Analysis of a halocline mesoscale Eddy in the Northwind Basin, Arctic Ocean

IF 2.1 4区 地球科学 Q2 MARINE & FRESHWATER BIOLOGY
Ailing Gan , Lina Lin , Long Fan , Na Liu , Lei Yang , Chengxuan Li
{"title":"Analysis of a halocline mesoscale Eddy in the Northwind Basin, Arctic Ocean","authors":"Ailing Gan ,&nbsp;Lina Lin ,&nbsp;Long Fan ,&nbsp;Na Liu ,&nbsp;Lei Yang ,&nbsp;Chengxuan Li","doi":"10.1016/j.seares.2024.102526","DOIUrl":null,"url":null,"abstract":"<div><p>Eddies have been observed at all depths and in all regions of the Arctic Ocean. However, given the complex geographic conditions and dynamic environments of this ocean, the synchronized observations of temperature, salinity, and currents, and the detailed analysis of individual eddies are still lacking in the Northwind Basin. Our study aims to address these research gaps. We observed an eddy from a mooring in the Northwind Basin in late October 2017. It is a large anticyclonic cold eddy within the Arctic halocline, with a maximum azimuthal velocity reaching 52.63 cm/s and a horizontal scale (~56 km) that significantly exceeds the first local baroclinic Rossby radius of deformation, i.e., it is in mesoscale. Its azimuthal velocity and scale are larger compared with those of nearby eddies, suggesting a relatively young state. This eddy possibly originated from the northern Chukchi Sea shelf, converging near Hanna Shoal with the Chukchi Slope Current before being advected northward into the Northwind Basin. Our study outlines detailed steps for extracting and analyzing eddies from mooring data and contributes to improving the understanding of the characteristics of Arctic Ocean eddies, providing a typical case for the investigation of eddies in the Northwind Basin.</p></div>","PeriodicalId":50056,"journal":{"name":"Journal of Sea Research","volume":"201 ","pages":"Article 102526"},"PeriodicalIF":2.1000,"publicationDate":"2024-08-06","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://www.sciencedirect.com/science/article/pii/S1385110124000595/pdf?md5=4f09d18d6b8dfe63d46a686425c23e3b&pid=1-s2.0-S1385110124000595-main.pdf","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Sea Research","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S1385110124000595","RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"MARINE & FRESHWATER BIOLOGY","Score":null,"Total":0}
引用次数: 0

Abstract

Eddies have been observed at all depths and in all regions of the Arctic Ocean. However, given the complex geographic conditions and dynamic environments of this ocean, the synchronized observations of temperature, salinity, and currents, and the detailed analysis of individual eddies are still lacking in the Northwind Basin. Our study aims to address these research gaps. We observed an eddy from a mooring in the Northwind Basin in late October 2017. It is a large anticyclonic cold eddy within the Arctic halocline, with a maximum azimuthal velocity reaching 52.63 cm/s and a horizontal scale (~56 km) that significantly exceeds the first local baroclinic Rossby radius of deformation, i.e., it is in mesoscale. Its azimuthal velocity and scale are larger compared with those of nearby eddies, suggesting a relatively young state. This eddy possibly originated from the northern Chukchi Sea shelf, converging near Hanna Shoal with the Chukchi Slope Current before being advected northward into the Northwind Basin. Our study outlines detailed steps for extracting and analyzing eddies from mooring data and contributes to improving the understanding of the characteristics of Arctic Ocean eddies, providing a typical case for the investigation of eddies in the Northwind Basin.

北冰洋北风海盆卤线中尺度涡分析
在北冰洋的所有深度和所有区域都观测到了漩涡。然而,鉴于该海域复杂的地理条件和动态环境,北风海盆仍缺乏对温度、盐度和海流的同步观测以及对单个漩涡的详细分析。我们的研究旨在填补这些研究空白。2017 年 10 月下旬,我们从北风海盆的系泊设备上观测到了一个漩涡。它是北极卤化线内的一个大型反气旋冷涡,最大方位角速度达到 52.63 cm/s,水平尺度(∼56 km)明显超过当地第一巴氏罗斯比变形半径,即处于中尺度。与附近的漩涡相比,它的方位速度和尺度都较大,表明它处于相对年轻的状态。该漩涡可能起源于楚科奇海大陆架北部,在汉纳浅滩附近与楚科奇斜坡流汇合,然后向北平流进入北风盆地。我们的研究概述了从系泊数据中提取和分析漩涡的详细步骤,有助于加深对北冰洋漩涡特征的了解,为北风海盆漩涡调查提供了一个典型案例。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
Journal of Sea Research
Journal of Sea Research 地学-海洋学
CiteScore
3.20
自引率
5.00%
发文量
86
审稿时长
6-12 weeks
期刊介绍: The Journal of Sea Research is an international and multidisciplinary periodical on marine research, with an emphasis on the functioning of marine ecosystems in coastal and shelf seas, including intertidal, estuarine and brackish environments. As several subdisciplines add to this aim, manuscripts are welcome from the fields of marine biology, marine chemistry, marine sedimentology and physical oceanography, provided they add to the understanding of ecosystem processes.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信