The Brewer-Dobson circulation during the last glacial maximum

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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Author Fu, Q.
White, R. H.
Wang, M.
Alexander, B.
Solomon, S.
Gettelman, Andrew
Battisti, D. S.
Lin, P.
Publisher UCAR/NCAR - Library
Publication Date 2020-03-16T00:00:00
Digital Object Identifier (DOI) Not Assigned
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Topic Category geoscientificInformation
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Metadata Date 2025-07-11T19:20:44.596002
Metadata Record Identifier edu.ucar.opensky::articles:23288
Metadata Language eng; USA
Suggested Citation Fu, Q., White, R. H., Wang, M., Alexander, B., Solomon, S., Gettelman, Andrew, Battisti, D. S., Lin, P.. (2020). The Brewer-Dobson circulation during the last glacial maximum. UCAR/NCAR - Library. https://n2t.org/ark:/85065/d7r214k9. Accessed 31 July 2025.

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