Ad
related to: tom garrison oceanography pdf
Search results
Results From The WOW.Com Content Network
In oceanography, a halocline (from Greek hals, halos 'salt' and klinein 'to slope') is a cline, a subtype of chemocline caused by a strong, vertical salinity gradient within a body of water. [1] Because salinity (in concert with temperature ) affects the density of seawater , it can play a role in its vertical stratification .
Moskstraumen [1] is a system of tidal eddies and whirlpools, one of the strongest in the world, [2] that forms at the Lofoten archipelago in Nordland county, Norway between the Norwegian Sea and the Vestfjorden.
Introduction to Physical Oceanography (PDF). College Station: Texas A&M University. ISBN 978-1-61610-045-2. OCLC 169907785. Willen E. (2005). "A new species of Paranannopus Lang, 1936 (Copepoda, Harpacticoida, Pseudotachidiidae) with atrophic mouthparts from the abyssal of the Angola Basin". Organisms Diversity & Evolution. 5 (Supplement 1): 19 ...
Regional Ocean Modeling System (ROMS) is a free-surface, terrain-following, primitive equations ocean model widely used by the scientific community for a diverse range of applications.
MV Liberty Star carrying the DeepWorker 2000 submersible. DeepWorker 2000 is a submarine vehicle developed by Nuytco Research, Ltd. It is capable of descending to a depth of 610 m (2001 ft) and remaining submerged for 12 hours.
AMOC-Index since 900 CE with pronounced slowdown since ~1850; Rahmstorf et al. (2015) [5] Climate scientists Michael Mann of Penn State and Stefan Rahmstorf from the Potsdam Institute for Climate Impact Research suggested that the observed cold pattern during years of temperature records is a sign that the Atlantic Ocean's Meridional overturning circulation (AMOC) may be weakening.
T-S diagram of a station in the North Pacific. In oceanography, temperature-salinity diagrams, sometimes called T-S diagrams, are used to identify water masses.In a T-S diagram, rather than plotting each water property as a separate "profile," with pressure or depth as the vertical coordinate, potential temperature (on the vertical axis) is plotted versus salinity (on the horizontal axis).
Paleoceanography makes use of so-called proxy methods as a way to infer information about the past state and evolution of the world's oceans. Several geochemical proxy tools include long-chain organic molecules (e.g. alkenones), stable and radioactive isotopes, and trace metals. [1]