• A personal note on IGBP and the social sciences

    Humans are an integral component of the Earth system as conceptualised by IGBP. João Morais recalls key milestones in IGBP’s engagement with the social sciences and offers some words of advice for Future Earth.
  • IGBP and Earth observation:
    a co-evolution

    The iconic images of Earth beamed back by the earliest spacecraft helped to galvanise interest in our planet’s environment. The subsequent evolution and development of satellites for Earth observation has been intricately linked with that of IGBP and other global-change research programmes, write Jack Kaye and Cat Downy .

Ecosystems and biodiversity

Biological processes interact strongly with physical and chemical processes to create the environment that keeps Earth habitable for life.
Life on Earth has fundamentally altered the chemical composition of Earth’s atmosphere. The evolution of the Earth’s atmosphere is closely linked to the evolution of life.

Biological processes interact strongly with physical and chemical processes to create the environment that keeps Earth habitable for life. The more we examine how the Earth system functions, the greater we realise the role played by life in helping control the system. For example, biological processes contribute significantly to atmospheric carbon dioxide absorption by the oceans, which in turn controls atmospheric carbon dioxide concentration on long time scales.

RUNNING Net Primary Productivity DIAGRAM

Photosynthesis by phytoplankton (small marine plants) reduces the amount of carbon dioxide in the surface layer of the ocean, allowing more carbon dioxide to dissolve from the atmosphere.

About 25% of the carbon fixed by phytoplankton in the upper layers sinks and remains stored away from contact with the atmosphere for hundreds or thousands of years.

Biological pump

This biological pump is a major control on how carbon dioxide moves between the oceans and the atmosphere.

Intriguingly, the nature of the phytoplankton species involved in the biological pump may hold a key to the rate of and potential for carbon storage.

Death and decay

The terrestrial biosphere helps control the atmospheric concentration of carbon dioxide. Plants remove carbon dioxide from the atmosphere and convert it to carbohydrates through photosynthesis. However, plant parts eventually die and decay, are eaten, or burn, all of which lead to the decomposition of the carbohydrates and the return of carbon dioxide to the atmosphere.

Terrestrial cycling of carbon is generally much faster than that of the ocean, and much of the short-term variability in the contemporary carbon dioxide growth rate in the atmosphere is due to variability in terrestrial uptake or loss.

Terrestrial life is an important component in Earth system functioning in other ways. For example, the type of vegetation on land influences the amount of water transpired back to the atmosphere. In addition, plants affect how much radiation from the sun is absorbed or reflected.

Plant root patterns and activity are also important controllers of both carbon and water storage.

Biological diversity

The biological diversity of terrestrial ecosystems affects the magnitude of key ecosystem processes such as productivity, and plays a role in the long-term stability of ecosystem functioning in the face of a changing environment.

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IGBP closed at the end of 2015. This website is no longer updated.

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