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Constraining the Parameters of the Andrade Rheological Model in the Earth’s Mantle Based on the Love Numbers of the M2 Lunar Semidiurnal Tide
Constraining the Parameters of the Andrade Rheological Model in the Earth’s Mantle Based on the Love Numbers of the M2 Lunar Semidiurnal Tide
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Constraining the Parameters of the Andrade Rheological Model in the Earth’s Mantle Based on the Love Numbers of the M2 Lunar Semidiurnal Tide
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Constraining the Parameters of the Andrade Rheological Model in the Earth’s Mantle Based on the Love Numbers of the M2 Lunar Semidiurnal Tide
Constraining the Parameters of the Andrade Rheological Model in the Earth’s Mantle Based on the Love Numbers of the M2 Lunar Semidiurnal Tide

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Constraining the Parameters of the Andrade Rheological Model in the Earth’s Mantle Based on the Love Numbers of the M2 Lunar Semidiurnal Tide
Constraining the Parameters of the Andrade Rheological Model in the Earth’s Mantle Based on the Love Numbers of the M2 Lunar Semidiurnal Tide
Journal Article

Constraining the Parameters of the Andrade Rheological Model in the Earth’s Mantle Based on the Love Numbers of the M2 Lunar Semidiurnal Tide

2024
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Overview
It has been demonstrated for the first time in this paper that the frequently used approximation of the Andrade rheology with only one parameter is oversimplified and might lead to incorrect conclusions when studying the internal structure of the planets of the Solar System. Instead, we have used the Andrade rheology with two empirical parameters: α and ζ. The Earth’s viscoelastic Love numbers for the principal lunar semidiurnal tide M 2 were computed for two viscosity profiles and for 16 100 different combinations of α and ζ. The comparison of the computed Love numbers with the measured values makes it possible to constrain the range of values of both parameters that successfully describes the rheological properties of the Earth’s mantle.