Zobrazeno 1 - 10
of 20
pro vyhledávání: '"K. Anders Olsson"'
Autor:
Christian Marcussen, Björn Eriksson, Timothy Janzen, Benjamin Hell, Dennis Antony, Sara Jutterström, Ludvig Löwemark, Bert Rudels, Emma Sellén, K. Anders Olsson, Johanna Linders, Morten Sölvsten, Martin Jakobsson, Göran Björk, Patrick B. Eriksson, Leif G. Anderson, Sofia Hjalmarsson
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers. 57:577-586
The LOMROG 2007 expedition targeted the previously unexplored southern part of the Lomonosov Ridge north of Greenland together with a section from the Morris Jesup Rise to Gakkel Ridge. The oceanog ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5e1c26044aa65b0228f3aed206ccd5f1
https://doi.org/10.1016/j.dsr.2010.01.006
https://doi.org/10.1016/j.dsr.2010.01.006
Autor:
Tor Eldevik, Anne Britt Sandø, Doroteaciro Iovino, Helge Drange, Jan Even Øie Nilsen, K. Anders Olsson
Publikováno v:
Nature Geoscience
The overflows from the Nordic seas maintain the deep branch of the North Atlantic circulation that is an important part of the global climate system. An analysis of observed ocean temperatures and salinities between 1950 and 2005 shows that the Atlan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::15ef3ab5bd8c6cc69671b12ca7b6abbe
Autor:
Daniel J. Torres, Marika Marnela, Marie-José Messias, James H. Swift, Andrew J. Watson, Emil Jeansson, Bert Rudels, Leif G. Anderson, K. Anders Olsson
Publikováno v:
Progress in Oceanography. 78:1-11
To determine the exchanges between the Nordic Seas and the Arctic Ocean through Fram Strait is one of the most important aspects, and one of the major challenges, in describing the circulation in the Arctic Mediterranean Sea. Especially the northward
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::00ab7f2757a52d8858ef23ac4174f358
https://doi.org/10.1016/j.pocean.2007.06.004
https://doi.org/10.1016/j.pocean.2007.06.004
Autor:
William M. Smethie, E. Peter Jones, James H. Swift, Emil Jeansson, K. Anders Olsson, Leif G. Anderson, Bert Rudels, Sara Jutterström
Publikováno v:
Progress in Oceanography. 78:12-28
Data from the East Greenland Current in 2002 are evaluated using optimum multiparameter analysis. The current is followed from north of Fram Strait to the Denmark Strait Sill and the contributions of different source waters, in mass fractions, are de
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e05c8aca8e23e946b73d05d9e55fa09b
https://doi.org/10.1016/j.pocean.2007.08.031
https://doi.org/10.1016/j.pocean.2007.08.031
Publikováno v:
Journal of Marine Systems. 57:264-288
The dense overflow across the Denmark Strait is investigated with hydrographic and hydro-chemical data and the water mass composition of the Denmark Strait Overflow Water (DSOW) is determined by multivariate analysis. Hydrographical properties, the t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d4796dc21d72d98b0e2a266a6a9424a8
https://doi.org/10.1016/j.jmarsys.2005.05.003
https://doi.org/10.1016/j.jmarsys.2005.05.003
Autor:
T. Tanhua, K. Anders Olsson
Publikováno v:
Marine Chemistry. 94:27-41
The persistence of the anthropogenic halogenated tracers, CFC-11 (CCl3F), CFC-12 (CCl2F2), CFC-113 (CCl2FCClF2), carbon tetrachloride (CCl4) and methyl chloroform (CH3CCl3) in oxygen-depleted waters was investigated in the anoxic fjord Framvaren in s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f70ff0a44571ffe865a075630ba88781
https://doi.org/10.1016/j.marchem.2004.07.009
https://doi.org/10.1016/j.marchem.2004.07.009
Autor:
Leif G. Anderson, Tor Eldevik, Bogi Hansen, K. Anders Olsson, Emil Jeansson, Marie-José Messias, Truls Johannessen, Andrew J. Watson, Regin Kristiansen
Publikováno v:
Deep Sea Research Part I: Oceanographic Research Papers
The Faroe Bank Channel is the deepest passage for dense water leaving the Nordic Seas into the North Atlantic. The contribution to this part of the Greenland-Scotland Overflow by intermediate water from the Greenland Sea is investigated by the tracer
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::beb3065d989e1e1edd60c84a8dd2e167
https://doi.org/10.1016/j.dsr.2004.09.009
https://doi.org/10.1016/j.dsr.2004.09.009
Publikováno v:
Deep Sea Research Part II: Topical Studies in Oceanography. 51:2683-2699
Halogenated transient tracers such as the chlorofluorocarbons CFC-11, CFC-12 and CFC-113 are commonly used in oceanographic studies. These compounds enter the ocean via the atmosphere and their transient atmospheric concentrations make them valuable
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::16abdd88de43cf35b3d9492d01d494d9
https://doi.org/10.1016/j.dsr2.2001.02.001
https://doi.org/10.1016/j.dsr2.2001.02.001
Publikováno v:
Geophysical Research Letters. 36
[1] This study evaluates the presence of intermediate water from the Greenland Sea in the Iceland Basin deduced from the observed excess of the tracer sulphur hexafluoride (SF6), released in the central Greenland Sea in 1996. The large tracer release
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e0d72bcd857bb84e1f717f5a8cc06ac2
https://doi.org/10.1029/2009gl037988
https://doi.org/10.1029/2009gl037988
Publikováno v:
Arctic–Subarctic Ocean Fluxes ISBN: 9781402067730
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::474e6075dc9f2e1d047af5394228bc1f
https://doi.org/10.1007/978-1-4020-6774-7_21
https://doi.org/10.1007/978-1-4020-6774-7_21
