An overview of the global warming and the greenhouse effect

History of climate change science The existence of the greenhouse effect was argued for by Joseph Fourier in The argument and the evidence were further strengthened by Claude Pouillet in and and reasoned from experimental observations by John Tyndall inwho measured the radiative properties of specific greenhouse gases. Most of the remaining energy is absorbed at the surface of Earth. Because the Earth's surface is colder than the Sun, it radiates at wavelengths that are much longer than the wavelengths that were absorbed.

An overview of the global warming and the greenhouse effect

Share Understanding Global Warming Potentials Greenhouse gases GHGs warm the Earth by absorbing energy and slowing the rate at which the energy escapes to space; they act like a blanket insulating the Earth.

Different GHGs can have different effects on the Earth's warming. Two key ways in which these gases differ from each other are their ability to absorb energy their "radiative efficiency"and how long they stay in the atmosphere also known as their "lifetime".

The time period usually used for GWPs is years. GWPs provide a common unit of measure, which allows analysts to add up emissions estimates of different gases e.

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CO2, by definition, has a GWP of 1 regardless of the time period used, because it is the gas being used as the reference. CO2 remains in the climate system for a very long time: CO2 emissions cause increases in atmospheric concentrations of CO2 that will last thousands of years.

Inventory of Greenhouse Gas Emissions and Sinks uses a different value. The net effect of the shorter lifetime and higher energy absorption is reflected in the GWP. N2O emitted today remains in the atmosphere for more than years, on average.

The GWPs for these gases can be in the thousands or tens of thousands.

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Why are GWPs presented as ranges? In the most recent report by the Intergovernmental Panel on Climate Change IPCCmultiple methods of calculating GWPs were presented based on how to account for the influence of future warming on the carbon cycle.

For this Web page, we are presenting the range of the lowest to the highest values listed by the IPCC. The Inventory also presents emissions by mass, so that CO2 equivalents can be calculated using any GWPs, and emission totals using more recent IPCC values are presented in the annexes of the Inventory report for informational purposes.

However, the scientific community has developed a number of other metrics that could be used for comparing one GHG to another.

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These metrics may differ based on timeframe, the climate endpoint measured, or the method of calculation. Just like the year GWP is based on the energy absorbed by a gas over years, the year GWP is based on the energy absorbed over 20 years.

This year GWP prioritizes gases with shorter lifetimes, because it does not consider impacts that happen more than 20 years after the emissions occur. While the GWP is a measure of the heat absorbed over a given time period due to emissions of a gas, the GTP is a measure of the temperature change at the end of that time period again, relative to CO2.

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The calculation of the GTP is more complicated than that for the GWP, as it requires modeling how much the climate system responds to increased concentrations of GHGs the climate sensitivity and how quickly the system responds based in part on how the ocean absorbs heat.

Contact Us to ask a question, provide feedback, or report a problem.The Earth's climate has changed throughout history.

We call the result global warming, but it is causing a set of changes to the Earth's climate, or long-term weather patterns, that varies from place to place. As the Earth spins each day, the new. A Brief History of Ice Ages and Warming. Global warming started long before the "Industrial Revolution" and the invention of the internal combustion ashio-midori.com warming began 18, years ago as the earth started warming its way out of the Pleistocene Ice Age-- a time when much of North America, Europe, and Asia lay buried beneath great sheets of glacial ice. Greenhouse Gases (GHG's) are the various gases that block outgoing long-wave infrared from easily leaving our atmosphere. The Greenhouse Effect (GHE) is the physical mechanism of this blocking mechanism in our atmosphere that influence how much heat we retain within the atmosphere.

Just in the last , years there have been seven cycles of glacial advance and retreat, with the abrupt end of the last ice age about 7, years ago marking the beginning of the modern climate era — and of human civilization. The greenhouse effect is the process by which radiation from a planet's atmosphere warms the planet's surface to a temperature above what it would be without its atmosphere..

If a planet's atmosphere contains radiatively active gases (i.e., greenhouse gases) they will radiate energy in all ashio-midori.com of this radiation is directed towards the surface, warming it. Greenhouse Gases (GHG's) are the various gases that block outgoing long-wave infrared from easily leaving our atmosphere.

The Greenhouse Effect (GHE) is the physical mechanism of this blocking mechanism in our atmosphere that influence how much heat we retain within the atmosphere.

Carbon dioxide (CO 2) is the primary greenhouse gas emitted through human ashio-midori.com , CO 2 accounted for about % of all U.S. greenhouse gas emissions from human activities.

Carbon dioxide is naturally present in the atmosphere as part of the Earth's carbon cycle (the natural circulation of carbon among the atmosphere, oceans, soil, plants, and animals). An Overview of Global Warming.

Global warming refers to the increase in the earth's average temperature that occurs naturally or, as theorized in recent years, is induced by human activity.

An overview of the global warming and the greenhouse effect

Most discussions on global warming today cite a correlation between an increase in global temperature and the increase in carbon dioxide, nitrous oxide, . For each greenhouse gas, a Global Warming Potential (GWP) has been calculated to reflect how long it remains in the atmosphere, on average, and how strongly it absorbs energy.

Gases with a higher GWP absorb more energy, per pound, than gases with a lower GWP, and thus contribute more to warming Earth.

Climate Change and Global Warming Introduction — Global Issues