Journal of Climate,
Warming of global abyssal and deep Southern Ocean waters between the 1990s and 2000s: Contributions to global heat and sea level rise budgets
Sarah G. Purkey¹,² and Gregory C. Johnson²,¹,*
¹School of Oceanography, University of Washington, Seattle, WA 98195, U.S.A.
²NOAA/Pacific Marine Environmental Laboratory, Seattle, WA 98115, U.S.A.
Abstract
*Correspondence e-mail: gregory.c.johnson@noaa.gov
Link to full paper (pdf file): http://www.pmel.noaa.gov/people/gjohnson/Recent_AABW_Warming_v3.pdf
Written by fatih al-farahat in
Antarctic Circumpolar Current,
ocean heat content,
Sea level rise,
Southern Annular Mode,
Southern Ocean
"Warming of global abyssal and deep Southern Ocean waters between the 1990s and 2000s: Contributions to global heat and sea level rise budgets by Sarah G. Purkey &
We quantify abyssal global and deep Southern Ocean temperature trends between
the 1990s and 2000s to assess the role of recent warming of these regions in global heat
and sea level budgets. We compute warming rates with uncertainties along 28 full-depth,
high-quality, hydrographic sections that have been occupied two or more times between
1980 and 2010. We divide the global ocean into 32 basins defined by the topography and
climatological ocean bottom temperatures and estimate temperature trends in the 24
sampled basins. The three southernmost basins show a strong statistically significant
abyssal warming trend, with that warming signal weakening to the north in the central
Pacific, western Atlantic, and eastern Indian Oceans. Eastern Atlantic and western Indian
Ocean basins show statistically insignificant abyssal cooling trends. Excepting the Arctic
Ocean and Nordic seas, the rate of abyssal (below 4000 m) global ocean heat content
change in the 1990s and 2000s is equivalent to a heat flux of 0.027 (±0.009) W m–2
applied over the entire surface of the Earth. Deep (1000–4000 m) warming south of the
Sub-Antarctic Front of the Antarctic Circumpolar Current adds 0.068 (±0.062) W m–2.
The abyssal warming produces a 0.053 (±0.017) mm yr–1 increase in global average sea
level and the deep warming south of the Sub-Antarctic Front adds another 0.093 (±0.081)
mm yr–1. Thus warming in these regions, ventilated primarily by Antarctic Bottom
Water, accounts for a statistically significant fraction of the present global energy and sea
level budgets.
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