Autonomous underwater gliders monitoring variability at “choke points” in our ocean system: A case study in the Western Mediterranean Sea
Article first published online: 31 OCT 2012
Published in 2012 by the American Geophysical Union
Geophysical Research Letters
Volume 39, Issue 20, 28 October 2012
How to Cite
2012), Autonomous underwater gliders monitoring variability at “choke points” in our ocean system: A case study in the Western Mediterranean Sea, Geophys. Res. Lett., 39, L20604, doi:10.1029/2012GL053717., , , , , and (
- Issue published online: 31 OCT 2012
- Article first published online: 31 OCT 2012
- Manuscript Accepted: 26 SEP 2012
- Manuscript Revised: 25 SEP 2012
- Manuscript Received: 31 AUG 2012
- EU. Grant Numbers: MyOcean, PERSEUS
Auxiliary material for this article contains five figures and two tables. The first table is a list of the glider missions conducted in the Ibiza Channel. The second table contains details from a statistical analysis to compare the ends of glider transects. The first figure shows the glider tracks from all missions. There next three images show data from the four oceanographic buoys. The final additional figure, Figure S3, shows two images of sea surface temperature.
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Additional file information is provided in the readme.txt.
|grl29692-sup-0001-readme.txt||plain text document||4K||readme.txt|
|grl29692-sup-0002-fs01.tif||TIFF image||264K||Figure S1. Glider tracks from all missions, January to June 2011, with way points for the Ibiza Channel monitoring transect marked.|
|grl29692-sup-0003-fs02a.tif||TIFF image||498K||Figure S2a. Data from Air temperature at 2 m, oceanographic buoys; Lion, Begur, Tarragona and Valencia.|
|grl29692-sup-0004-fs02b.tif||TIFF image||608K||Figure S2b. Data from Wind speed, oceanographic buoys; Lion, Begur, Tarragona and Valencia.|
|grl29692-sup-0005-fs02c.tif||TIFF image||324K||Figure S2c. Data from Sea surface temperature, oceanographic buoys; Lion and Tarragona.|
|grl29692-sup-0006-fs03.tif||TIFF image||6593K||Figure S3. SST from GHRSST a) 25/01/2011 and b) 03/02/2011.|
|grl29692-sup-0007-ts01.doc||Word document||43K||Table S1. SST from GHRSST a) 25/01/2011 and b) 03/02/2011.|
|grl29692-sup-0008-ts02.doc||Word document||18K||Table S2. The mean difference in potential temperature and salinity per half transect, mid-point located at 0.7 Deg E, for rapidly repeated sides and temporally distant sides are compared.|
|grl29692-sup-0009-t01.txt||plain text document||1K||Tab-delimited Table 1.|
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