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    Glacial Isostatic Adjustment: Theory for a Spherically Symmetric Earth and Numerical Results

    Glacial Isostatic Adjustment by Spada, Giorgio; Melini, Daniele;

    Theory for a Spherically Symmetric Earth and Numerical Results

    Series: Springer Geophysics;

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      • Publisher's listprice EUR 171.19
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        72 618 Ft (69 160 Ft + 5% VAT)
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    72 618 Ft

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    Product details:

    • Publisher Springer
    • Date of Publication 29 July 2025
    • Number of Volumes 1 pieces, Book

    • ISBN 9783031905377
    • Binding Hardback
    • No. of pages372 pages
    • Size 235x155 mm
    • Language English
    • Illustrations 74 Illustrations, black & white
    • 700

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    Short description:

    This book aims at presenting a synthetic but self-contained theory of Glacial Isostatic Adjustment (GIA), firmly grounded on physics and mathematics. However, at the same time, it also describes various phenomenological aspects, making it appealing also to a broad audience of Earth scientists not having a technical background. The interest on GIA is motivated by the entangled processes involved, reflecting interactions between the solid Earth, the oceans, and the cryosphere. In the context of climate change, GIA has a special role. For example, ground or space-based geodetic methods aimed at observing the mass balance variations of the contemporary ice sheets require a GIA correction before they can be suitably interpreted. For these reasons, GIA modeling has seen a considerable development recently, with a growing attention by a broad audience of scientists in the fields of geophysics, geology, geodesy, and Earth system science.

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    Long description:

    This book aims at presenting a synthetic but self-contained theory of Glacial Isostatic Adjustment (GIA), firmly grounded on physics and mathematics. However, at the same time, it also describes various phenomenological aspects, making it appealing also to a broad audience of Earth scientists not having a technical background. The interest on GIA is motivated by the entangled processes involved, reflecting interactions between the solid Earth, the oceans, and the cryosphere. In the context of climate change, GIA has a special role. For example, ground or space-based geodetic methods aimed at observing the mass balance variations of the contemporary ice sheets require a GIA correction before they can be suitably interpreted. For these reasons, GIA modeling has seen a considerable development recently, with a growing attention by a broad audience of scientists in the fields of geophysics, geology, geodesy, and Earth system science.

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    Table of Contents:

    1.Gravity, rheology and mass distributions.- 2.Love numbers and Green’s functions.- 3.The Earth’s response to surface loads.- 4.Rotational response of the Earth.- 5.The Sea Level Equation.- 6.Solving the Sea Level Equation.

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    Glacial Isostatic Adjustment: Theory for a Spherically Symmetric Earth and Numerical Results

    Glacial Isostatic Adjustment: Theory for a Spherically Symmetric Earth and Numerical Results

    Spada, Giorgio; Melini, Daniele;

    72 618 HUF

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