Next Article in Journal
Wetland Roofs as an Attractive Option for Decentralized Water Management and Air Conditioning Enhancement in Growing Cities—A Review
Next Article in Special Issue
Steric Sea Level Changes from Ocean Reanalyses at Global and Regional Scales
Previous Article in Journal
Modeling Spatiotemporal Rainfall Variability in Paraíba, Brazil
Previous Article in Special Issue
Low-End Probabilistic Sea-Level Projections
Open AccessFeature PaperReview

On Some Properties of the Glacial Isostatic Adjustment Fingerprints

by 1,*,† and 2,†
1
Dipartimento di Scienze Pure e Applicate (DiSPeA), Sezione di Fisica, Università degli Studi di Urbino “Carlo Bo”, I-61029 Urbino, Italy
2
Istituto Nazionale di Geofisica e Vulcanologia (INGV), Via di Vigna Murata 605, I-00143 Rome, Italy
*
Author to whom correspondence should be addressed.
These authors contributed equally to this work.
Water 2019, 11(9), 1844; https://doi.org/10.3390/w11091844
Received: 31 July 2019 / Revised: 28 August 2019 / Accepted: 2 September 2019 / Published: 5 September 2019
(This article belongs to the Special Issue Past, Present and Future Trends in Sea Level Change)
Along with density and mass variations of the oceans driven by global warming, Glacial Isostatic Adjustment (GIA) in response to the last deglaciation still contributes significantly to present-day sea-level change. Indeed, in order to reveal the impacts of climate change, long term observations at tide gauges and recent absolute altimetry data need to be decontaminated from the effects of GIA. This is now accomplished by means of global models constrained by the observed evolution of the paleo-shorelines since the Last Glacial Maximum, which account for the complex interactions between the solid Earth, the cryosphere and the oceans. In the recent literature, past and present-day effects of GIA have been often expressed in terms of fingerprints describing the spatial variations of several geodetic quantities like crustal deformation, the harmonic components of the Earth’s gravity field, relative and absolute sea level. However, since it is driven by the delayed readjustment occurring within the viscous mantle, GIA shall taint the pattern of sea-level variability also during the forthcoming centuries. The shapes of the GIA fingerprints reflect inextricable deformational, gravitational, and rotational interactions occurring within the Earth system. Using up-to-date numerical modeling tools, our purpose is to revisit and to explore some of the physical and geometrical features of the fingerprints, their symmetries and intercorrelations, also illustrating how they stem from the fundamental equation that governs GIA, i.e., the Sea Level Equation. View Full-Text
Keywords: Glacial Isostatic Adjustment; sea level change; fingerprints of past ice melting Glacial Isostatic Adjustment; sea level change; fingerprints of past ice melting
Show Figures

Figure 1

MDPI and ACS Style

Spada, G.; Melini, D. On Some Properties of the Glacial Isostatic Adjustment Fingerprints. Water 2019, 11, 1844. https://doi.org/10.3390/w11091844

AMA Style

Spada G, Melini D. On Some Properties of the Glacial Isostatic Adjustment Fingerprints. Water. 2019; 11(9):1844. https://doi.org/10.3390/w11091844

Chicago/Turabian Style

Spada, Giorgio; Melini, Daniele. 2019. "On Some Properties of the Glacial Isostatic Adjustment Fingerprints" Water 11, no. 9: 1844. https://doi.org/10.3390/w11091844

Find Other Styles
Note that from the first issue of 2016, MDPI journals use article numbers instead of page numbers. See further details here.

Article Access Map by Country/Region

1
Search more from Scilit
 
Search
Back to TopTop