average temperature of the earth's atmosphere near its surface - either from natural or human causes - that may result in a change in global climate patterns.Aug 19, 2021

What is global warming 8th answer?

Global Warming Questions And Answers Class 8th. The term global warming refers to the general increase in the average temperature of the earth caused by the presence of greenhouse gasses in the atmosphere, causing changes in climate patterns throughout the globe.Jan 17, 2021

What is global warming essay?

Essay On Global Warming in 300 Words. Global warming is a phenomenon where the earth's average temperature rises due to increased amounts of greenhouse gases. Greenhouse gases such as carbon dioxide, methane and ozone trap the incoming radiation from the sun.

What is global warming Slideshare?

GLOBAL WARMING. Global warming is the increase in average temperature of the earths near surface air and oceans. Most of the observed temperature increase is caused by increased concentration of greenhouse gases Major gases water vapor – 36-70% carbon dioxide- 9 – 26 % methane - 4- 9 % ozone -3–7% GREEN HOUSE EFFECT.

What is global warming for kids?

Global warming is a process that causes the Earth to become hotter. Most of the evidence causing the increase in temperature is from human activity. These activities such as driving cars, using fossil fuels, working in factories and agriculture, cause an increase in the gases that keep the Earth warm.Jun 12, 2021

What is global warming definition PDF?

Global Warming is defined as the increase of the average temperature on Earth. As the Earth is getting hotter, disasters like hurricanes, droughts and floods are getting more frequent.

What is example of global warming?

The rate at which sea levels are rising throughout the world is increasing. This is due to both the melting of glaciers and the thermal expansion of the oceans as they absorb atmospheric heat increases caused by emissions. Widespread decreases in the extent of snow and ice is an example of global warming.

How does global warming work simple?

Global warming is caused by an increase in the greenhouse effect. The greenhouse effect occurs when certain gases in the atmosphere trap heat. These gases prevent the heat from escaping back into the space. The more greenhouse gases are in the atmosphere, the more heat gets trapped.

What are the five examples of global warming?

These phenomena include the increased temperature trends described by global warming, but also encompass changes such as sea-level rise; ice mass loss in Greenland, Antarctica, the Arctic and mountain glaciers worldwide; shifts in flower/plant blooming; and extreme weather events.”Apr 27, 2020

Environment

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Global warming is the unusually rapid increase in Earths average surface temperature over the past century primarily due to the greenhouse gases released by people burning fossil fuels. Global warming is the unusually rapid increase in Earths average surface temperature over the past century primarily due to the gre…
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Climate

  • Earth has experienced climate change in the past without help from humanity. But the current climatic warming is occurring much more rapidly than past warming events. As the Earth moved out of ice ages over the past million years, the global temperature rose a total of 4 to 7 degrees Celsius over about 5,000 years. In the past century alone, the temperature has climbed 0.7 degre…
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Setting

  • In Earths history before the Industrial Revolution, Earths climate changed due to natural causes unrelated to human activity. These natural causes are still in play today, but their influence is too small or they occur too slowly to explain the rapid warming seen in recent decades.
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Models

  • Models predict that as the world consumes ever more fossil fuel, greenhouse gas concentrations will continue to rise, and Earths average surface temperature will rise with them. Based on plausible emission scenarios, average surface temperatures could rise between 2°C and 6°C by the end of the 21st century. Some of this warming will occur even if future greenhouse gas emis…
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Impact

  • The impact of global warming is far greater than just increasing temperatures. Warming modifies rainfall patterns, amplifies coastal erosion, lengthens the growing season in some regions, melts ice caps and glaciers, and alters the ranges of some infectious diseases. Some of these changes are already occurring.
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Mechanism

  • Earths temperature begins with the Sun. Roughly 30 percent of incoming sunlight is reflected back into space by bright surfaces like clouds and ice. Of the remaining 70 percent, most is absorbed by the land and ocean, and the rest is absorbed by the atmosphere. The absorbed solar energy heats our planet. As the rocks, the air, and the seas warm, they radiate heat energy (thermal infr…
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Function

  • When they absorb the energy radiating from Earths surface, microscopic water or greenhouse gas molecules turn into tiny heaters like the bricks in a fireplace, they radiate heat even after the fire goes out. They radiate in all directions. The energy that radiates back toward Earth heats both the lower atmosphere and the surface, enhancing the heating they get from direct sunlight.
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Research

  • See the Earth Observatorys series Paleoclimatology for details about how scientists study past climates.
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Timeline

  • Using this ancient evidence, scientists have built a record of Earths past climates, or paleoclimates. The paleoclimate record combined with global models shows past ice ages as well as periods even warmer than today. But the paleoclimate record also reveals that the current climatic warming is occurring much more rapidly than past warming events.
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Causes

  • These natural causes are still in play today, but their influence is too small or they occur too slowly to explain the rapid warming seen in recent decades. We know this because scientists closely monitor the natural and human activities that influence climate with a fleet of satellites and surface instruments. Scientists theorize that there may be a multi-decadal trend in solar out…
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Applications

  • Scientists integrate these measurements into climate models to recreate temperatures recorded over the past 150 years. Climate model simulations that consider only natural solar variability and volcanic aerosols since 1750omitting observed increases in greenhouse gasesare able to fit the observations of global temperatures only up until about 1950. After that point, the decadal trend …
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Characteristics

  • Each cycle exhibits subtle differences in intensity and duration. As of early 2010, the solar brightness since 2005 has been slightly lower, not higher, than it was during the previous 11-year minimum in solar activity, which occurred in the late 1990s. This implies that the Suns impact between 2005 and 2010 might have been to slightly decrease the warming that greenhouse emi…
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Purpose

  • To further explore the causes and effects of global warming and to predict future warming, scientists build climate modelscomputer simulations of the climate system. Climate models are designed to simulate the responses and interactions of the oceans and atmosphere, and to account for changes to the land surface, both natural and human-induced. They comply with fun…
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Example

  • Perhaps the most well known feedback comes from melting snow and ice in the Northern Hemisphere. Warming temperatures are already melting a growing percentage of Arctic sea ice, exposing dark ocean water during the perpetual sunlight of summer. Snow cover on land is also dwindling in many areas. In the absence of snow and ice, these areas go from having bright, sun…
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Introduction

  • The question that scientists ask is, how much water vapor will be in the atmosphere in a warming world? The atmosphere currently has an average equilibrium or balance between water vapor concentration and temperature. As temperatures warm, the atmosphere becomes capable of containing more water vapor, and so water vapor concentrations go up to regain equilibrium. Wil…
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Advantages

  • The amount of water vapor that enters the atmosphere ultimately determines how much additional warming will occur due to the water vapor feedback. The atmosphere responds quickly to the water vapor feedback. So far, most of the atmosphere has maintained a near constant balance between temperature and water vapor concentration as temperatures have gone up in r…
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Effects

  • If clouds become brighter, or the geographical extent of bright clouds expands, they will tend to cool Earths surface. Clouds can become brighter if more moisture converges in a particular region or if more fine particles (aerosols) enter the air. If fewer bright clouds form, it will contribute to warming from the cloud feedback.
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Formation

  • Clouds, like greenhouse gases, also absorb and re-emit infrared energy. Low, warm clouds emit more energy than high, cold clouds. However, in many parts of the world, energy emitted by low clouds can be absorbed by the abundant water vapor above them. Further, low clouds often have nearly the same temperatures as the Earths surface, and so emit similar amounts of infrared en…
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Benefits

  • If warmer temperatures result in a greater amount of high clouds, then less infrared energy will be emitted to space. In other words, more high clouds would enhance the greenhouse effect, reducing the Earths capability to cool and causing temperatures to warm.
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Future

  • Scientists arent entirely sure where and to what degree clouds will end up amplifying or moderating warming, but most climate models predict a slight overall positive feedback or amplification of warming due to a reduction in low cloud cover. A recent observational study found that fewer low, dense clouds formed over a region in the Pacific Ocean when temperature…
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