Zobrazeno 1 - 9
of 9
pro vyhledávání: '"Carolina M. L. Camargo"'
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
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
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8ad08e9450b00b19925ef3a20a76f247
https://doi.org/10.1175/jpo-d-20-0103.1
https://doi.org/10.1175/jpo-d-20-0103.1
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::08a221cb8b5747be820e8ae191f179fb
https://doi.org/10.1029/2020jc016551
https://doi.org/10.1029/2020jc016551
The steric component of sea-level change comprises variations in the temperature (thermosteric) and salinity (halosteric) of the oceans, which alter the water’s density, leading to volumetric variations of the water column. Although its importance
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::66454f9c47142a996eaa3f69c638de31
https://doi.org/10.5194/egusphere-egu2020-3009
https://doi.org/10.5194/egusphere-egu2020-3009
Autor:
Dewi Le Bars, Francisco M. Calafat, Caroline A. Katsman, Theo Gerkema, Carolina M. L. Camargo, Jonathan Tinker, Aimée B. A. Slangen, Tim H. J. Hermans
Publikováno v:
Journal of Geophysical Research: Oceans
Journal Of Geophysical Research-Oceans, 125(10)
Journal Of Geophysical Research-Oceans, 125(10)
Sea level on the northwestern European shelf (NWES) varies substantially from year to year. Removing explained parts of interannual sea level variability from observations helps to improve estimates of long-term sea level trends. To this end, the con
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::56d17a26743d27313e4a75441085cbbd
https://www.vliz.be/imisdocs/publications/17/352917.pdf
https://www.vliz.be/imisdocs/publications/17/352917.pdf