Zobrazeno 1 - 10
of 16
pro vyhledávání: '"M. L. Camargo"'
Publikováno v:
Geophysical Research Letters, Vol 51, Iss 14, Pp n/a-n/a (2024)
Abstract Sea‐level change threatens the U.S. East Coast. Thus, it is important to understand the underlying causes, including ocean dynamics. Most past studies emphasized links between coastal sea level and local atmospheric variability or large‐
Externí odkaz:
https://doaj.org/article/7613974729c242b5871270d8debb0197
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
Publikováno v:
Frontiers in Marine Science, Vol 10 (2023)
Sea-level change is one of the most concerning climate change and global warming consequences, especially impacting coastal societies and environments. The spatial and temporal variability of sea level is neither linear nor globally uniform, especial
Externí odkaz:
https://doaj.org/article/308062f6333f41a5a99a67ee0ccff877
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
Publikováno v:
Journal of Physical Oceanography. 51:1187-1203
The interaction between the incoming winds and high mountainous islands produces a wind-sheltered area on the leeward side, known as the atmospheric wake. In addition to weaker winds, the wake is also characterized by a clearing of clouds, resulting
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
Ocean mass variation is one of the main drivers of present-day sea-level change (SLC). Also known as barystatic SLC, those fluctuations are due to the melting of continental ice from glaciers and ice sheets, and variations in landwater storage. While
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8cc6f839f330c93a10f517ef3372d89c
https://doi.org/10.5194/egusphere-egu21-2574
https://doi.org/10.5194/egusphere-egu21-2574
Publikováno v:
Journal Of Geophysical Research-Oceans, 125(10)
Recent studies disagree about the contribution of variations in temperature and salinity of the oceans—steric change—to the observed sea-level change. This article explores two sources of uncertainty to both global mean and regional steric sea-le