Filling the gap: winter thermohaline evolution along and below the Ross Ice Shelf
编号:740 访问权限:仅限参会人 更新:2024-10-13 08:49:36 浏览:37次 口头报告

报告开始:2025年01月15日 15:20(Asia/Shanghai)

报告时间:15min

所在会场:[S7] Session 7-Advances in the Oceanography of the Ross Sea [S7-1] Advances in the Oceanography of the Ross Sea

暂无文件

摘要
The Ross Ice Shelf floats above the southern sector of the Ross Sea; this creates a cavity where critical ocean-ice interactions take place (see1 and references therein). Crucial processes occurring in this area are: the formation of Ice Shelf Water, the coldest ocean water mass; the intrusion of Antarctic Surface Water, the main driver of frontal and basal melting.  The warm surface water can also contribute to calving, which is the predominant cause of ice shelf thinning and then may directly affect global sea level. Due to the difficulty of direct exploration of the Ross Ice Shelf in the winter, processes occurring there have been only hypothesized to date. We present unprecedented thermohaline observations collected along the Ross Ice Shelf front from 2020 to 2023 by unconventionally programmed Argo floats. These measurements provided the first-ever year-round observations of water column changes in crucial areas of the Ross Ice Shelf, such as the polynya. We estimated the production of High Salinity Shelf Water to be 0.1 to 0.4 Sv, the precursor of Ice Shelf Water and Antarctic Bottom Water. From temperature and salinity profiles we calculated the ocean heat content (on average  5x108 Jm-2), the basal melt rate (the average value ranges between 0.6 and 1.6 m yr-1) and the freshwater content relative to a reference salinity of 34.8 (summer values up to 10 cm). This study suggests that innovative observation systems may provide insights into oceanographic processes and ice-ocean interactions throughout the entire year, offering a unique possibility to enhance the capabilities of climate models and predictions of future sea-level rise.
关键词
Ross Ice Self, Argo Float, High Salinity Shelf Water, ice shelf cavity
报告人
Pierpaolo Falco
Associate Professor University of Ancona

稿件作者
Pierpaolo Falco University of Ancona
发表评论
验证码 看不清楚,更换一张
全部评论
重要日期
  • 会议日期

    01月14日

    2025

    01月17日

    2025

  • 09月27日 2024

    初稿截稿日期

  • 12月14日 2024

    注册截止日期

主办单位
State Key Laboratory of Marine Environmental Science, Xiamen University
联系方式
移动端
在手机上打开
小程序
打开微信小程序
客服
扫码或点此咨询