Editing Ross Sea (section)

=== Circulation ===
[[File:Bloom in the Ross Sea.jpg|thumb|Bloom in the Ross Sea, January 2011]]

The Ross Sea circulation, dominated by [[polynya]] processes, is in general very slow-moving. [[Circumpolar Deep Water]] (CDW) is a relatively warm, salty and nutrient-rich water mass that flows onto the continental shelf at certain locations in the Ross Sea. Through heat flux, this water mass moderates the ice cover.  The near-surface water also provides a warm environment for some animals and nutrients to excite primary production. CDW transport onto the shelf is known to be persistent and periodic, and is thought to occur at specific locations influenced by bottom topography.  The circulation of the Ross Sea is dominated by a wind-driven [[gyre]]. The flow is strongly influenced by three submarine ridges that run from southwest to northeast. Flow over the shelf below the surface layer consists of two anticyclonic gyres connected by a central cyclonic flow. The flow is considerable in spring and winter, due to influencing tides. The Ross Sea is covered with ice for much of the year and ice concentrations and in the south-central region little melting occurs.  Ice concentrations in the Ross Sea are influenced by winds with ice remaining in the western region throughout the austral spring and generally melting in January due to local heating. This leads to extremely strong stratification and shallow mixed layers in the western Ross Sea.<ref>{{cite web |url=http://www.ccpo.odu.edu/~klinck/Reprints/PDF/dinnimanDSR03.pdf |title=Archived copy |access-date=2013-12-23 |url-status=dead |archive-url=https://web.archive.org/web/20131224113244/http://www.ccpo.odu.edu/~klinck/Reprints/PDF/dinnimanDSR03.pdf |archive-date=24 December 2013 |df=dmy-all }}</ref> Observation and data access in the region is coordinated by the Ross Sea Working Group of the [[Southern_Ocean_Observing_System_(SOOS)|Southern Ocean Observing System]].