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The journal and all its back issues, dating to 1988, are available both in print and in full PDF format online in the journal website's archives. Oceanography is abstracted and indexed in the Science Citation Index Expanded. According to the Journal Citation Reports, the journal had an impact factor of 3.431 in 2019. [1]
co-founding editor of the journal Deep-Sea Research, founding editor of the journal Progress in Oceanography Mary Sears (July 18, 1905 – September 2, 1997) was a commander in the United States Naval Reserve and an oceanographer at the Woods Hole Oceanographic Institution (WHOI).
The Great Salinity Anomaly (GSA) originally referred to an event in the late 1960s to early 1970s where a large influx of freshwater from the Arctic Ocean led to a salinity anomaly in the northern North Atlantic Ocean, which affected the Atlantic meridional overturning circulation. [1]
Journal of Geophysical Research. 111 (C11). Bibcode:2006JGRC..11111010S. doi: 10.1029/2005jc003424. ISSN 0148-0227. Woodgate, Rebecca A. (2018-01-01). "Increases in the Pacific inflow to the Arctic from 1990 to 2015, and insights into seasonal trends and driving mechanisms from year-round Bering Strait mooring data". Progress in Oceanography.
The Journal of Physical Oceanography is a peer-reviewed scientific journal published by the American Meteorological Society. It was established in January 1971 and is available on the web since 1996. Online articles older than one year are available as open access. The editor-in-chief is Jerome Smith (Scripps Institution of Oceanography).
Wheeler grew up in Garden Grove, California and received her education at University of California, Irvine where she earned her B.S. and MS. Degrees, as well as earning her Ph.D. in 1976 studying in the laboratory of Grover C. Stephens.
Transparent exopolymer particles (TEPs) are extracellular acidic polysaccharides produced by phytoplankton and bacteria in saltwater, freshwater, and wastewater. [1] They are incredibly abundant and play a significant role in biogeochemical cycling of carbon and other elements in water. [2]
A baroclinic instability is a fluid dynamical instability of fundamental importance in the atmosphere and ocean. It can lead to the formation of transient mesoscale eddies, with a horizontal scale of 10-100 km. [1] [2] In contrast, flows on the largest scale in the ocean are described as ocean currents, the largest scale eddies are mostly created by shearing of two ocean currents and static ...