Zobrazeno 1 - 10
of 16
pro vyhledávání: '"R. E. M. Riva"'
Autor:
C. M. L. Camargo, R. E. M. Riva, T. H. J. Hermans, E. M. Schütt, M. Marcos, I. Hernandez-Carrasco, A. B. A. Slangen
Publikováno v:
Ocean Science, Vol 19, Pp 17-41 (2023)
Attribution of sea-level change to its different drivers is typically done using a sea-level budget approach. While the global mean sea-level budget is considered closed, closing the budget on a finer spatial scale is more complicated due to, for ins
Externí odkaz:
https://doaj.org/article/a0fdaa3468e249d28ee8cdf4f3f2937f
Publikováno v:
Earth System Dynamics, Vol 13, Pp 1351-1375 (2022)
Ocean mass change is one of the main drivers of present-day sea-level change (SLC). Also known as barystatic SLC, ocean mass change is caused by the exchange of freshwater between the land and the ocean, such as melting of continental ice from glacie
Externí odkaz:
https://doaj.org/article/9133642a993943e1a7bb729ecf9169fc
Autor:
Y. Sun, R. E. M. Riva
Publikováno v:
Earth System Dynamics, Vol 11, Pp 129-137 (2020)
The effect of glacial isostatic adjustment (GIA) on the shape and gravity of the Earth is usually described by numerical models that solve for both glacial evolution and Earth's rheology, being mainly constrained by the geological evidence of local i
Externí odkaz:
https://doaj.org/article/4923d4c994024538b1dcc416d20ff205
Autor:
C. G. van der Boog, J. D. Pietrzak, H. A. Dijkstra, N. Brüggemann, R. M. van Westen, R. K. James, T. J. Bouma, R. E. M. Riva, D. C. Slobbe, R. Klees, M. Zijlema, C. A. Katsman
Publikováno v:
Ocean Science, Vol 15, Pp 1419-1437 (2019)
The mesoscale variability in the Caribbean Sea is dominated by anticyclonic eddies that are formed in the eastern part of the basin. These anticyclones intensify on their path westward while they pass the coastal upwelling region along the Venezuelan
Externí odkaz:
https://doaj.org/article/b176c763d1034a4fbeb341db5753ff50
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 4, Pp n/a-n/a (2021)
Abstract The 2018 Mw7.5 Palu earthquake is a remarkable strike‐slip event due to its nature as a shallow supershear fault rupture across several segments and a destructive tsunami that followed coseismic deformation. GPS offsets in the wake of the
Externí odkaz:
https://doaj.org/article/4acf30b6a3204ecf8c881ea78a517c89
Publikováno v:
Solid Earth, Vol 9, Pp 777-795 (2018)
The glacial isostatic adjustment (GIA) signal at present day is constrained via the joint inversion of geodetic observations and GIA models for a region encompassing northern Europe, the British Isles, and the Barents Sea. The constraining data ar
Externí odkaz:
https://doaj.org/article/e0b835ea9d7343d9af6d4c60353e4f2d
Publikováno v:
The Cryosphere, Vol 11, Pp 1327-1332 (2017)
Melting glaciers, ice caps and ice sheets have made an important contribution to sea-level rise through the last century. Self-attraction and loading effects driven by shrinking ice masses cause a spatially varying redistribution of ocean waters t
Externí odkaz:
https://doaj.org/article/bceb33c11cce4f5fbc753f71114e3f2d
Autor:
B. C. Gunter, O. Didova, R. E. M. Riva, S. R. M. Ligtenberg, J. T. M. Lenaerts, M. A. King, M. R. van den Broeke, T. Urban
Publikováno v:
The Cryosphere, Vol 8, Iss 2, Pp 743-760 (2014)
This study explores an approach that simultaneously estimates Antarctic mass balance and glacial isostatic adjustment (GIA) through the combination of satellite gravity and altimetry data sets. The results improve upon previous efforts by incorporati
Externí odkaz:
https://doaj.org/article/f4647e83c69646deaf11014e7cc16de0
Autor:
A. Aoudia, R. E. M. Riva
Publikováno v:
Annals of Geophysics, Vol 51, Iss 2-3 (2008)
The geodynamic complexity of the Apennines and adjacent sedimentary basins in Umbria-Marche (North-Central Italy) makes the dynamics of the present day deformation and its relationships with the seismicity less well understood. In this paper, we ar
Externí odkaz:
https://doaj.org/article/f8e0ef0da66741de90f4db111b56cd2a
Publikováno v:
Journal of Geophysical Research: Solid Earth
JGR Solid Earth, 128(3)
JGR Solid Earth, 128(3)
Greater landward velocities were recorded after six megathrust earthquakes in subduction zone regions adjacent to the ruptured portion. Previous explanations invoked either increased slip deficit accumulation or plate bending during postseismic relax
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::48d526431113d4bce00fcc04501bc40b
https://doi.org/10.1029/2022jb025431
https://doi.org/10.1029/2022jb025431