Figure 14 . Cross-slope volume/heat transport. Meridional eddy transports for ASW and CDW (averaged within 1° bin in longitude over the continental slope; 1,000–3,000 m isobaths) are zonally integrated. Standard errors due to the cross-slope variation are shown by shade. Volume transport can precisely be translated to heat flux using the mean temperature of CDW and ASW as indicated by ticks to the left. The 90°E meridian for CDW corresponds to the interbasin boundary between eastern/western Indian sectors, while 130°E is transitional longitude for the ASW transport direction.