Zobrazeno 1 - 10
of 89
pro vyhledávání: '"D. Quadfasel"'
Autor:
S. Østerhus, R. Woodgate, H. Valdimarsson, B. Turrell, L. de Steur, D. Quadfasel, S. M. Olsen, M. Moritz, C. M. Lee, K. M. H. Larsen, S. Jónsson, C. Johnson, K. Jochumsen, B. Hansen, B. Curry, S. Cunningham, B. Berx
Publikováno v:
Ocean Science, Vol 15, Pp 379-399 (2019)
The Arctic Mediterranean (AM) is the collective name for the Arctic Ocean, the Nordic Seas, and their adjacent shelf seas. Water enters into this region through the Bering Strait (Pacific inflow) and through the passages across the Greenland–Scotla
Externí odkaz:
https://doaj.org/article/69cd8ba8071d4d8aa4796fb19a849ab7
Publikováno v:
Ocean Science, Vol 14, Pp 871-885 (2018)
The Iceland–Faroe Ridge (IFR) is considered to be the third most important passage for dense overflow water from the Nordic Seas feeding into the lower limb of the Atlantic Meridional Overturning Circulation with a volume transport on the order
Externí odkaz:
https://doaj.org/article/2dbc563114d8493cb606d74605763b60
Autor:
B. Hansen, T. Poulsen, K. M. Húsgarð Larsen, H. Hátún, S. Østerhus, E. Darelius, B. Berx, D. Quadfasel, K. Jochumsen
Publikováno v:
Ocean Science, Vol 13, Pp 873-888 (2017)
Through the Faroese Channels – the collective name for a system of channels linking the Faroe–Shetland Channel, Wyville Thomson Basin, and Faroe Bank Channel – there is a deep flow of cold waters from Arctic regions that exit the system as o
Externí odkaz:
https://doaj.org/article/8991f9d54e0e44768cfa320cf98643e7
Biased thermohaline exchanges with the Arctic across the Iceland–Faroe Ridge in ocean climate models
Publikováno v:
Ocean Science, Vol 12, Iss 2, Pp 545-560 (2016)
The northern limb of the Atlantic thermohaline circulation and its transport of heat and salt towards the Arctic strongly modulate the climate of the Northern Hemisphere. The presence of warm surface waters prevents ice formation in parts of the Arct
Externí odkaz:
https://doaj.org/article/68e9f5d18e584c09a7a0e64c90be8009
Publikováno v:
Ocean Science, Vol 9, Iss 6, Pp 1003-1014 (2013)
To examine processes controlling the entrainment of ambient water into the Denmark Strait overflow (DSO) plume/gravity current, measurements of turbulent dissipation rate were carried out by a quasi-free-falling (tethered) microstructure profiler (MS
Externí odkaz:
https://doaj.org/article/91d6312847d847b8b6728d67c4ea9ecd
Autor:
G. Voet, D. Quadfasel
Publikováno v:
Ocean Science, Vol 6, Iss 1, Pp 301-310 (2010)
The entrainment of buoyant ambient water into the overflow plume of Denmark Strait and the associated downstream warming of the plume are estimated using time series of currents and temperature from moored instrumentation and classical hydrographic d
Externí odkaz:
https://doaj.org/article/28eb636cbb9c44a1a20053094d3bb47f
Autor:
B. Rudels, R. Meyer, E. Fahrbach, V. V. Ivanov, S. Østerhus, D. Quadfasel, U. Schauer, V. Tverberg, R. A. Woodgate
Publikováno v:
Annales Geophysicae, Vol 18, Pp 687-705 (2000)
The water mass distribution in northern Fram Strait and over the Yermak Plateau in summer 1997 is described using CTD data from two cruises in the area. The West Spitsbergen Current was found to split, one part recirculated towards the west, while
Externí odkaz:
https://doaj.org/article/cfca181e9e4d44d8858d69ea9650e244
Autor:
S. Østerhus, R. Woodgate, H. Valdimarsson, B. Turrell, L. de Steur, D. Quadfasel, S. M. Olsen, M. Moritz, C. M. Lee, K. M. H. Larsen, S. Jónsson, C. Johnson, K. Jochumsen, B. Hansen, B. Curry, S. Cunningham, B. Berx
Publikováno v:
Ocean Science
Ocean Science, Vol 15, Pp 379-399 (2019)
Ocean Science, Vol 15, Pp 379-399 (2019)
The Arctic Mediterranean (AM) is the collective name for the Arctic Ocean, the Nordic Seas, and their adjacent shelf seas. Water enters into this region through the Bering Strait (Pacific inflow) and through the passages across the Greenland–Scotla
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0ddb69cc40f2f5ee3e92c4e7d5a8c135
https://doi.org/10.5194/os-2018-114
https://doi.org/10.5194/os-2018-114
Autor:
B. Rudels, R. Meyer, E. Fahrbach, V. V. Ivanov, S. Østerhus, D. Quadfasel, U. Schauer, V. Tverberg, R. A. Woodgate
Publikováno v:
Annales Geophysicae, Vol 18, Iss 6, Pp 687-705 (0000)
Annales Geophysicae
Annales Geophysicae, European Geosciences Union, 2000, 18 (6), pp.687-705
Annales Geophysicae, Vol 18, Pp 687-705 (2000)
Annales Geophysicae
Annales Geophysicae, European Geosciences Union, 2000, 18 (6), pp.687-705
Annales Geophysicae, Vol 18, Pp 687-705 (2000)
The water mass distribution in northern Fram Strait and over the Yermak Plateau in summer 1997 is described using CTD data from two cruises in the area. The West Spitsbergen Current was found to split, one part recirculated towards the west, while th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::5ffd95f689b5c68f6732b9a153285a80
https://www.ann-geophys.net/18/687/2000/
https://www.ann-geophys.net/18/687/2000/