Using Ocean Bottom Pressure from the Gravity Recovery and Climate Experiment (GRACE) to Estimate Transport Variability in the Southern Indian Ocean

Previous studies have suggested that ocean bottom pressure (OBP) from the Gravity Recovery and Climate Experiment (GRACE) can be used to measure the depth-averaged, or barotropic, transport variability of the Antarctic Circumpolar Current (ACC). Here, we use GRACE OBP observations to calculate trans...

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Bibliographic Details
Published in:Journal of Geophysical Research: Oceans
Main Authors: Makowski, Jessica K., Chambers, Don P., Bonin, Jennifer A.
Format: Article in Journal/Newspaper
Language:unknown
Published: Digital Commons @ University of South Florida 2015
Subjects:
Antarctic circumpolar current
Southern Ocean
GRACE
ocean bottom pressure
Life Sciences
Antarctic
Indian
The Antarctic
Antarc*
Online Access:https://digitalcommons.usf.edu/msc_facpub/1405
https://doi.org/10.1002/2014JC010575
https://digitalcommons.usf.edu/context/msc_facpub/article/2413/viewcontent/2014JC010575.pdf
Description
Summary:Previous studies have suggested that ocean bottom pressure (OBP) from the Gravity Recovery and Climate Experiment (GRACE) can be used to measure the depth-averaged, or barotropic, transport variability of the Antarctic Circumpolar Current (ACC). Here, we use GRACE OBP observations to calculate transport variability in a region of the southern Indian Ocean encompassing the major fronts of the ACC. We use a statistical analysis of a simulated GRACE-like data set to determine the uncertainty of the estimated transport for the 2003.0–2013.0 time period. We find that when the transport is averaged over 60° of longitude, the uncertainty (one standard error) is close to 1 Sv (1 Sv = 106 m3 s−1) for low-pass filtered transport, which is significantly smaller than the signal and lower than previous studies have found. The interannual variability is correlated with the Southern Annual mode (SAM) (0.61), but more highly correlated with circumpolar zonally averaged winds between 45°S and 65°S (0.88). GRACE transport reflects significant changes in transport between 2007 and 2009 that is observed in the zonal wind variations but not in the SAM index. We also find a statistically significant trend in transport (−1.0 ± 0.4 Sv yr−1, 90% confidence) that is correlated with a local deceleration in zonal winds related to an asymmetry in the SAM on multidecadal periods.

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