Zobrazeno 1 - 10
of 20
pro vyhledávání: '"Tim H. J. Hermans"'
Autor:
Tim H. J. Hermans, Julius J. M. Busecke, Thomas Wahl, Víctor Malagón‐Santos, Michael G. Tadesse, Robert A. Jane, Roderik S. W. van deWal
Publikováno v:
Earth's Future, Vol 12, Iss 5, Pp n/a-n/a (2024)
Abstract When different flooding drivers co‐occur, they can cause compound floods. Despite the potential impact of compound flooding, few studies have projected how the joint probability of flooding drivers may change. Furthermore, existing project
Externí odkaz:
https://doaj.org/article/e792cf0d5fba408cb121255073aafd51
Autor:
Víctor Malagón-Santos, Aimée B. A. Slangen, Tim H. J. Hermans, Sönke Dangendorf, Marta Marcos, Nicola Maher
Publikováno v:
eISSN
Ocean Science
Ocean Science
Regional emulation tools based on statistical relationships, such as pattern scaling, provide a computationally inexpensive way of projecting ocean dynamic sea-level change for a broad range of climate change scenarios. Such approaches usually requir
Autor:
Robert E. Kopp, Gregory G. Garner, Tim H. J. Hermans, Shantenu Jha, Praveen Kumar, Aimée B. A. Slangen, Matteo Turilli, Tamsin L. Edwards, Jonathan M. Gregory, George Koubbe, Anders Levermann, Andre Merzky, Sophie Nowicki, Matthew D. Palmer, Chris Smith
Publikováno v:
eISSN
Future sea-level rise projections are characterized by both quantifiable uncertainty and unquantifiable, structural uncertainty. Thorough scientific assessment of sea-level rise projections requires analysis of both dimensions of uncertainty. Probabi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::40ffb883c30d1aaac44dde1ecdbd654c
https://doi.org/10.5194/egusphere-2023-14
https://doi.org/10.5194/egusphere-2023-14
Autor:
Tim H. J. Hermans, Víctor Malagón-Santos, Caroline A. Katsman, Robert A. Jane, D. J. Rasmussen, Marjolijn Haasnoot, Gregory G. Garner, Robert E. Kopp, Michael Oppenheimer, Aimée B. A. Slangen
Publikováno v:
XXVIII General Assembly of the International Union of Geodesy and Geophysics (IUGG)
Sea-level rise (SLR) causes the frequency of extreme sea levels to amplify. Projections of the frequency amplification of extremes are often computed for arbitrary future years and for the historical centennial event. Such projections may therefore n
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::edb308e8b81ca45530d196db79611738
http://imis.nioz.nl/imis.php?module=ref&refid=363583
http://imis.nioz.nl/imis.php?module=ref&refid=363583
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
Autor:
Robert Kopp, Michael Oppenheimer, Jessica L O'Reilly, Sybren S Drijfhout, Tamsin L Edwards, Baylor Fox-Kemper, Gregory G Garner, Nicholas R Golledge, Tim H J Hermans, Helene T Hewitt, Benjamin P Horton, Gerhard Krinner, Dirk Notz, Sophie Nowicki, Matthew D Palmer, Aimée B A Slangen, Cunde Xiao
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fafe042679225acb96a802f39effff76
https://doi.org/10.1002/essoar.10511663.1
https://doi.org/10.1002/essoar.10511663.1
Autor:
Gonéri Le Cozannet, Rémi Thiéblemont, Jeremy Rohmer, Guy Wöppelman, Aimée B A Slangen, Tim H J Hermans
While the understanding and modelling of RSLC due to ocean density and mass changes have greatly improved over the past few decades, RSLC contributions due to vertical ground motions (VGMs) remain a major source of uncertainty, in particular for loca
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e007ce3610b6eebd2e60cfab0bc39820
https://doi.org/10.5194/egusphere-egu22-5217
https://doi.org/10.5194/egusphere-egu22-5217
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
Ocean mass change is one of the main drivers of present-day sea-level change (SLC). Also known as barystatic SLC, it is driven by the exchange of freshwater between the land and the ocean, such as melting of continental ice from glaciers and ice shee
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5a744fe43b69c53bdb2873e5551b9a5a
https://doi.org/10.5194/esd-2021-80
https://doi.org/10.5194/esd-2021-80