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Author Zeng, L.; Chassignet, E.P.; Schmitt, R.W.; Xu, X.; Wang, D. url  doi
openurl 
  Title Salinification in the South China Sea Since Late 2012: A Reversal of the Freshening Since the 1990s Type $loc['typeJournal Article']
  Year 2018 Publication Geophysical Research Letters Abbreviated Journal Geophys. Res. Lett.  
  Volume 45 Issue 6 Pages 2744-2751  
  Keywords South China Sea; salinification; Argo floats; Aquarius; SMAP; PDO  
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  Series Volume Series Issue Edition  
  ISSN 0094-8276 ISBN Medium  
  Area Expedition Conference  
  Funding Approved $loc['no']  
  Call Number COAPS @ mfield @ Serial 853  
Permanent link to this record
 

 
Author Xu, X.; Chassignet, E.P.; Johns, W.E.; Schmitz Jr, W.J.; Metzger, E.J. url  doi
openurl 
  Title Intraseasonal to interannual variability of the Atlantic meridional overturning circulation from eddy-resolving simulations and observations Type $loc['typeJournal Article']
  Year 2014 Publication Journal of Geophysical Research: Oceans Abbreviated Journal J. Geophys. Res. Oceans  
  Volume 119 Issue 8 Pages 5140-5159  
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  Series Editor Series Title Abbreviated Series Title  
  Series Volume Series Issue Edition  
  ISSN 2169-9275 ISBN Medium  
  Area Expedition Conference  
  Funding Approved $loc['no']  
  Call Number COAPS @ mfield @ Serial 152  
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Author Zou, S.; Bower, A.; Furey, H.; Susan Lozier, M.; Xu, X. doi  openurl
  Title Redrawing the Iceland-Scotland Overflow Water pathways in the North Atlantic Type $loc['typeJournal Article']
  Year 2020 Publication Abbreviated Journal Nat Commun  
  Volume 11 Issue 1 Pages 1890  
  Keywords  
  Abstract Iceland-Scotland Overflow Water (ISOW) is a primary deep water mass exported from the Norwegian Sea into the North Atlantic as part of the global Meridional Overturning Circulation. ISOW has historically been depicted as flowing counter-clockwise in a deep boundary current around the subpolar North Atlantic, but this single-boundary-following pathway is being challenged by new Lagrangian observations and model simulations. We show here that ISOW leaves the boundary and spreads into the interior towards the central Labrador and Irminger basins after flowing through the Charlie-Gibbs Fracture Zone. We also describe a newly observed southward pathway of ISOW along the western flank of the Mid-Atlantic Ridge. The partitioning of these pathways is shown to be influenced by deep-reaching eddies and meanders of the North Atlantic Current. Our results, in tandem with previous studies, call for a revision in the historical depiction of ISOW pathways throughout the North Atlantic.  
  Address Center for Ocean-Atmosphere Prediction Studies, Florida State University, Tallahassee, FL, USA  
  Corporate Author Thesis  
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  Language English Summary Language Original Title  
  Series Editor Series Title Abbreviated Series Title  
  Series Volume Series Issue Edition  
  ISSN 2041-1723 ISBN Medium  
  Area Expedition Conference  
  Funding strtoupper('3').strtolower('2313002'); strtoupper('P').strtolower('MC7170894') Approved $loc['no']  
  Call Number COAPS @ user @ Serial 1105  
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