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南极每个冰间湖每日边界的数据集。

A dataset of the daily edge of each polynya in the Antarctic.

作者信息

Lin Yichen, Nakayama Yoshihiro, Liang Kaixin, Huang Yongtao, Chen Dake, Yang Qinghua

机构信息

School of Atmospheric Sciences, Sun Yat-sen University, and Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), 519082, Zhuhai, China.

Institute of Low Temperature Science, Hokkaido University, N19W8, Sapporo, Japan.

出版信息

Sci Data. 2024 Sep 17;11(1):1006. doi: 10.1038/s41597-024-03848-2.

DOI:10.1038/s41597-024-03848-2
PMID:39289369
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11408600/
Abstract

Polynyas play a critical role in the formation of Antarctic Bottom Water and the enhancement of polar primary productivity. Accurate and exhaustive identification of Antarctic polynyas is fundamental to advancing in-depth research. However, due to methodological limitations, previous studies paid more attention to frequent polynyas and infrequent polynyas have not been investigated much despite that they could be vulnerable to climate change. Inspired by a cyclone tracking algorithm, we develop a novel method to overcome challenges identifying all types of polynyas satisfying spatiotemporal criteria and tracing their daily evolution, extracting from an extensive amount of sea ice concentration data. Based on it, we establish a dataset called "Daily Edge of Each Polynya in Antarctica" (DEEP-AA). Validation against remote sensing and ship-based observations confirms DEEP-AA's reliability. Compared to existing maps, the DEEP-AA identifies a threefold number of polynyas and reveals the seasonal area recovery of infrequent polynyas is earlier than frequent ones.

摘要

冰间湖在南极底层水的形成以及极地初级生产力的增强过程中发挥着关键作用。准确且详尽地识别南极冰间湖是推进深入研究的基础。然而,由于方法上的局限性,以往的研究更多地关注频繁出现的冰间湖,而对不频繁出现的冰间湖研究较少,尽管它们可能更容易受到气候变化的影响。受气旋跟踪算法的启发,我们开发了一种新方法,以克服在识别满足时空标准的各类冰间湖并追踪其每日演变方面所面临的挑战,该方法从大量海冰浓度数据中提取信息。在此基础上,我们建立了一个名为“南极每个冰间湖的每日边界”(DEEP - AA)的数据集。与遥感和船基观测结果的验证证实了DEEP - AA的可靠性。与现有地图相比,DEEP - AA识别出的冰间湖数量增加了两倍,并揭示出不频繁出现的冰间湖的季节性面积恢复比频繁出现的冰间湖更早。

相似文献

1
A dataset of the daily edge of each polynya in the Antarctic.南极每个冰间湖每日边界的数据集。
Sci Data. 2024 Sep 17;11(1):1006. doi: 10.1038/s41597-024-03848-2.
2
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Dominant frazil ice production in the Cape Darnley polynya leading to Antarctic Bottom Water formation.在达恩利角冰间湖形成优势针状冰,导致南极底层水的形成。
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Seasonal Dynamics of Dissolved Iron on the Antarctic Continental Shelf: Late-Fall Observations From the Terra Nova Bay and Ross Ice Shelf Polynyas.南极大陆架溶解铁的季节动态:特拉诺瓦湾和罗斯冰架冰间湖的秋末观测
J Geophys Res Oceans. 2022 Oct;127(10):e2022JC018999. doi: 10.1029/2022JC018999. Epub 2022 Oct 17.

本文引用的文献

1
Modeling the Seasonal Cycle of Iron and Carbon Fluxes in the Amundsen Sea Polynya, Antarctica.模拟南极阿蒙森海冰间湖中铁和碳通量的季节性循环
J Geophys Res Oceans. 2019 Mar;124(3):1544-1565. doi: 10.1029/2018JC014773. Epub 2019 Mar 7.
2
Observed interannual changes beneath Filchner-Ronne Ice Shelf linked to large-scale atmospheric circulation.菲尔希纳-龙尼冰架下观测到的年际变化与大规模大气环流有关。
Nat Commun. 2021 May 20;12(1):2961. doi: 10.1038/s41467-021-23131-x.
3
Antarctic offshore polynyas linked to Southern Hemisphere climate anomalies.
南极外海冰间湖与南半球气候异常有关。
Nature. 2019 Jun;570(7761):319-325. doi: 10.1038/s41586-019-1294-0. Epub 2019 Jun 10.
4
Open-ocean polynyas and deep convection in the Southern Ocean.南大洋开阔海域的冰间湖与深层对流。
Sci Rep. 2019 May 6;9(1):6935. doi: 10.1038/s41598-019-43466-2.
5
The suppression of Antarctic bottom water formation by melting ice shelves in Prydz Bay.普里兹湾冰架融化抑制南极底层水形成。
Nat Commun. 2016 Aug 23;7:12577. doi: 10.1038/ncomms12577.
6
Responding to climate change: Adélie Penguins confront astronomical and ocean boundaries.应对气候变化:阿德利企鹅面临天文和海洋界限。
Ecology. 2010 Jul;91(7):2056-69. doi: 10.1890/09-0688.1.