{"refrec":{"BRefID":330779,"RR":"<b>Pacini, A.; Pickart, R.S.; Bahr, F.; Torres, D.J.; Ramsey, A.L.; Holte, J.; Karstensen, J.; Oltmanns, M.; Straneo, F.; Le Bras, I.A.; Moore, G.W.K.; de Jong, M.F.</b> (2020). Mean conditions and seasonality of the West Greenland boundary current system near Cape Farewell. <i>J. Phys. Oceanogr. 50(10)</i>: 2849-2871. <a href=\"https://doi.org/10.1175/jpo-d-20-0086.1\" target=\"_blank\">https://doi.org/10.1175/jpo-d-20-0086.1</a>","BEntID":324389,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>J. Phys. Oceanogr. 50(10)</i>: 2849-2871. <a href=\"https://doi.org/10.1175/jpo-d-20-0086.1\" target=\"_blank\">https://doi.org/10.1175/jpo-d-20-0086.1</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Pacini, A.; Pickart, R.S.; Bahr, F.; Torres, D.J.; Ramsey, A.L.; Holte, J.; Karstensen, J.; Oltmanns, M.; Straneo, F.; Le Bras, I.A.; Moore, G.W.K.; de Jong, M.F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Pacini, A. <i>et al.</i>","Englishabstract":"  The structure, transport, and seasonal variability of the West Greenland    boundary current system near Cape Farewell are investigated using a    high-resolution mooring array deployed from 2014 to 2018. The boundary    current system is comprised of three components: the West Greenland Coastal    Current, which advects cold and fresh Upper Polar Water (UPW); the West    Greenland Current, which transports warm and salty Irminger Water (IW)    along the upper slope and UPW at the surface; and the Deep Western Boundary    Current, which advects dense overflow waters. Labrador Sea Water (LSW) is    prevalent at the seaward side of the array within an offshore recirculation    gyre and at the base of the West Greenland Current. The 4-yr mean transport    of the full boundary current system is 31.1 ± 7.4 Sv (1 Sv ≡ 10<sup>6</sup>    m<sup>3</sup> s<sup>−1</sup>), with no clear seasonal signal. However, the    individual water mass components exhibit seasonal cycles in hydrographic    properties and transport. LSW penetrates the boundary current locally,    through entrainment/mixing from the adjacent recirculation gyre, and also    enters the current upstream in the Irminger Sea. IW is modified through    air–sea interaction during winter along the length of its trajectory around    the Irminger Sea, which converts some of the water to LSW. This, together    with the seasonal increase in LSW entering the current, results in an    anticorrelation in transport between these two water masses. The    seasonality in UPW transport can be explained by remote wind forcing and    subsequent adjustment via coastal trapped waves. Our results provide the    first quantitatively robust observational description of the boundary    current in the eastern Labrador Sea.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Mean conditions and seasonality of the West Greenland boundary current system near Cape Farewell","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-06-06 01:34:21.396067","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":null,"OtherDescriptors":null,"Notes":null,"AnaPub":2020,"MonPub":null,"DateUpdate":"2021-01-11","DateCreate":"2020-11-10","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000589826300004","VABBcode":null,"OpenAcc":0,"DOI":"10.1175/jpo-d-20-0086.1"},"refs":null,"anarec":{"AnaID":330779,"PubliDate":2020,"Pagination":"2849-2871","XtraPublOfAnaID":null,"ISBN":null,"Volume":"50","Issue":"10","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":43252,"SerRR":"Journal of Physical Oceanography. 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