Human-induced changes in the global meridional overturning circulation are emerging from the Southern Ocean

Lee, Sang-Ki; Lumpkin, Rick; Gomez, Fabian; Yeager, Stephen; Lopez, Hosmay; Takglis, Filippos; Dong, Shenfu; Aguiar, Wilton; Kim, Dongmin; Baringer, Molly

doi:10.1038/s43247-023-00727-3

Title: Human-induced changes in the global meridional overturning circulation are emerging from the Southern Ocean

Journal Article · Mon Mar 13 00:00:00 EDT 2023 · Communications Earth & Environment

DOI:https://doi.org/10.1038/s43247-023-00727-3· OSTI ID:1961574

^[1];

^[2];

^[3];

^[1]; Takglis, Filippos ^[4];

^[1]; Aguiar, Wilton ^[4];

^[4]; Baringer, Molly ^[1]

NOAA Atlantic Oceanographic and Meteorological Lab., Miami, FL (United States)
NOAA Atlantic Oceanographic and Meteorological Lab., Miami, FL (United States); Mississippi State Univ., Mississippi State, MS (United States)
National Center for Atmospheric Research (NCAR), Boulder, CO (United States)
NOAA Atlantic Oceanographic and Meteorological Lab., Miami, FL (United States); Univ. of Miami, FL (United States)

In a warming climate, the Global Meridional Overturning Circulation (GMOC) is expected to change significantly with a risk of disrupting the global redistribution of ocean properties that sustains marine ecosystems, carbon cycle, and others. Here we make a novel attempt to utilize a diagnostic ocean & sea-ice model to estimate the GMOC and its interdecadal changes since the mid-1950s that are consistent with historical hydrographic observations. We find that significant changes in the GMOC have already occurred, most notably in the upper and lower overturning cells in the Southern Ocean. The former has expanded poleward and into denser water and strengthened by 3–4 Sv since the mid-1970s, while the latter has contracted and weakened by a similar rate during the same period. These changes are driven by the increasing Southern Hemisphere (SH) Ferrel cell and associated increases in the westerlies and the surface buoyancy loss over its sinking branch, and the increasing Antarctic meltwater discharge, in response to ozone depletion in the SH stratosphere and increasing atmospheric CO₂. A large-scale readjustment of the GMOC seems to be underway in the South Atlantic and Indo-Pacific Oceans since the mid-2000s in response to the Southern Ocean changes.

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Research Organization:: University Corporation for Atmospheric Research (UCAR), Boulder, CO (United States)

Sponsoring Organization:: USDOE Office of Science (SC), Biological and Environmental Research (BER)

Grant/Contract Number:: SC0022070

OSTI ID:: 1961574

Journal Information:: Communications Earth & Environment, Vol. 4, Issue 1; ISSN 2662-4435

Publisher:: Springer NatureCopyright Statement

Country of Publication:: United States

Language:: English

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