One of the strongest pieces of evidence for human-induced climate change is the consistent rise in carbon dioxide (CO2) in modern times, as measured at the Mauna Loa Observatory in Hawaii, where CO2 has been observed since 1958. As of 2005, the concentration of CO2 in Earth’s atmosphere was about 378 parts per million (ppm).

CO2 lifetime in the atmosphere can range from 50-200 years. Once it enters the atmosphere, there is very little that can be done to reduce carbon dioxide in the atmosphere.

C02 is naturally released into the air from rotting or burning trees and plants. When it is released, some C02 stays in the air for a long time and some is stored in plants, plankton and seashells. Some C02 also dissolves in seawater. Human activity is adding to the amount of C02 in the air. People burn fossil fuels like coal, oil and gas to power factories and make electricity to heat our homes.

Carbon dioxide is believed to cause global warming. Others feel that global warming is a natural cycle.

Green-e Climate is primarily aimed at emission reductions from the six primary greenhouse gases-carbon dioxide, nitrous oxide, methane, hydrofluorocarbons, perfluorocarbons, and sulfur hexafluoride (CO2, N2O, CH4, HFCs, PFCs and SF6) that are included under the Kyoto Protocol. Green-e Climate only verifies and certifies offsets comprising GHG emission reductions already verified and certified according to an Endorsed Program's protocols.

Presently, according to the IPCC and its range of possible scenarios, atmospheric carbon dioxide could double as soon as 2050. [4] Among other things, this could result in more destructive storms, flooding, ice cap melting, and rising sea levels.

If we start with 1000 cubic feet of natural gas (and assuming it is pure methane or CH4) at STP (standard temperature and pressure, i.e., temperature of 273&#176K = 0&#176C = 32&#176F and pressure of 1 atm = 14.7 psia = 760 torr), and burn it completely, here's what we come up with: Since 1 mole of a gas occupies 22.4 L at STP, 28316.85 L of CH4 contains 28316.85/22.4 = 1264.145 moles of CH4 (each mole of CH4 = approx. 16 g) One mole of CO2 has a mass of approx. 44 g, so 1264.

In reference to the above question, water vapor is not included as an anthropogenic greenhouse gas. Non-carbon dioxide greenhouse gases include methane, nitrous oxide (N2O), Hydrofluorocarbons, Perfluorocarbons, and Sulfur Hexafluoride. In 2001 carbon dioxide accounted for 83.7% of the total U.S. greenhouse gas gas emissions. Methane accounted for 9.3% of total greenhouse gas emissions, N2O 5.2%, and the others combine for 1.7%.

The answer to that question is complicated by the fact that human activity is not the only factor affecting the amount of carbon dioxide in the atmosphere. Plants, both on land and in the oceans, continually absorb and release large amounts of carbon dioxide. Plants absorb carbon dioxide when they grow and release carbon dioxide as they decay. Forest fires, volcanoes, droughts and other natural phenomena can affect the natural rate of carbon dioxide uptake and release.

Yes.Therapeutic laser treatment with carbon dioxide lasers has become more and more popular. This does not require instruments expressly designed for that purpose. Practically any carbon dioxide laser can be used as long as the beam can be spread out over an appropriate area, and as long as the power can be regulated to avoid burning. This can always be achieved with an additional lens of germanium or zinc selenide, if it cannot be done with the standard accessories accompanying the apparatus.

Greenhouse gas emissions are gases that trap heat in the Earth's atmosphere. Without greenhouse gases the average global temperature would go from 59 degrees Fahrenheit to 0 degrees Fahrenheit. The most notable greenhouse gases are carbon dioxide (CO2), methane (CH4), nitrous oxide (N2O), halocarbons that contain fluorine such as hydrofluorocarbons (HFCs) and perfluorocarbons (PFCs), and sulfur hexafluoride (SF6) (EPA 2003c). Each greenhouse gas differs in its ability to hold heat.

Scientists know for certain that human activities are changing the composition of Earth's atmosphere. Increasing levels of greenhouse gases, like carbon dioxide (CO2 ), in the atmosphere since pre-industrial times have been well documented. There is no doubt this atmospheric buildup of carbon dioxide and other greenhouse gases is largely the result of human activities. It's well accepted by scientists that greenhouse gases trap heat in the Earth's atmosphere and tend to warm the planet.

Humans exhale about 1 kg of carbon dioxide per day (http://cdiac.esd.ornl.gov/pns/faq.html). The exact amount depends on age, sex, size, and most importantly activity level. Multiply that by a world population of six billion and you get a very large number. However, human exhalation of carbon dioxide is part of a closed system.

Several experiments have shown that the rate of carbon dioxide uptake in certain species of plants does increase with increased ambient carbon dioxide concentrations. However, many scientists and climatologists believe that increased atmospheric greenhouse gas concentrations will cause increased occurrence of droughts, floods, and other extreme weather events which would disrupt plant growth and counter any positive uptake effects from atmospheric carbon dioxide concentrations.

The gas that humans and animals breathe out and that plants use during photosynthesis to produce oxygen.

Supercritical fluid extraction has emerged as an attractive separation technique for the food and pharmaceutical industries due to a growing demand for "natural" processes that do not introduce any residual organic chemicals. Supercritical carbon dioxide is by far the most commonly used supercritical fluid.

Oil production totaled 42,692 barrels from 18 producing wells in 2007, down from 54,807 barrels from 20 wells in 2006. Gas production totaled 650 million cubic feet from 7 producing gas wells, up from 608 million cubic feet from 7 wells in 2006. No CO2 was produced in 2007. There was one active disposal well and 23 shut-in wells at yearend including 20 oil, 1 gas, 1 CO2, and 2 disposal wells.

Landfill gas recovery projects provide a highly effective means of reducing overall greenhouse gas emissions from landfills, whether the landfill gas is combusted by flare, electricity generation equipment, or another end use system. By using the otherwise wasted methane contained in the collected landfill gas to generate electricity or directly as a fuel, fossil fuels such as oil and coal are displaced.

Natural gas is primarily methane, which is a major greenhouse gas. Methane is emitted directly to the atmosphere from sources such as leaks in natural gas wells and pipelines and is produced in landfills, sewage treatment facilities and livestock operations. Other major greenhouse gases, carbon dioxide and nitrous oxides are produced when natural gas is burned for heating and electric power production.

The greenhouse gas estimates presented here are full fuel-cycle estimates, combining the three major greenhouse gases emitted by motor vehicles: Full fuel-cycle estimates include all steps in the use of a fuel, from production and refining to distribution and final use. This gives a more complete picture of the climate change impacts of using a particular fuel. Some greenhouse gases have greater impacts on climate than others.

Inventory of U.S. Greenhouse Gas Emissions and Sinks: 1990-2004. U.S. EPA, Office of Atmospheric Programs. EPA/430/R-06-002. April 15, 2006. This report presents estimates by the United States government of U.S. human-related greenhouse gas emissions and sinks for the years 1990 through 2004. The information provided in this inventory is presented in accordance with the Revised 1996 Intergovernmental Panel on Climate Change (IPCC) Guidelines for National Greenhouse Gas Inventories.

There are six main greenhouse gases, the most common of which are carbon dioxide (C02), methane (CH4) and nitrous oxide (N20). These are all produced from human activity - C02 from transport and energy; CH4 mainly from animals burping out the gas as they digest their food; N20 mainly from agriculture such as the use of fertiliser and when animals urinate.

Carbon dioxide persists for more than a century in the air. Methane’s average lifetime is about 11 years.

There has been no scientific data to prove that these machines collect enough mosquitoes to make any significant reduction in the mosquito population. Carbon dioxide is only one of the chemicals that attract female mosquitoes. They are also very sensitive to other chemicals, such as hormones and amino acids. Some people claim the carbon dioxide attracts more mosquitoes to a specific area, potentially increasing the population.

The Program Developed for CO2 System Calculations (ORNL/CDIAC-105), recently released by Ernie Lewis, Department of Applied Science, Brookhaven National Laboratory, and Doug Wallace, Abteilung Meereschemie, Institut fuer Meereskunde, was developed to help calculate inorganic carbon speciation in seawater.

The properties which make supercritical carbon dioxide an attractive solvent for extraction also apply to its use as a medium for reaction chemistry. A fluid's most important physical and transport properties that influence the kinetics of a chemical reaction are intermediate between those of a liquid and a gas in the supercritical carbon dioxide. The reactants and the supercritical carbon dioxide frequently form a single supercritical fluid phase.

Various types of pumps can be used for supercritical fluid applications. For medium to large volume processes, a pneumatic booster pump is most often used. A diaphragm pushes against a piston to compress the liquid carbon dioxide to a set pressure point. The air that drives the pump increases the liquid carbon dioxide pressure (boosts) in a ratio of about 100 to 1. So for every 1 psi of air delivered to the pump, the carbon dioxide pressure is boosted by 100 psi. (i.e. Air at 50 psi.

The Program Developed for CO2 System Calculations (ORNL/CDIAC-105), recently released by Ernie Lewis, Department of Applied Science, Brookhaven National Laboratory, and Doug Wallace, Abteilung Meereschemie, Institut fuer Meereskunde, was developed to help calculate inorganic carbon speciation in seawater.