Greenhouse Effect - AP Environmental Science

The greenhouse effect plays a role in all of the options because of the interaction between the layer of gasses surrounding the earth and the solar radiation that approaches the earth. An easy way to remember this is to follow the path of solar radiation traveling from the sun to the earth and think of all the possible ways in which this radiation can travel. The radiation can bounce off and not enter, it can enter and be absorbed in the surface, or it can enter and both bounce off the earth's surface and then be absorbed.

Every scientist listed but Norman Burlaug are responsible for the early studies of the greenhouse effect. Joseph Fourier spoke about the effect in 1824. Claude Pouillet studied its existence further in 1827 and 1838. John Tyndall conducted experimental observations in 1859.

This term was first used by Nils Gustaf Ekholm in 1901. Ekholm was an early adopter of climate control. His early studies included how the burning of coal could add unnecessary levels of carbon dioxide to the atmosphere.

Water vapor is the largest contributor to greenhouse gases at 36-70%. Carbon dioxide is second with 9-26%, then methane with 4-9%, and finally ozone with 3-7%.

The greenhouse effect can also be found on Mars, Venus, and Saturn's largest moon, Titan. The effect on Venus is large because of its dense atmosphere of made of carbon dioxide.

The greenhouse effect plays a role in all of the options because of the interaction between the layer of gasses surrounding the earth and the solar radiation that approaches the earth. An easy way to remember this is to follow the path of solar radiation traveling from the sun to the earth and think of all the possible ways in which this radiation can travel. The radiation can bounce off and not enter, it can enter and be absorbed in the surface, or it can enter and both bounce off the earth's surface and then be absorbed.

Every scientist listed but Norman Burlaug are responsible for the early studies of the greenhouse effect. Joseph Fourier spoke about the effect in 1824. Claude Pouillet studied its existence further in 1827 and 1838. John Tyndall conducted experimental observations in 1859.

This term was first used by Nils Gustaf Ekholm in 1901. Ekholm was an early adopter of climate control. His early studies included how the burning of coal could add unnecessary levels of carbon dioxide to the atmosphere.

Water vapor is the largest contributor to greenhouse gases at 36-70%. Carbon dioxide is second with 9-26%, then methane with 4-9%, and finally ozone with 3-7%.

The greenhouse effect can also be found on Mars, Venus, and Saturn's largest moon, Titan. The effect on Venus is large because of its dense atmosphere of made of carbon dioxide.

The greenhouse effect plays a role in all of the options because of the interaction between the layer of gasses surrounding the earth and the solar radiation that approaches the earth. An easy way to remember this is to follow the path of solar radiation traveling from the sun to the earth and think of all the possible ways in which this radiation can travel. The radiation can bounce off and not enter, it can enter and be absorbed in the surface, or it can enter and both bounce off the earth's surface and then be absorbed.

Every scientist listed but Norman Burlaug are responsible for the early studies of the greenhouse effect. Joseph Fourier spoke about the effect in 1824. Claude Pouillet studied its existence further in 1827 and 1838. John Tyndall conducted experimental observations in 1859.

This term was first used by Nils Gustaf Ekholm in 1901. Ekholm was an early adopter of climate control. His early studies included how the burning of coal could add unnecessary levels of carbon dioxide to the atmosphere.

Water vapor is the largest contributor to greenhouse gases at 36-70%. Carbon dioxide is second with 9-26%, then methane with 4-9%, and finally ozone with 3-7%.

The greenhouse effect can also be found on Mars, Venus, and Saturn's largest moon, Titan. The effect on Venus is large because of its dense atmosphere of made of carbon dioxide.

The greenhouse effect plays a role in all of the options because of the interaction between the layer of gasses surrounding the earth and the solar radiation that approaches the earth. An easy way to remember this is to follow the path of solar radiation traveling from the sun to the earth and think of all the possible ways in which this radiation can travel. The radiation can bounce off and not enter, it can enter and be absorbed in the surface, or it can enter and both bounce off the earth's surface and then be absorbed.

Every scientist listed but Norman Burlaug are responsible for the early studies of the greenhouse effect. Joseph Fourier spoke about the effect in 1824. Claude Pouillet studied its existence further in 1827 and 1838. John Tyndall conducted experimental observations in 1859.

This term was first used by Nils Gustaf Ekholm in 1901. Ekholm was an early adopter of climate control. His early studies included how the burning of coal could add unnecessary levels of carbon dioxide to the atmosphere.

Water vapor is the largest contributor to greenhouse gases at 36-70%. Carbon dioxide is second with 9-26%, then methane with 4-9%, and finally ozone with 3-7%.

The greenhouse effect can also be found on Mars, Venus, and Saturn's largest moon, Titan. The effect on Venus is large because of its dense atmosphere of made of carbon dioxide.