Zobrazeno 1 - 4
of 4
pro vyhledávání: '"K. A. Van Scoy"'
Autor:
T. Tanhua, K. A. Olsson, Sólveig Rósa Ólafsdóttir, Andrew J. Watson, Marie-José Messias, J. Balle, Jean-Claude Gascard, Jón Ólafsson, Truls Johannessen, Sheldon Bacon, Noam Bergman, K. A. Van Scoy, Knud Simonsen, Kevin I. C. Oliver, E. Fogelqvist, James R. Ledwell, Magnús Danielsen, Gereon Budéus, Emil Jeansson
Publikováno v:
Progress in Oceanography
Progress in Oceanography, 2008, 78, pp.85-105. ⟨10.1016/j.pocean.2007.06.005⟩
Progress in Oceanography, 2008, 78, pp.85-105. ⟨10.1016/j.pocean.2007.06.005⟩
International audience; In summer 1996, a tracer release experiment using sulphur hexafluoride (SF 6) was launched in the intermediate-depth waters of the central Greenland Sea (GS), to study the mixing and ventilation processes in the region and its
Autor:
Philip D. Nightingale, Timothy P. Stanton, Andrew J. Watson, Kurt R. Buck, K. A. Van Scoy, Mikel Latasa, Kenneth S. Johnson, John H. Martin, W. Yao, Craig N. Hunter, Zbigniew Kolber, J. Z. Zhang, Suzanne M. Turner, Steve E. Fitzwater, Steven T. Lindley, S. J. Tanner, Francisco P. Chavez, Sallie W. Chisholm, Kenneth H. Coale, Kitack Lee, Angela D. Hatton, Frank J. Millero, Richard M. Greene, Michael Ondrusek, Frank E. Hoge, R. D. Ling, Gernot E. Friederich, A. Anderson, Teresa L. Coley, Cliff S. Law, Jocelyn L. Nowicki, Robert R. Bidigare, M.I. Liddicoat, Virginia A. Elrod, Peter S. Liss, Carole M. Sakamoto, Clare E. Collins, Richard T. Barber, R. M. Gordon, James K. Yungel, Paul G. Falkowski, J. Stockel, Robert N. Swift, Neil Tindale
Publikováno v:
Nature. 371:123-129
The idea that iron might limit phytoplankton growth in large regions of the ocean has been tested by enriching an area of 64 km2 in the open equatorial Pacific Ocean with iron. This resulted in a doubling of plant biomass, a threefold increase in chl
Autor:
Wensheng Yao, Frank J. Millero, K. A. Van Scoy, Rik Wanninkhof, M.I. Liddicoat, Gernot E. Friederich, Cliff S. Law, Andrew J. Watson, Kenneth H. Coale, Richard T. Barber
Publikováno v:
Nature. 371:143-145
IT has long been hypothesized that iron concentrations limit phyto-plankton productivity in some parts of the ocean1–3. As a result, iron may have played a role in modulating atmospheric CO2 levels between glacial and interglacial times4, and it ha
Autor:
Truls Johannessen, J. A. Kruepke, Marie-José Messias, K. A. Olsson, David P. Stevens, T. Tanhua, K. A. Van Scoy, F. Carse, Knud Simonsen, Kevin I. C. Oliver, Eric Guilyardi, D. J. Cooper, E. Fogelqvist, James R. Ledwell, Andrew J. Watson, Eystein Jansen, Francisco Escobar del Rey
Publikováno v:
ResearcherID
Convective vertical mixing in restricted areas of the subpolar oceans, such as the Greenland Sea, is thought to be the process responsible for forming much of the dense water of the ocean interior1,2. Deep-water formation varies substantially on annu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fd1c9f14b06c1e9f1bb9e3b695f55b34
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http://gateway.webofknowledge.com/gateway/Gateway.cgi?GWVersion=2&SrcAuth=ORCID&SrcApp=OrcidOrg&DestLinkType=FullRecord&DestApp=WOS_CPL&KeyUT=WOS:000083464700054&KeyUID=WOS:000083464700054