Global Contraction of Antarctic Bottom Water between the 1980s and 2000s

Citation:
Purkey, SG, Johnson GC.  2012.  Global Contraction of Antarctic Bottom Water between the 1980s and 2000s. Journal of Climate. 25:5830-5844.

Date Published:

Sep 1

Keywords:

boundary current, circumpolar current, climate-change, deep-ocean, meridional overturning circulation, north-atlantic, pacific-ocean, Southern Annular mode, temperature trends, weddell sea

Abstract:

A statistically significant reduction in Antarctic Bottom Water (AABW) volume is quantified between the 1980s and 2000s within the Southern Ocean and along the bottom-most, southern branches of the meridional overturning circulation (MOC). AABW has warmed globally during that time, contributing roughly 10% of the recent total ocean heat uptake. This warming implies a global-scale contraction of AABW. Rates of change in AABW-related circulation are estimated in most of the world's deep-ocean basins by finding average rates of volume loss or gain below cold, deep potential temperature (theta) surfaces using all available repeated hydrographic sections. The Southern Ocean is losing water below theta = 0 degrees C at a rate of -8.2 (+/- 2.6) 3 10(6) m(3) s (1). This bottom water contraction causes a descent of potential isotherms throughout much of the water column until a near-surface recovery, apparently through a southward surge of Circumpolar Deep Water from the north. To the north, smaller losses of bottom waters are seen along three of the four main northward outflow routes of AABW. Volume and heat budgets below deep, cold theta surfaces within the Brazil and Pacific basins are not in steady state. The observed changes in volume and heat of the coldest waters within these basins could be accounted for by small decreases to the volume transport or small increases to theta of their inflows, or fractional increases in deep mixing. The budget calculations and global contraction pattern are consistent with a global-scale slowdown of the bottom, southern limb of the MOC.

Notes:

n/a

Website

DOI:

10.1175/JCLI-D-11-00612.1