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- 1From:Science (Vol. 298, Issue 5599) Peer-ReviewedOn page 1769 of this issue, Adkins et al. (1) report data constraining the salinity (and density) of ocean deep waters during the last glacial period. In contrast to today's ocean, they find that at the last glacial...
- 2From:Science (Vol. 249, Issue 4971) Peer-ReviewedQuaternary Deepwater Paleoceanography THE CIRCULATION AND CHEMISTRY OF THE DEEP OCEAN play major roles in maintenance of the earth's climate and must be undestood in order to assess and to predict climate change. Deep...
- 3From:Science (Vol. 264, Issue 5162) Peer-ReviewedOcean models routinely used in simulations of the Earth's climate do not resolve mesoscale eddies because of the immense computational cost. A new parameterization of the effects of these eddies has been implemented in a...
- 4From:Nature (Vol. 525, Issue 7570) Peer-ReviewedAuthor(s): Jaime Palter (corresponding author) [1] Seawater absorbs most sunlight within 100 metres of the ocean's surface, where available inorganic nutrients are rapidly assimilated by photosynthesizing plankton....
- 5From:Climate of the Past (Vol. 9, Issue 3) Peer-ReviewedByline: C. F. Schleussner, G. Feulner To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
- 6From:Biogeosciences (Vol. 10, Issue 7) Peer-ReviewedByline: Y. Choi, S. Kida, K. Takahashi To access, purchase, authenticate, or subscribe to the full-text of this article, please visit this link:...
- 7From:Science (Vol. 276, Issue 5322) Peer-ReviewedThe provenance of ice-rafted debris (IRD) in four Arctic sediment cores implies that icebergs from the northwestern Laurentide ice sheets drifted across the western Arctic Ocean along the 180 [degrees]-0 [degrees]...
- 8From:Environmental Reviews (Vol. 17) Peer-ReviewedSystematic monitoring of seabird populations in Canada has been ongoing since the 1920s and the monitoring of diets and other biological indicators of ecosystem change started in the 1970s. Long-term monitoring of...
- 9From:Climate Dynamics (Vol. 43, Issue 3-4) Peer-ReviewedThis work evaluates the performance of several global climate models (GCMs) as forcing of a regional ocean model configuration centered in the Iberian Basin. The study is divided in two parts. First, the output of nine...
- 10From:Geofizika (Vol. 26, Issue 2) Peer-ReviewedFifteen open-sea time-series observations of tidal velocities and tidal bottom pressures for more than six months duration provide a new database for North Adriatic tides. The observations show nearly reversing tidal...
- 11From:Climate Dynamics (Vol. 38, Issue 9-10) Peer-ReviewedArabian Sea Mini Warm Pool (ASMWP) is a part of the Indian Ocean Warm Pool and formed in the eastern Arabian Sea prior to the onset of the summer monsoon season. This warm pool attained its maximum intensity during the...
- 12From:Climate Dynamics (Vol. 52, Issue 7-8) Peer-ReviewedThe tropical Indian Ocean sea level displayed decadal variations in response to Pacific Decadal Oscillation (PDO). Contrasting patterns of decadal oscillation in sea level is found during the opposite phases of PDO...
- 13From:Nature (Vol. 554, Issue 7693) Peer-ReviewedAuthor(s): Fiz F. Perez (corresponding author) [1]; Marcos Fontela [1]; Maribel I. Garca-Ibez [1]; Herl Mercier [2]; Anton Velo [1]; Pascale Lherminier [2]; Patricia Zunino [2]; Mercedes de la Paz [1]; Fernando...
- 14From:Geoscientific Model Development (Vol. 13, Issue 11) Peer-ReviewedOcean biogeochemical models are key tools for both scientific and operational applications. Nevertheless the cost of these models is often expensive because of the large number of biogeochemical tracers. This has...
- 15From:Nature (Vol. 575, Issue 7782) Peer-ReviewedAs the seas rise, our understanding of the processes within them must deepen. As the seas rise, our understanding of the processes within them must deepen. Author(s): Richard Hodson Author Affiliations:...
- 16From:Atmosphere (Vol. 11, Issue 6) Peer-ReviewedThis study investigates the physical processes controlling the mixed layer buoyancy using a regional configuration of an ocean general circulation model. Processes are quantified by using a linearized equation of state,...
- 17From:Climate of the Past (Vol. 12, Issue 4) Peer-ReviewedGlobal warming during the Paleocene-Eocene Thermal Maximum (PETM) ââ¼ââ¯55 million years ago (Ma) coincided with a...
- 18From:PLoS ONE (Vol. 7, Issue 9) Peer-ReviewedThe Indian Ocean is the least known ocean in the world with the biogeography of marine species in the West Indian Ocean (WIO) understudied. The hydrography of WIO is characterized by four distinct oceanographic systems...
- 19From:Geoscientific Model Development (Vol. 8, Issue 7) Peer-ReviewedThe natural abundance of .sup.14 C in total CO.sub.2 dissolved in seawater (DIC) is a property applied to evaluate the water age structure and circulation in the ocean and in ocean models. In this study we use three...
- 20From:Climate Dynamics (Vol. 46, Issue 5-6) Peer-ReviewedEl Nino-Southern Oscillation (ENSO) is the leading mode of interannual global climate variability, which in its essence is often described by the equatorial dynamics of the recharge oscillator with a fixed pattern. Here...