High salinity shelf water
WebApr 18, 2024 · The low salinity shelf outflow directly enters the upper estuarine loop, and the shelf seas farther east, the East Siberian and Chukchi Seas, almost exclusively feed the upper loop. The waters on the shelves are supplied by river runoff and also by a more saline water mass that provides the saline mixing end member. WebMar 19, 2024 · High Salinity Shelf Water production in Terra Nova Bay, Ross Sea from high-resolution near-surface salinity observations Preprint Full-text available Sep 2024 Una …
High salinity shelf water
Did you know?
WebMar 9, 2012 · Sensitivity of coastal polynyas and high-salinity shelf water production in the Ross Sea, Antarctica, to the atmospheric forcing Pierre Mathiot, Nicolas C. Jourdain, Bernard Barnier, Hubert Gallée, Jean Marc Molines, Julien Le Sommer & Thierry Penduff Ocean Dynamics 62 , 701–723 ( 2012) Cite this article 644 Accesses 21 Citations Metrics Abstract WebFeb 28, 2024 · The TNBP is well known for a great heat flux per area and high ice formation rates 4, 9, 11, although the area of TNBP is small (annual average ~4200 km 2) 27. Numerical modeling suggests that...
WebJun 28, 2005 · This paper presents results from a model study of the interannual variability of high salinity shelf water (HSSW) properties in the Ross Sea. Salinity and potential … WebSep 14, 2024 · In this part of Prydz Bay, salinities did not attain values as high as those in what is called High Salinity Shelf Water (HSSW; S < 34.6 PSS78) in the Weddell Sea, and therefore are unlikely to contribute to bottom water formation (Reference Carmack and Untersteiner Carmack, 1986). Initial CTD data from moorings at similar depths in the …
WebDec 15, 1991 · A model of the flow and salinity fields forced by sea-surface salinity flux and wind stress curl is developed and used to examine the processes that create High … WebMar 9, 2012 · During sea-ice production, salt is rejected and the salinity of surface waters increases. This leads to convection in polynyas with a deepening of the mixed layer. …
WebMar 21, 2024 · Key Points. The salt advection is important for the production of High Salinity Shelf Water in the polynyas of the Ross Sea continental shelf. Within the polynyas, brine …
WebThe water column is destratified to ~350-m depth by the end of September, and the mixed-layer salinity reaches ~34.5 g kg −1, as observed. If the contribution from meteoric water is not taken into account, convection extends to the seafloor and the mixed-layer salinity (~34.6 g kg −1) is higher than observed. chili\u0027s irresistible bowlsWebWe finally take the median of all the combinations: temperature or salinity, NADW properties from SPG or GIN, and AABW or NADW contents. For the NADW layer, we detect the NADW core as the maximum NADW content with the extra criterion that the maximum must be larger than 80 % NADW. grace baptist church twin falls idahoWebSep 15, 2008 · The higher the saline content in water the heavier the water. This causes it to sink towards the bottom and water with lower levels will rise to the top. It will remain so unless stirred... grace baptist church virginia mnWebThe formation of High-Salinity Shelf Water (HSSW), which is the major source of Antarctic bottom water (AABW), has been observed in Terra Nova Bay (TNB) in Antarctica. We believe that a description of the spatio-temporal variation of salinity in TNB would help understand the production of HSSW in the region. chili\u0027s irving 635WebApr 11, 2024 · Coastal polynyas in the Ross Sea are important source regions of high salinity shelf water (HSSW) – the precursor of Antarctic Bottom Water that supplies the lower limb of the thermohaline circulation. Here, the response of sea ice production and HSSW formation to synoptic- and meso-scale cyclones was investigated for the Ross Ice … grace baptist church troygrace baptist church walworth nyWebIce formation increases sea-surface salinity and produces High Salinity Shelf Water (HSSW) that presents a salinity value greater than 34.62. HSSW is formed mostly in the TNB area during winter ( Budillon et al., 2003 ), spreads northwards following the Drygalski Basin, and finally flows off the shelf near Cape Adare, where it mixes with CDW to ... chili\u0027s iron point road folsom