Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Michael Schindelegger"'
Publikováno v:
Communications Earth & Environment, Vol 5, Iss 1, Pp 1-13 (2024)
Abstract Stratification—that is, the vertical change in seawater density—exerts a subtle control on the energetics and thus the surface elevation of barotropic (depth independent) flows in the ocean. Changes in stratification therefore provide a
Externí odkaz:
https://doaj.org/article/5eacecdb82a9400f9f5818fcabbd8d06
Autor:
Kristin N. Barton, Nairita Pal, Steven R. Brus, Mark R. Petersen, Brian K. Arbic, Darren Engwirda, Andrew F. Roberts, Joannes J. Westerink, Damrongsak Wirasaet, Michael Schindelegger
Publikováno v:
Journal of Advances in Modeling Earth Systems, Vol 14, Iss 11, Pp n/a-n/a (2022)
Abstract We examine ocean tides in the barotropic version of the Model for Prediction Across Scales (MPAS‐Ocean), the ocean component of the Department of Energy Earth system model. We focus on four factors that affect tidal accuracy: self‐attrac
Externí odkaz:
https://doaj.org/article/2e00899e3b874839b3f9a91d39d2c832
Autor:
Michael Schindelegger
The lunar semidiurnal (M2) tide of the Gulf of Maine and Bay of Fundy is remarkable not only for its large amplitude but also for its spatially coherent temporal changes of ∼1–3 cm on secular to seasonal time scales. Previous work suggests a role
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d3ddaf2dc61c5382b14761b9c741b6a1
https://doi.org/10.5194/egusphere-egu23-17440
https://doi.org/10.5194/egusphere-egu23-17440
Simulations of the tides from the Last Glacial Maximum (26.5 – 19 kyr BP) to the present show large amplitude and dissipation changes, especially in the semi-diurnal band during the deglacial period. New reconstructions of global ice sheet history
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e30747a502551c7dfe73e5983bea4cd
https://doi.org/10.5194/egusphere-egu23-9698
https://doi.org/10.5194/egusphere-egu23-9698
Low-frequency non-astronomical changes of ocean tides of (1 cm) have been documented in water level measurements around the globe, but their causative mechanisms remain poorly understood in many cases. While anthropogenic developments (e.g., harbor d
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53a6747d1db2a6b474e0bf35a1f39543
https://doi.org/10.5194/egusphere-egu23-11720
https://doi.org/10.5194/egusphere-egu23-11720
Autor:
Rory Barnes, Amani E. Becker, David Bowers, Elizabeth Bradshaw, Lucy M. Bricheno, Jennifer M. Brown, Susana Custódio, Hannah S. Davies, João C. Duarte, Stéphanie Dumont, Mattias Green, David Hadley-Pryce, Angela Hibbert, Harriet C.P. Lau, Yueng-Djern Lenn, Alberto Mavume, Fialho Nehama, Simona Petrosino, Alex J. Poulton, Takatoshi Sakazaki, Michael Schindelegger, Christopher Scotese, Gianluca Sottili, Bernadette Tessier, Amanda M. Thomas, Katsuto Uehara, Sophie Ward, Sophie-Berenice Wilmes, Philip L. Woodworth
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3e82c04f027622ac2379d0a5bd462b3a
https://doi.org/10.1016/b978-0-323-90851-1.09992-1
https://doi.org/10.1016/b978-0-323-90851-1.09992-1
Autor:
Michael Schindelegger, Daniel P. Kotzian, Richard D. Ray, J. A. Mattias Green, Sophie Stolzenberger
Publikováno v:
Geophysical Research Letters. 49
Autor:
Steven R. Brus, Kristin N. Barton, Nairita Pal, Andrew F. Roberts, Darren Engwirda, Mark R. Petersen, Brian K. Arbic, Damrongsak Wirasaet, Joannes J. Westerink, Michael Schindelegger
Publikováno v:
Ocean Modelling. 182:102160