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Climatic fluctuations due to deep ocean circulation.

R G Watts, M E Hayder

    Science (New York, N.Y.)
    |January 28, 1983
    PubMed
    Summary
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    A basic climate model shows oscillating behavior when deep ocean turnover is a time delay. This deep ocean signal reveals frequencies from both the climate forcing and the ocean

    Area of Science:

    • Climate science
    • Oceanography
    • Dynamical systems

    Background:

    • Deep ocean turnover plays a crucial role in regulating Earth's climate system.
    • Understanding the temporal dynamics of ocean processes is essential for accurate climate modeling.

    Purpose of the Study:

    • To investigate the impact of deep ocean turnover time delay on climate model behavior.
    • To analyze the frequency characteristics of the deep ocean signal in a simplified climate model.

    Main Methods:

    • Development of a simple climate model incorporating deep ocean turnover as a pure time delay.
    • Analysis of the model's output to identify oscillatory behavior and frequency components.

    Main Results:

    • The climate model exhibits oscillatory behavior due to the inclusion of deep ocean turnover time delay.

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  • The deep ocean signal contains frequencies influenced by both the external forcing function and the internal ocean delay.

    • Conclusions:

    • Deep ocean turnover time delays can introduce significant oscillatory dynamics into climate models.
    • The frequency analysis of the deep ocean signal provides insights into the interplay between external climate forcings and internal ocean processes.