國立虎尾科技大學 |

Glacial isostatic adjustment = theory for a spherically symmetric Earth and numerical results /

紀錄類型:	書目-語言資料,印刷品 : Monograph/item
正題名/作者:	Glacial isostatic adjustment/ by Giorgio Spada, Daniele Melini.
其他題名:	theory for a spherically symmetric Earth and numerical results /
作者:	Spada, Giorgio.
其他作者:	Melini, Daniele.
出版者:	Cham :Springer Nature Switzerland : : 2025.,
面頁冊數:	xix, 393 p. :ill. (some col.), digital ; : 24 cm.;
Contained By:	Springer Nature eBook
標題:	Glacial isostasy. -
電子資源:	https://doi.org/10.1007/978-3-031-90538-4
ISBN:	9783031905384

Glacial isostatic adjustment = theory for a spherically symmetric Earth and numerical results /
Spada, Giorgio.

Glacial isostatic adjustmenttheory for a spherically symmetric Earth and numerical results /[electronic resource] :by Giorgio Spada, Daniele Melini. - Cham :Springer Nature Switzerland :2025. - xix, 393 p. :ill. (some col.), digital ;24 cm. - Springer geophysics,2364-9127. - Springer geophysics..

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.

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.

ISBN: 9783031905384

Standard No.: 10.1007/978-3-031-90538-4doiSubjects--Topical Terms:

1495578
Glacial isostasy.

LC Class. No.: QE511

Dewey Class. No.: 551.313

Glacial isostatic adjustment = theory for a spherically symmetric Earth and numerical results /
LDR:02262nam a2200337 a 4500 001 1166776
003 DE-He213
005 20250728130253.0
006 m d
007 cr nn 008maaau
008 251217s2025 sz s 0 eng d
020 $a 9783031905384 $q (electronic bk.)
020 $a 9783031905377 $q (paper)
024 7 $a 10.1007/978-3-031-90538-4 $2 doi
035 $a 978-3-031-90538-4
040 $a GP $c GP
041 0 $a eng
050 4 $a QE511
072 7 $a PHVG $2 bicssc
072 7 $a SCI032000 $2 bisacsh
072 7 $a PHVG $2 thema
082 0 4 $a 551.313 $2 23
090 $a QE511 $b .S732 2025
100 1 $a Spada, Giorgio. $3 1495576
245 1 0 $a Glacial isostatic adjustment $h [electronic resource] : $b theory for a spherically symmetric Earth and numerical results / $c by Giorgio Spada, Daniele Melini.
260 $a Cham : $c 2025. $b Springer Nature Switzerland : $b Imprint: Springer,
300 $a xix, 393 p. : $b ill. (some col.), digital ; $c 24 cm.
490 1 $a Springer geophysics, $x 2364-9127
505 0 $a 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.
520 $a 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.
650 0 $a Glacial isostasy. $3 1495578
650 1 4 $a Geophysics. $3 686174
650 2 4 $a Computational Mathematics and Numerical Analysis. $3 669338
650 2 4 $a Gravitational Physics. $3 1389576
700 1 $a Melini, Daniele. $3 1495577
710 2 $a SpringerLink (Online service) $3 593884
773 0 $t Springer Nature eBook
830 0 $a Springer geophysics. $3 883652
856 4 0 $u https://doi.org/10.1007/978-3-031-90538-4
950 $a Earth and Environmental Science (SpringerNature-11646)