Dense shelf water spreading from Antarctic coastal polynyas to the deep Southern Ocean: A regional circumpolar model study. Issue 8 (4th August 2017)

• Record Type: Journal Article
• Authors: Kusahara, Kazuya; Williams, Guy D.; Tamura, Takeshi; Massom, Robert; Hasumi, Hiroyasu
• Is Part Of: Journal of geophysical research. Volume 122:Issue 8(2017)
• Page Start: 6238
• Page End: 6253
• Publication Date: 2017-08-04
• Subjects: Antarctic dense shelf water -- Antarctic coastal polynyas -- DSW pathways over the Southern Ocean -- passive tracer experiments; Oceanography -- Periodicals; 551.4605
• DOI: 10.1002/2017JC012911
• Languages: English
• ISSNs: 2169-9275

Abstract

Abstract: The spreading of dense shelf water (DSW) from Antarctic coastal margins to lower latitudes plays a vital role in the ocean thermohaline circulation and the global climate system. Through enhanced localized sea ice production in Antarctic coastal polynyas, cold and saline DSW is formed over the continental shelf regions as a precursor to Antarctic Bottom Water (AABW). However, the detailed fate of coastal DSW over the Southern Ocean is still unclear. Here we conduct extensive passive tracer experiments using a circumpolar ocean‐sea ice‐ice shelf model to investigate pathways of the regional polynya‐based DSW from the Antarctic margins to the deep Southern Ocean basins. In the numerical experiments, the Antarctic coastal margin is divided into nine regions, and a passive tracer is released from each region at the same rate as the local sea ice production. The modeled spatial distribution of the total concentration of the nine tracers is consistent with the observed AABW distribution and clearly demonstrates nine routes of the DSW over the Southern Ocean along its bottom topography. Furthermore, the model shows that while ∼50% of the total tracer is distributed northward from the continental shelf to the deep ocean, ∼7% is transported poleward beneath ice shelf cavities. The comprehensive tracer experiments allow us to estimate the contribution of local DSW to the total concentration along each of the pathways. Key Points: Passive tracer experiments detail the export of DSW formed in Antarctic coastal polynyas to the offshore basins of the Southern Ocean Nine key pathways of DSW over the Southern Ocean are described The contributions of regional DSW formation and distributions are estimated