Zobrazeno 1 - 10
of 578
pro vyhledávání: '"Weddell Sea Bottom Water"'
Autor:
Toste Tanhua, Mian Liu
Publikováno v:
Ocean Science, Vol 17, Pp 463-486 (2021)
A large number of water masses are presented in the Atlantic Ocean, and knowledge of their distributions and properties is important for understanding and monitoring of a range of oceanographic phenomena. The characteristics and distributions of wate
Autor:
Tore Hattermann, Christof Lüpkes, Olaf Boebel, Steven Herbette, Nicolas Le Paih, Volker Strass, Gerd Rohardt, Torsten Kanzow
Publikováno v:
Journal of Geophysical Research: Oceans
Journal of Geophysical Research: Oceans, 2020, 125, ⟨10.1029/2020JC016316⟩
Journal Of Geophysical Research-oceans (2169-9275) (American Geophysical Union (AGU)), 2020-10, Vol. 125, N. 10, P. e2020JC016316 (20p.)
Journal of Geophysical Research: Oceans, 2020, 125, ⟨10.1029/2020JC016316⟩
Journal Of Geophysical Research-oceans (2169-9275) (American Geophysical Union (AGU)), 2020-10, Vol. 125, N. 10, P. e2020JC016316 (20p.)
The Weddell Sea is of global importance in the formation of dense bottom waters associated with sea‐ice formation and ocean‐ice sheet interaction occurring on the shelf areas. In this context, the Weddell Sea boundary current system (BCS) present
Publikováno v:
Geophysical Research Letters. 47
The Weddell Sea Bottom Water (WSBW) export from 1999 to 2019 displays distinct seasonal and interannual variability. From 2014 into 2017 a marked salinity decrease was recorded, with the lowest salinity, 34.615, attained in early 2016. The reduced sa
Publikováno v:
Climate Research. 74:171-184
Evidence for a dynamic grounding line in outer Filchner Trough, Antarctica, until the early Holocene
Publikováno v:
Geology. 45:1035-1038
Previous reconstructions of ice-sheet changes in Antarctica’s Weddell Sea sector since the Last Glacial Maximum (LGM) at 19–23 cal. (calibrated) kyr B.P. suffered from large uncertainties and were partly contradictory. As a consequence, the contr
Autor:
Carolina O. Dufour, Hannah Zanowski, Ivy Frenger, Michael Winton, Adele K. Morrison, Stephen M. Griffies
Publikováno v:
Journal of Climate, 30 (19). pp. 7719-7737.
The Weddell Sea polynya is a large opening in the open-ocean sea ice cover associated with intense deep convection in the ocean. A necessary condition to form and maintain a polynya is the presence of a strong subsurface heat reservoir. This study in
Autor:
Thomas J. Bracegirdle, J. Scott Hosking, Gareth J. Marshall, James Pope, Tony Phillips, John Turner, Pranab Deb
Publikováno v:
Geophysical Research Letters. 44:6868-6875
During Austral spring 2016 Antarctic sea ice extent (SIE) decreased at a record rate of 75 × 103 km2 day-1, which was 46% faster than the mean rate and 18% faster than in any previous spring season during the satellite era. The decrease of sea ice a
Publikováno v:
Journal of Climate, 30 (12). pp. 4337-4350.
EPIC3FRISP-Forum for Research into Ice Shelf Processes, Sotra, Norway, 2017-06-19-2017-06-22
EPIC3Journal of Climate, American Meteorological Society, 30, pp. 4337-4350, ISSN: 0894-8755
EPIC3FRISP-Forum for Research into Ice Shelf Processes, Sotra, Norway, 2017-06-19-2017-06-22
EPIC3Journal of Climate, American Meteorological Society, 30, pp. 4337-4350, ISSN: 0894-8755
Warm water of open ocean origin on the continental shelf of the Amundsen and Bellingshausen Seas causes the highest basal melt rates reported for Antarctic ice shelves with severe consequences for the ice shelf/ice sheet dynamics. Ice shelves fringin
Autor:
Denis L. Volkov, Arnold L. Gordon, Hosmay Lopez, Rik Wanninkhof, Sang-Ki Lee, Woo Geun Cheon, Yanyun Liu
Publikováno v:
Journal of Geophysical Research: Oceans. 122:4413-4430
Since late 1978, Antarctic sea-ice extent in the East Pacific has retreated persistently over the Amundsen and Bellingshausen Seas in warm seasons, but expanded over the Ross and Amundsen Seas in cold seasons, while almost opposite seasonal trends ha
Publikováno v:
Paleoceanography. 32:304-317
The Weddell Sea is a main location of bottom water formation and, thus, an important component of global ocean circulation. In this study we examine the ocean and climatic responses to a shelf progradation induced by ice sheet advance and glacially t