Zobrazeno 1 - 10
of 13
pro vyhledávání: '"D. Gwyn Evans"'
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-13 (2022)
Abstract The fate of mesoscale eddy kinetic energy represents a large source of uncertainty in the global ocean energy budget. Satellite altimetry suggests that mesoscale eddies vanish at ocean western boundaries. However, the fate of the eddies’ k
Externí odkaz:
https://doaj.org/article/fd248843b42c4ab7b042e9186c9b282a
The surface forced water mass transformation (SFWMT) is known to be the main contributor of the Atlantic Meridional Overturning Circulation (AMOC) over the subpolar gyre. Over the eastern part of the subpolar gyre, a recent study revealed the dominan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::685d0acd1b1157b9b9e4750c21d113c6
https://doi.org/10.5194/egusphere-egu23-7844
https://doi.org/10.5194/egusphere-egu23-7844
Autor:
Marilena Oltmanns, N. Penny Holliday, James Screen, Ben I. Moat, Simon A. Josey, D. Gwyn Evans, Sheldon Bacon
Amplified Arctic ice loss in recent decades has been linked to increased occurrence of extreme mid-latitude weather. The underlying mechanisms remain elusive, however. One potential link occurs through the ocean as the loss of sea ice and glacial ice
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c992170bd56438b9f5a41e79b44a5220
https://doi.org/10.5194/wcd-2023-1
https://doi.org/10.5194/wcd-2023-1
Publikováno v:
eISSN
The overturning streamfunction as measured at the OSNAP (Overturning in the Subpolar North Atlantic Program) mooring array represents the transformation of warm, salty Atlantic Water into cold, fresh North Atlantic Deep Water (NADW). The magnitude of
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::39f5badbd2c4564b418b038930aed666
https://doi.org/10.5194/egusphere-2022-1059
https://doi.org/10.5194/egusphere-2022-1059
The overturning streamfunction as measured at the OSNAP (Overturning in the Subpolar North Atlantic Program) mooring array represents the transformation of warm/salty Atlantic Water into cold/fresh North Atlantic Deep Water (NADW). The magnitude and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28f871be7f47c86c45c66ea9dc783e74
https://doi.org/10.5194/egusphere-egu22-8447
https://doi.org/10.5194/egusphere-egu22-8447
Autor:
Marilena Oltmanns, N. Penny Holliday, James Screen, D. Gwyn Evans, Simon A. Josey, Sheldon Bacon, Ben I. Moat
Amplified Arctic ice loss in recent decades has been linked to increased occurrence of extreme mid-latitude weather. The underlying dynamical mechanisms remain elusive, however. Here, we demonstrate a novel mechanism linking freshwater releases into
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::16f5ca20eae0b415928f690f3e9c90d4
https://doi.org/10.5194/wcd-2021-79
https://doi.org/10.5194/wcd-2021-79
The OSNAP (Overturning in the Subpolar North Atlantic Program) array at ~60°N has provided new and unprecedented insight into the strength and variability of the meridional overturning circulation in the subpolar North Atlantic. OSNAP has identified
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca9fb3f4bfb7c3e7e185c047e0634fbf
https://doi.org/10.5194/egusphere-egu21-15972
https://doi.org/10.5194/egusphere-egu21-15972
Autor:
Simon A. Josey, G. W. Kent Moore, Ben Moat, Marilena Oltmanns, D. Gwyn Evans, James A. Screen, Johannes Karstensen, N. Penny Holliday
Recent decades have been characterised by amplified Arctic warming and increased occurrence of extreme weather events in the North Atlantic region. While earlier studies noticed statistical links between high-latitude warming and mid-latitude weather
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4be4a128b916cd4a57e97e9dddcd6dd0
https://doi.org/10.5194/egusphere-egu21-5271
https://doi.org/10.5194/egusphere-egu21-5271
Publikováno v:
Geophysical Research Letters (0094-8276) (American Geophysical Union (AGU)), 2019-10, Vol. 46, N. 20, P. 11281-11291
Mooring and glider observations and a high‐resolution satellite sea surface temperature image reveal features of a transient submesoscale front in a typical mid‐ocean region of the Northeast Atlantic. Analysis of the observations suggests that th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d5c1b889b68bf48d17979fcf93622f27
https://archimer.ifremer.fr/doc/00514/62521/
https://archimer.ifremer.fr/doc/00514/62521/