Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Gillian Damerell"'
Autor:
Karen J. Heywood, Esther Portela, Walker Smith, Gillian Damerell, Peter Sheehan, Meredith Meyer
Relatively warm modified Circumpolar Deep Water accesses the southern Ross Sea steered by bathymetric troughs. There it provides nutrients to support phytoplankton blooms in spring, and heat to melt the Ross Ice Shelf. Here we present new observation
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f8338270ab567ea7b598907ab49660d4
https://doi.org/10.5194/egusphere-egu23-9657
https://doi.org/10.5194/egusphere-egu23-9657
Autor:
Karen J. Heywood, Ria Oelerich, Peter Sheehan, Gillian Damerell, Andrew Thompson, Michael Schodlok, Mar Flexas
The circulation of the Bellingshausen Sea has not attracted as much attention as that of its neighbours, the Amundsen Sea and the West Antarctic Peninsula. Like them, it hosts a wide variety of vulnerable ice shelves, and exhibits inflows of warm dee
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6f2f481ef3f30b85e4b543ae4f2161b0
https://doi.org/10.5194/egusphere-egu22-2561
https://doi.org/10.5194/egusphere-egu22-2561
Ocean gliders enable us to collect the ocean microstructure observations necessary to calculate the dissipation rate of turbulent kinetic energy, ε, on timescales of weeks to months: far longer than is normally possible using traditional ship-based
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::cd7c615f72c175d54c9305b75c132617
https://doi.org/10.5194/egusphere-egu22-2848
https://doi.org/10.5194/egusphere-egu22-2848
Publikováno v:
Ocean Science, Vol 15, Pp 1439-1453 (2019)
Internal tide energy flux is an important diagnostic for the study of energy pathways in the ocean, from large-scale input by the surface tide to small-scale dissipation by turbulent mixing. Accurate calculation of energy flux requires repeated full-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::51b947617aa4bdf5a094d814f423c20c
https://doi.org/10.5194/os-15-1439-2019
https://doi.org/10.5194/os-15-1439-2019
In July 2016, a Seaglider equipped with a microstructure sensor system was deployed in the southern Bay of Bengal at 7° 54.0′ N, 89° 4.5′ E. 162 profiles (of which 146 were to 1000 m) of microstructure shear and temperature were collected as a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9047c9d851c6e277445cd57d891acfb8
https://doi.org/10.5194/egusphere-egu21-1295
https://doi.org/10.5194/egusphere-egu21-1295
The continental shelf of the Bellingshausen Sea, located between the West Antarctic Peninsula and the Amundsen Sea, Antarctica, is poorly investigated, compared with its neighbours. Here, the southernmost frontal jet of the Antarctic Circumpolar Curr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::beede9ae4996280edc4dbd41934ece49
https://doi.org/10.5194/egusphere-egu21-4788
https://doi.org/10.5194/egusphere-egu21-4788
Autor:
A. Grant, Stephen E. Belcher, Karen J. Heywood, Daley Calvert, Michael J. Bell, Gillian Damerell
Five upper ocean mixed layer models driven by ERA-Interim surface forcing are compared with a year of hydrographic observations of the upper 1000 m, taken at the Porcupine Abyssal Plain observatory site using profiling gliders. All the models reprodu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ba75674740950e56f78bf8642d8d1150
https://ueaeprints.uea.ac.uk/id/eprint/75131/
https://ueaeprints.uea.ac.uk/id/eprint/75131/
Autor:
Anna Rumyantseva, Adrian Martin, Umberto Binetti, Stephanie A. Henson, Gillian Damerell, Jan Kaiser, Karen J. Heywood
Publikováno v:
Progress in Oceanography
As part of the OSMOSIS project, a fleet of gliders surveyed the Porcupine Abyssal Plain site (Northeast Atlantic) from September 2012 to September 2013. Salinity, temperature, dissolved oxygen concentration and chlorophyll fluorescence were measured
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0918afc9e32551cc06c6c633eb787239
https://ueaeprints.uea.ac.uk/id/eprint/74159/
https://ueaeprints.uea.ac.uk/id/eprint/74159/
The Bellingshausen Sea, located between the West Antarctic Peninsula and the Amundsen Sea, is poorly observed, compared with its neighbours. The Antarctic Slope Front (ASF), that rings the continental slope of Antarctica, supports a westward current
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::93dc7e2c4895d663a76e46d870145a68
https://doi.org/10.5194/egusphere-egu2020-463
https://doi.org/10.5194/egusphere-egu2020-463
Sea surface temperature (SST) seasonal extrema are important for water mass formation, intensification of tropical cyclones and coral bleaching, so should be well-represented in models used for future climate projections. Typically, climate model eva
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6c2797e337cb31334e60589143eeb84a
https://doi.org/10.5194/egusphere-egu2020-702
https://doi.org/10.5194/egusphere-egu2020-702