Historic Carbon Dioxide Levels
Scientists in the 19th century have figured out that gases in the atmosphere can cause "greenhouse effect".
These scientists became interested mainly interested in the possibility that a lower level of carbon dioxide gas may explain the ice ages of the distant past as at the twist of the century, Svante Arrhenius has calculated that emissions from human industry can bring a global warming in the future.
Nonetheless, other scientists dismissed his idea as faulty and in 1938, G.
S.
Calendar argued that the historic carbon dioxide levels were climbing and raising global temperature, but then most scientists found his arguments unbelievable then it was almost by chance that a few researchers in the 1950s discovered that global warming was really possible.
In the early 1960s, C.
D.
Keeling determined that the level of carbon dioxide in the atmosphere was rising fast.
From then, researchers began to take an interest about the changes on carbon dioxide levels, and how these were influenced by chemical and biological forces.
Gas plays a crucial role in climate change, so that the rising level could gravely affect our future; hence, it is just important to take into account the historic carbon dioxide levels in different locations.
Like many Victorian natural philosophers, John Tyndall was fascinated by many questions as while he was preparing an important treatise on "Heat as a Mode of Motion", he took time to consider geology.
Familiar with glaciers, Tyndall had been convinced by the evidence, which became hotly debated among scientists of his day - that for thousands of years ago, colossal layers of ice had covered the northern Europe.
These have proven that climate change has been affected by the alteration of the composition of the Earth's atmosphere.
From the work of Joseph Fourier in the 1820s, scientists understood that gases in the atmosphere might trap the heat received from the Sun.
This phenomenon is better known as "greenhouse effect", which is more defined by the historic carbon dioxide levels.
The equations and data available to 19th-century scientists used to be far too poor to allow an accurate calculation.
Nonetheless, the physics was straightforward enough to show that a bare rock at the Earth's distance from the Sun needs to be far colder than the Earth.
Historic carbon dioxide levels can effectively determine any gas that could trap heat rays.
In 1859, Tyndall's laboratory work identified the different gases that did such.
In some disputes, the increase in carbon dioxide has minimal effects on global warming but to think about it, when there is excessive supply of carbon dioxide, and there are just few plants that will use such for photosynthesis, greenhouse effect has been evidently brought by high levels of CO2 in the atmosphere.
These scientists became interested mainly interested in the possibility that a lower level of carbon dioxide gas may explain the ice ages of the distant past as at the twist of the century, Svante Arrhenius has calculated that emissions from human industry can bring a global warming in the future.
Nonetheless, other scientists dismissed his idea as faulty and in 1938, G.
S.
Calendar argued that the historic carbon dioxide levels were climbing and raising global temperature, but then most scientists found his arguments unbelievable then it was almost by chance that a few researchers in the 1950s discovered that global warming was really possible.
In the early 1960s, C.
D.
Keeling determined that the level of carbon dioxide in the atmosphere was rising fast.
From then, researchers began to take an interest about the changes on carbon dioxide levels, and how these were influenced by chemical and biological forces.
Gas plays a crucial role in climate change, so that the rising level could gravely affect our future; hence, it is just important to take into account the historic carbon dioxide levels in different locations.
Like many Victorian natural philosophers, John Tyndall was fascinated by many questions as while he was preparing an important treatise on "Heat as a Mode of Motion", he took time to consider geology.
Familiar with glaciers, Tyndall had been convinced by the evidence, which became hotly debated among scientists of his day - that for thousands of years ago, colossal layers of ice had covered the northern Europe.
These have proven that climate change has been affected by the alteration of the composition of the Earth's atmosphere.
From the work of Joseph Fourier in the 1820s, scientists understood that gases in the atmosphere might trap the heat received from the Sun.
This phenomenon is better known as "greenhouse effect", which is more defined by the historic carbon dioxide levels.
The equations and data available to 19th-century scientists used to be far too poor to allow an accurate calculation.
Nonetheless, the physics was straightforward enough to show that a bare rock at the Earth's distance from the Sun needs to be far colder than the Earth.
Historic carbon dioxide levels can effectively determine any gas that could trap heat rays.
In 1859, Tyndall's laboratory work identified the different gases that did such.
In some disputes, the increase in carbon dioxide has minimal effects on global warming but to think about it, when there is excessive supply of carbon dioxide, and there are just few plants that will use such for photosynthesis, greenhouse effect has been evidently brought by high levels of CO2 in the atmosphere.
