Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Riccardo E M Riva"'
Publikováno v:
Environmental Research Letters, Vol 17, Iss 7, p 074002 (2022)
Global mean sea-level rise (SLR) has accelerated since 1900 from less than 2 mm yr ^−1 during most of the century to more than 3 mm yr ^−1 since 1993. Decision-makers in coastal countries, however, require information on SLR at the regional scale
Externí odkaz:
https://doaj.org/article/21602c0cbf5946d2ab83cfd57637e623
Autor:
Carolina M. L. Camargo, Riccardo E. M. Riva, Tim H. J. Hermans, Eike M. Schütt, Marta Marcos, Ismael Hernandez-Carrasco, Aimée B. A. Slangen
Publikováno v:
eISSN
Ocean Science, 19(1)
Ocean Science, 19(1)
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://explore.openaire.eu/search/publication?articleId=doi_dedup___::837b8457662a33abac4a0080b4db489c
https://doi.org/10.5194/os-19-17-2023
https://doi.org/10.5194/os-19-17-2023
In this study, we examine the effect of transient mantle creep on the prediction of glacial isostatic adjustment (GIA) signals. Specifically, we compare predictions of relative sea level change from GIA from a set of Earth models in which transient c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15f7ef81a35a357f628671fdff6e0f76
https://doi.org/10.5194/egusphere-egu22-6236
https://doi.org/10.5194/egusphere-egu22-6236
Publikováno v:
Earth System Dynamics, 13
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://explore.openaire.eu/search/publication?articleId=doi_dedup___::5767039193694ead574400650aa4fc47
https://doi.org/10.5194/esd-13-1351-2022
https://doi.org/10.5194/esd-13-1351-2022
Autor:
Thomas, Ian D., King, Matt A., Bentley, Michael J., Whitehouse, Pippa L., Penna, Nigel T., Williams, Simon D. P., Riccardo, E. M. Riva, Lavallee, David A., Clarke, Peter J., King, Edward C., Hindmarsh, Richard C.A., Koivula, Hannu
Publikováno v:
Geophysical Research Letters, 38, 2011
Geophysical Research Letters
Geophysical Research Letters
Bedrock uplift in Antarctica is dominated by a combination of glacial isostatic adjustment (GIA) and elastic response to contemporary mass change. Here, we present spatially extensive GPS observations of Antarctic bedrock uplift, using 52% more stati
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::894aded2f5bbac1ffda8bb3e216fc03f
http://resolver.tudelft.nl/uuid:849c1136-dc1b-4dbb-b92d-b4090dfccc3c
http://resolver.tudelft.nl/uuid:849c1136-dc1b-4dbb-b92d-b4090dfccc3c