Salinity and temperature budgets in the Ross Sea inner continental shelf
编号:743 访问权限:仅限参会人 更新:2024-12-31 10:40:53 浏览:188次 张贴报告

报告开始:2025年01月15日 17:05(Asia/Shanghai)

报告时间:15min

所在会场:[S7] Session 7-Advances in the Oceanography of the Ross Sea [S7-P] Advances in the Oceanography of the Ross Sea

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摘要
The Ross Ice Shelf (RIS) polynya is one of the major production sites of the Dense Shelf Water (DSW), which is the precursor of the Antarctic Bottom Water that fills the deep ocean basin. Over the Ross Sea continental shelf, DSW is modified by local and remote water masses such as the Ice Shelf Water, Circumpolar Deep Water and the remnant summer surface water; the production rate of Antarctic Bottom Water is thus modulated by the exchange of DSW with these water masses.

Using a combined dataset of historical bottle/CTD measurements, autonomous profiling floats, seal-borne CTD tags and glider surveys, this study generates a monthly climatology of temperature and salinity in the RIS polynya and inner continental shelf to reveal the seasonal evolution of water masses and water column stratification. The climatology shows an evident annual cycle in the RIS polynya, where surface stratification begins to develop in November and reaches maximum (N2=2×10-4 s-2) in January, then decreases and drops below 1×10-5 s-2 in May. During austral summer, air-sea fluxes raise surface bulk temperature to -0.5°C in the inner continental shelf, where the heat is preserved in subsurface layers over a few months. Strong glacial influence is found in the RIS polynya, where salinity is consistently lower (by up to 0.05 PSU) compared with the inner continental shelf. No clear evidence of Circumpolar Deep Water influence is found in the RIS polynya.

Using a reduced-physics box model, salinity and temperature budgets in the RIS polynya and the RIS cavity is estimated based on the newly formed climatology. Results reveal a total heat loss rate of 7×1012 W from the cavity sea water to the ice shelf, which is balanced by advective heat flux driven by exchange flow. Heat loss to the RIS is accompanied by glacial basal melting, which reduces the formation rate of DSW in the RIS polynya and weakens the exchange flow. This is a potential negative feedback mechanism that regulates DSW production in the Ross Sea continental shelf.
 
关键词
tracer budgets, climatology, box model
报告人
Chuning Wang
Postdoctor Shanghai Jiao Tong University

稿件作者
Chuning Wang Shanghai Jiao Tong University
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重要日期
  • 会议日期

    01月13日

    2025

    01月17日

    2025

  • 09月27日 2024

    初稿截稿日期

  • 01月17日 2025

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
承办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
Department of Earth Sciences, National Natural Science Foundation of China
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