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Related Concept Videos

Tidal Forces01:06

Tidal Forces

The origin of Earth's ocean tides has been a subject of continuous investigation for over 2000 years. However, the work of Newton is considered to be the beginning of the proper understanding of the phenomenon. Ocean tides are the result of gravitational tidal forces. These same tidal forces are present in any astronomical body; they are responsible for the internal heat that creates the volcanic activity on Io, one of Jupiter's moons, and the breakup of stars that get too close to black holes.
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.
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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...
What is Climate?01:16

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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.
Conditions on Early Earth02:06

Conditions on Early Earth

Around 4 billion years ago, oceans began to condense on earth while volcanic eruptions released nitrogen, carbon dioxide, methane, ammonia, and hydrogen into the primordial atmosphere. However, organisms with the characteristics of life were not initially present on earth. Scientists have used experimentation to determine how organisms evolved that could grow, reproduce, and maintain an internal environment.

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Hydrogen-Water Vapor Mixtures: Control of Hydrothermal Atmospheres by Hydrogen Osmosis.

Science (New York, N.Y.)·1963
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Using Generative Art to Convey Past and Future Climate Transitions
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Earth tides, global heat flow, and tectonics.

H R Shaw

    Science (New York, N.Y.)
    |May 29, 1970
    PubMed
    Summary

    Tidal energy can power a heat engine, explaining magma production and seafloor spreading. This process influences heat flux similarity across continents and oceans.

    Area of Science:

    • Geophysics
    • Earth Science
    • Tectonics

    Background:

    • Magma production and seafloor spreading are key geological processes.
    • Understanding heat flux variations over continents and oceans is crucial.

    Purpose of the Study:

    • To investigate the role of tidal energy in driving geological processes.
    • To explain the observed similarity in heat flux between continental and oceanic regions.

    Main Methods:

    • Modeling a heat engine powered by tidal energy.
    • Analyzing the relationship between mass transfer depth and radiogenic heat production.

    Main Results:

    • Tidal energy can account for geologically reasonable rates of magma production.
    • Tidal energy explains observed seafloor spreading rates.

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  • An inverse relationship exists between mass transfer depth and radiogenic heat production, influencing heat flux.
  • Conclusions:

    • Tidal energy is a significant factor in magma production and seafloor spreading.
    • The model successfully explains heat flux similarity across different Earth regions.