Published September 3, 2020 | Version v1
Journal article Open

The Brewer‐Dobson Circulation During the Last Glacial Maximum

Authors/Creators

  • 1. University of Washington
  • 2. University of British Columbia
  • 3. Massachusetts Institute of Technology
  • 4. NCAR
  • 5. Princeton University

Description

The Brewer‐Dobson circulation during the Last Glacial Maximum (LGM) is investigated in simulations using the Whole Atmosphere Community Climate Model version 6. We examine vertical mass fluxes, age of stratospheric air, and the transformed Eulerian mean stream function and find that the modeled annual‐mean Brewer‐Dobson circulation during the LGM is almost everywhere slower than that in the modern climate (with or without anthropogenic ozone depleting substances). Compared to the modern climate, the annual‐mean tropical upwelling in the LGM is 11.3–16.9%, 11.2–15.8%, and 4.4–10.2% weaker, respectively, at 100, 70, and 30 hPa. Simulated decreases in annual‐mean mass fluxes at 70 and 100 hPa are caused by a weaker parameterized orographic gravity wave drag and resolved wave drag, respectively.

 

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Fu et al 2020 Brewer Dobson in LGM.pdf

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Additional details

Funding

European Commission
PROTECT - Propagation of atmospheric ROssby waves - connection to prEdictability of Climate exTremes 797961