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  2. Eunice Newton Foote - Wikipedia

    en.wikipedia.org/wiki/Eunice_Newton_Foote

    Eunice Newton Foote (July 17, 1819 – September 30, 1888) was an American scientist, inventor, and women's rights campaigner.She was the first scientist to confirm that certain gases warm when exposed to sunlight, and that therefore rising carbon dioxide (CO 2) levels could increase atmospheric temperature and affect climate, a phenomenon now referred to as the greenhouse effect.

  3. Charles David Keeling - Wikipedia

    en.wikipedia.org/wiki/Charles_David_Keeling

    Charles David Keeling (April 20, 1928 – June 20, 2005) [1] [2] was an American scientist whose recording of carbon dioxide at the Mauna Loa Observatory [3] confirmed Svante Arrhenius's proposition (1896) of the possibility of anthropogenic contribution to the greenhouse effect and global warming, by documenting the steadily rising carbon dioxide levels.

  4. Keeling Curve - Wikipedia

    en.wikipedia.org/wiki/Keeling_Curve

    Atmospheric carbon dioxide (CO 2) concentrations from 1958 to 2023. The Keeling Curve is a graph of the annual variation and overall accumulation of carbon dioxide in the Earth's atmosphere based on continuous measurements taken at the Mauna Loa Observatory on the island of Hawaii from 1958 to the present day.

  5. Guy Stewart Callendar - Wikipedia

    en.wikipedia.org/wiki/Guy_Stewart_Callendar

    Although Callendar was an amateur climatologist, [2] he expanded on the work of several 19th century scientists, including Arrhenius and Nils Gustaf Ekholm as a hobby. Callendar published 10 major scientific articles, and 25 shorter ones, between 1938 and 1964 on global warming , infra-red radiation and anthropogenic carbon dioxide.

  6. Gas exchange - Wikipedia

    en.wikipedia.org/wiki/Gas_exchange

    The spongy mesophyll cells are loosely packed, allowing for an increased surface area, and consequently an increased rate of gas-exchange. Uptake of carbon dioxide necessarily results in some loss of water vapor, [38] because both molecules enter and leave by the same stomata, so plants experience a gas exchange dilemma: gaining enough CO

  7. Carbon dioxide in Earth's atmosphere - Wikipedia

    en.wikipedia.org/wiki/Carbon_dioxide_in_Earth's...

    Carbon dioxide has unique long-term effects on climate change that are nearly "irreversible" for a thousand years after emissions stop (zero further emissions). The greenhouse gases methane and nitrous oxide do not persist over time in the same way as carbon dioxide. Even if human carbon dioxide emissions were to completely cease, atmospheric ...

  8. Carbon dioxide - Wikipedia

    en.wikipedia.org/wiki/Carbon_dioxide

    Carbon dioxide is a chemical compound with the chemical formula CO 2.It is made up of molecules that each have one carbon atom covalently double bonded to two oxygen atoms. It is found in the gas state at room temperature and at normally-encountered concentrations it is odorless.

  9. Atmospheric carbon cycle - Wikipedia

    en.wikipedia.org/wiki/Atmospheric_carbon_cycle

    Ocean circulation events cause this process to be variable. For example, during El Nino events there is less deep ocean upwelling, leading to lower outgassing of carbon dioxide into the atmosphere. [18] Biological processes also lead to ocean-atmosphere carbon exchange. Carbon dioxide equilibrates between the atmosphere and the ocean's surface ...

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