The Deadly Cycle – How Global Warming Causes Global Warming

16 08 2009

The Deadliest Cycle – How Global Warming Causes Global Warming

It is a process known as “feedback”. This process involves some sort of action or event which triggers another event which worsens the first event leading to another secondary event which worsens the first event even more. Confusing? I’ll explain.

A good example of feedback is the melting of the polar ice caps and it’s involvement with global warming. The ice naturally reflects heat energy in the form of radiation back into space. As the ice melts, it covers less area and reveals more water coverage. Less ice enhances the atmospheres heat energy (ice cools air just like it cools your summer drinks). With less ice, the remaining ice melts faster revealing yet more water. Water absorbs heat energy instead of reflecting it. This causes the ice to melt even faster.

There are several types of natural “feedback”: Ice Albedo feedback, water vapor feed back, arctic methane feedback, lapse rate feedback and more. These feedback types enhance global warming and are also, simultaneously, caused by global warming to some extent.

Ice Albedo Feedback

As discussed earlier, Ice Albedo Feedback involves the fact ice reflects more radiation than it absorbs. When ice melts it is replaced by land or water which absorbs more than it reflects. This causes more heat absorption which causes more ice melting which causes yet more absorption. This cycle is never-ending unless affected by an outside source.
Northern Hemisphere Glacial Regression

Water Vapor Feedback
Water Vapor is a Greenhouse Gas. As the earth warms, more water is evaporated leading to more water vapor. More water vapor leads to more warming which leads to more evaporation thus more water vapor. This cycle is never-ending unless affected by an outside source.

Lapse Rate Feedback
Temperature differences between the lower atmosphere and upper atmosphere is called the Lapse Rate. The higher the temperature of the upper atmosphere, the more radiation is emitted. Thus, if the upper atmosphere (which is supposed to be cold) is heated, it emits much more radiation than if it were cold. This cycle is never-ending unless affected by an outside source.

Methane Release
Warming of the earth has effects both on land and in the ocean in the form of methane release. As the earth’s temperature increases, certain areas of permafrost on the earth melt releasing long frozen and stored methane gas, which in turn, causes more warming since it’s considered a greenhouse gas. This cycle is never-ending unless affected by an outside source.

Cloud Feedback
Some types of clouds, particularly cumulus, are expected to increase in frequency and coverage in the future due to warming and higher, faster evaporation rates. Clouds of this type tend to reflect radiation back down to the ground thus enhancing the lower atmosphere’s ability to retain heat. This increases the earth’s temperature even more causing more cumulus clouds and more back-to-earth radiation reflection. This cycle is never-ending unless affected by an outside source.

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A Synopsis on Climate Change

15 08 2009

There has been skepticism during the entire lifetime of the theoretical atmospheric anomaly called “Global Warming”. Global Warming is a term coined to describe the unnatural rise of the mean low-level atmosphere temperature over a period of time called climate. Global Warming has also been described as Climate Change although it is not a deserved alias as the earth’s climate often changes in temperature over long periods of time (see ice ages and medieval warming). As such, Global Warming should have been coined as the 21st century Global Warming Trend instead of its current names.

Cycle of Greenhouse Gases

The evidence of Global Warming has seemed to pile-up over the time span of its coined existence. This could be due to the fact that more investigations into the global climate heating has resulted in both expected and unexpected evidence and it could be a result of ongoing changes that take place in real time such as the breaking off and thinning of glaciers. Some of the evidence already observed include a research study by various scientists and reported by the Intergovernmental Panel on Climate Change (IPCC) include a global mean temperature increase of 0.74 ± 0.18 °C (1.33 ± 0.32 °F) over the period of the last century although it seems variations in solar radiation and volcanic activity was the primary contributors before the pre-industrial times before 1950.

Temperature Changes
It is forecasted by the IPCC that the global mean temperature could increase yet another 1.1 to 6.4 °C (2.0 to 11.5 °F) by 2100. The uncertainty in the predicted temperature increases is partially due to the fact that different models have forecasted different amounts of chemicals such as Carbon Dioxide in the atmosphere during varying spans of time. The prediction of 2 °F is a conservative guess but the 11.5 °F increase is also quite possible and would be, of course, the worst case scenario.

Temperature History

The NASA Goddard Space Institute estimated that 2005 was the warmest year globally since dependable and accurate modern satellite temperature monitoring began, exceeding the previous record established in 1998 by only a few hundredths of a degree. The high temperatures recorded in 1998 is thought to be a result of an unusually strong El Niño event – the strongest in over a century.

Since global temperatures have been monitored and recorded, various global locations seem to heat faster than others such as the difference in ocean temperatures relative to land-based atmosphere temperatures. Ocean temperatures rise approximately 0.13 °C relative to land-based atmosphere temperatures which rise an average of 0.25 °C during the course of a decade. Many factors contribute to the difference in temperature increases including the ocean having a vast depth and spread in which temperature is required to increase as well as the effect of evaporation on the air above the ocean. Liquids warm and cool much slower than the air, being more dense, thus the difference in temperature fluctuations. Also, the north hemisphere would warm much faster than the southern hemisphere mainly due to the fact that the northern hemisphere has more land area than does the south. With upper air currents in combination with the difference in temperature, the polar regions would heat much faster than regions closer to the equator, thus the rapid warming and thinning of the polar ice caps in the Arctic and Antarctic Circles. Due to the heat-retaining capacity of the oceans as well as the lifespan of Carbon Dioxide, even if all emissions were to cease the global temperature would continue to rise well after 2100.

Global Warming Projections

Another area which affects the global mean temperature is the effects of “Greenhouse Gases” originally discovered and coined by Joseph Fourier in 1824 and was first investigated quantitatively by Svante Arrhenius in 1896. “Greenhouse Gases” are gases which emit and absorb infrared radiation in the planets atmosphere and enhance the atmosphere’s ability to withhold heat energy. “Greenhouse Gases” include but are not limited to: Water Vapor, Methane, Carbon Dioxide, Nitrous Oxide and Tropospheric Ozone. Higher concentrations of these gases lead to the planet’s atmosphere retaining more heat than it exerts thus raising the global mean temperature. Since the industrial revolution, global carbon dioxide levels have increased by 36% – ¾ of the increase is suspected to be a direct result of the burning of fossil fuels. Evidence extracted from deep ice pockets suggest that carbon dioxide levels are higher than they have been in the last 650,000 years – additional evidence is believed to indicate that levels are actually higher than they have been in the last 20 million years. Although most of the gases mentioned enhance the planets ability to retain heat, some chemicals known as aerosols which are either released naturally, as is the case with volcanoes, or by human sowing as is the case with some CFCs. These chemicals reflect radiation back into space from the upper atmosphere countering the effects of “Greenhouse Gases”. Although this may have been the case up until now, it seems as if the amount of “Greenhouse Gases” such as carbon dioxide and methane are well exceeding the amount of aerosol in the atmosphere. This may have been the reason that extreme global mean temperature increase was delayed during the latter half of the 20th century and only become urgent from the beginning of the new millennium onward. Methods have also been used by scientists to combat global warming indirectly and directly including the use of Biochar, Geoengineering and the like.

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