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Related Concept Videos

Global Climate Change01:50

Global Climate Change

Throughout its ~4.5 billion year history, the Earth has experienced periods of warming and cooling. However, the current drastic increase in global temperatures is well outside of the Earth’s cyclic norms, and evidence for human-caused global climate change is compelling. Paleoclimatology, the study of ancient climate conditions, provides ample evidence for human-caused global climate change by comparing recent conditions with those in the past.
Microbes and Climate Change01:27

Microbes and Climate Change

Microorganisms are pivotal agents in Earth's biogeochemical cycles, significantly influencing climate dynamics through their metabolic activities. These microbes modulate the levels of key greenhouse gases by both contributing to and helping mitigate climate change.Microbial Contributions to Greenhouse Gas EmissionsRising global temperatures accelerate microbial metabolism, which, in turn, speeds up the decomposition of organic matter. This process releases carbon dioxide (CO₂) through...
What is Climate?01:16

What is Climate?

Climate refers to the prevailing weather conditions in a specific area over an extended period. As the saying goes, “Climate is what you expect. Weather is what you get.” Climate is influenced by geographic factors, such as latitude, terrain, and proximity to bodies of water.
Radiation: Applications01:17

Radiation: Applications

The average temperature of Earth is the subject of much current discussion. Earth is in radiative contact with both the Sun and dark space; it receives almost all its energy from the radiation of the Sun and reflects some of it into outer space. Dark space is very cold, about 3 K, so Earth radiates energy into it. For instance, heat transfer occurs from soil and grasses, the rate of which can be so rapid that frost can occur on clear summer evenings, even in warm latitudes.
The average...
The Carbon Cycle01:14

The Carbon Cycle

Carbon is the basis of all organic matter on Earth, and is recycled through the ecosystem in two primary processes: one in which carbon is exchanged among living organisms, and one in which carbon is cycled over long periods of time through fossilized organic remains, weathering of rocks, and volcanic activity. Human activities, including increased agricultural practices and the burning of fossil fuels, has greatly affected the balance of the natural carbon cycle.
The Calvin Benson Cycle01:46

The Calvin Benson Cycle

Ribulose 1,5- bisphosphate carboxylase/oxygenase (RuBisCo) is a critical enzyme that catalyzes carbon dioxide assimilation during photosynthesis. However, it is an inefficient enzyme, having an extremely slow catalytic rate. A typical enzyme can process about a thousand molecules per second; however, RuBisCo fixes only around three-carbon dioxides per second. Photosynthetic cells compensate for this slow rate by synthesizing very high amounts of RuBisCo, making it the most abundant single...

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Related Experiment Video

Updated: Jul 11, 2026

A CO2 Concentration Gradient Facility for Testing CO2 Enrichment and Soil Effects on Grassland Ecosystem Function
10:19

A CO2 Concentration Gradient Facility for Testing CO2 Enrichment and Soil Effects on Grassland Ecosystem Function

Published on: November 21, 2015

The greenhouse effect: science and policy.

S H Schneider

    Science (New York, N.Y.)
    |February 10, 1989
    PubMed
    Summary
    This summary is machine-generated.

    Global warming, driven by increased greenhouse gases like carbon dioxide (CO2), is a significant issue. While the science of warming is clear, precise future impacts and detection of a definitive signal remain subjects of scientific uncertainty and policy debate.

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    Design and Use of a Full Flow Sampling System (FFS) for the Quantification of Methane Emissions
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    Area of Science:

    • Climate Science
    • Environmental Science
    • Atmospheric Chemistry

    Background:

    • The increase in atmospheric greenhouse gases, including carbon dioxide (CO2), methane, and chlorofluorocarbons, is well-established.
    • Fossil fuel combustion and land-use changes are primary drivers of rising CO2 levels since 1850.

    Purpose of the Study:

    • To review the scientific consensus and uncertainties surrounding global warming.
    • To discuss the implications of climate models and potential policy responses.

    Main Methods:

    • Analysis of existing scientific literature and climate models.
    • Evaluation of data on greenhouse gas concentrations and their historical trends.

    Main Results:

    • Climate models project a 2-6°C rise in global average surface temperatures over the next century.
    • Sea level rise is projected to be 0.5-1.5 meters, with considerable uncertainty.
    • Significant uncertainties exist in predicting future greenhouse gas concentrations and feedback processes, impacting temperature and precipitation forecasts.

    Conclusions:

    • While the fundamental science of greenhouse gas-induced warming is not controversial, precise future impacts involve significant uncertainties.
    • Policy decisions regarding greenhouse gas emissions involve value judgments beyond purely scientific data.
    • Implementing policies that reduce emissions and offer societal benefits is a proposed approach.