scholarly journals Horizontal circulation and volume transports in the Weddell Gyre derived from Argo float data

2019 ◽  
Vol 175 ◽  
pp. 263-283 ◽  
Author(s):  
Krissy Anne Reeve ◽  
Olaf Boebel ◽  
Volker Strass ◽  
Torsten Kanzow ◽  
Rüdiger Gerdes
2020 ◽  
Vol 184 ◽  
pp. 102294
Author(s):  
Krissy Anne Reeve ◽  
Olaf Boebel ◽  
Volker Strass ◽  
Torsten Kanzow ◽  
Rüdiger Gerdes

2016 ◽  
Vol 8 (1) ◽  
pp. 15-40 ◽  
Author(s):  
K. A. Reeve ◽  
O. Boebel ◽  
T. Kanzow ◽  
V. Strass ◽  
G. Rohardt ◽  
...  

Abstract. The Weddell Gyre plays a crucial role in the modification of climate by advecting heat poleward to the Antarctic ice shelves and by regulating the density of water masses that feed the lowest limb of the global ocean overturning circulation. However, our understanding of Weddell Gyre water mass properties is limited to regions of data availability, primarily along the Prime Meridian. The aim of this paper is to provide a data set of the upper water column properties of the entire Weddell Gyre. Objective mapping was applied to Argo float data in order to produce spatially gridded, time-composite maps of temperature and salinity for fixed pressure levels ranging from 50 to 2000 dbar, as well as temperature, salinity and pressure at the level of the sub-surface temperature maximum. While the data are currently too limited to incorporate time into the gridded structure, the data are extensive enough to produce maps of the entire region across three time-composite periods (2001–2005, 2006–2009 and 2010–2013), which can be used to determine how representative conclusions drawn from data collected along general RV transect lines are on a gyre scale perspective. The work presented here represents the technical prerequisite for addressing climatological research questions in forthcoming studies. The data sets are available in netCDF format at doi:10.1594/PANGAEA.842876.


2015 ◽  
Vol 2015 ◽  
pp. 1-15 ◽  
Author(s):  
Luiz Paulo de Freitas Assad ◽  
Carina Stefoni Böck ◽  
Rogerio Neder Candella ◽  
Luiz Landau

The knowledge of wind stress variability could represent an important contribution to understand the variability over upper layer ocean volume transports. The South Brazilian Bight (SBB) circulation had been studied by numerous researchers who predominantly attempted to estimate its meridional volume transport. The main objective and contribution of this study is to identify and quantify possible interannual variability in the ocean volume transport in the SBB induced by the sea surface wind stress field. A low resolution ocean global circulation model was implemented to investigate the volume transport variability. The results obtained indicate the occurrence of interannual variability in meridional ocean volume transports along three different zonal sections. These results also indicate the influence of a wind driven large-scale atmospheric process that alters locally the SBB and near-offshore region wind stress field and consequently causes interannual variability in the upper layer ocean volume transports. A strengthening of the southward flow in 25°S and 30°S was observed. The deep layer ocean volume transport in the three monitored sections indicates a potential dominance of other remote ocean processes. A small time lag between the integrated meridional volume transports changes in each monitored zonal section was observed.


2018 ◽  
Vol 123 (12) ◽  
pp. 8714-8729 ◽  
Author(s):  
Agatha M. Boer ◽  
Estanislao Gavilan Pascual‐Ahuir ◽  
David P. Stevens ◽  
Léon Chafik ◽  
David K. Hutchinson ◽  
...  
Keyword(s):  

2019 ◽  
Vol 83 (sp1) ◽  
pp. 116
Author(s):  
Hanling Wu ◽  
Yanjun Liu ◽  
Gang Xue ◽  
Fengxiang Guo ◽  
Zhitong Li ◽  
...  

2018 ◽  
Vol 45 (21) ◽  
pp. 11,866-11,874
Author(s):  
Qian Li ◽  
Sukyoung Lee ◽  
Matthew Mazloff
Keyword(s):  

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