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Outflow from under the Pine Island Bay Ice Shelf: finescale structure and its temporal variability

Robin Robertson

极地科学进展(英文版)2016,Vol.27Issue(4):245-263,19.
极地科学进展(英文版)2016,Vol.27Issue(4):245-263,19.DOI:10.13679/j.advps.2016.4.00245

Outflow from under the Pine Island Bay Ice Shelf: finescale structure and its temporal variability

Outflow from under the Pine Island Bay Ice Shelf: finescale structure and its temporal variability

Robin Robertson1

作者信息

  • 1. School of Physical, Environmental, and Mathematical Sciences, University of New South Wales, Canberra ACT 2610, Australia;Department of Marine Science, Nanjing University of Information Science and Technology, Nanjing 210044, China
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摘要

关键词

Pine Island Bay/double-diffusion/Amundsen Sea/internal tides

Key words

Pine Island Bay/double-diffusion/Amundsen Sea/internal tides

引用本文复制引用

Robin Robertson..Outflow from under the Pine Island Bay Ice Shelf: finescale structure and its temporal variability[J].极地科学进展(英文版),2016,27(4):245-263,19.

基金项目

Acknowledgements I would like to thank the crew and support personnel on the RVIB Nathaniel B. Palmer during NPB0901, Stan Jacobs for providing me the opportunity of participating in the research voyage, and the people who collected the CTD data: Katherine Leonard, Christopher Little, and Kenneth Mankoff. Thanks are also due to Pierre Dutrieux for providing the shipboard ADCP data and first noting the gyre in PIB. Additionally, I would like to thank the anonymous reviewers who made valuable suggestions resulting in significant changes to this paper. This project was funded partially by both the Australian Antarctic Division, project 2944. ()

极地科学进展(英文版)

OACSTPCD

1674-9928

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