Intraseasonal response of mixed layer temperature and salinity in the Bay of Bengal to heat and freshwater flux
Version of Record online: 4 MAY 2010
Copyright 2010 by the American Geophysical Union.
Journal of Geophysical Research: Oceans (1978–2012)
Volume 115, Issue C5, May 2010
How to Cite
2010), Intraseasonal response of mixed layer temperature and salinity in the Bay of Bengal to heat and freshwater flux, J. Geophys. Res., 115, C05002, doi:10.1029/2009JC005790., , , and (
- Issue online: 4 MAY 2010
- Version of Record online: 4 MAY 2010
- Manuscript Accepted: 14 DEC 2009
- Manuscript Revised: 24 NOV 2009
- Manuscript Received: 9 SEP 2009
This material illustrates the following three issues: (1) the gridded Argo product does not capture 10–90 day variability with sufficient fidelity to be used in the study of intraseasonal variability of heat and freshwater, (2) an estimate of the error in satellite-derived forcing by comparing with in situ data, and (3) a comparison between intraseasonal SST and time integral of d(Qeff)/dt in different seasons.
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|jgrc11548-sup-0001-readme.txt||plain text document||3K||readme.txt|
|jgrc11548-sup-0002-fs01.eps||PS document||1126K||Figure S1. Five day temperature T (°C) at 5 m depth from float 093 (gray), and from gridded Argo data (black) following the float trajectory.|
|jgrc11548-sup-0003-fs02.eps||PS document||521K||Figure S2. Intraseasonal Qsw (Wm−2) at 1.5°S, 90°E from satellite estimate (gray) and buoy data (black).|
|jgrc11548-sup-0004-fs03.pdf||PDF document||15K||Figure S3. Observed SST anomaly (black; °C) from float 093, and predicted SST anomaly (gray) SSTp = ∫(Qeff/ρCpH0)dt.|
|jgrc11548-sup-0005-t01.txt||plain text document||1K||Tab-delimited Table 1.|
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