The Brewer‐Dobson Circulation During the Last Glacial Maximum
| Main Authors: | Qiang, Fu, White, Rachel H., Wang, Mingcheng, Alexander, Becky, Solomon, Susan, Gettelman, Andrew, Battisti, David S., Lin, Pu |
|---|---|
| Format: | Article eJournal |
| Terbitan: |
, 2020
|
| Online Access: |
https://zenodo.org/record/4091805 |
| ctrlnum |
4091805 |
|---|---|
| fullrecord |
<?xml version="1.0"?>
<dc schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><creator>Qiang, Fu</creator><creator>White, Rachel H.</creator><creator>Wang, Mingcheng</creator><creator>Alexander, Becky</creator><creator>Solomon, Susan</creator><creator>Gettelman, Andrew</creator><creator>Battisti, David S.</creator><creator>Lin, Pu</creator><date>2020-09-03</date><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.
</description><identifier>https://zenodo.org/record/4091805</identifier><identifier>10.1029/2019GL086271</identifier><identifier>oai:zenodo.org:4091805</identifier><relation>info:eu-repo/grantAgreement/EC/H2020/797961/</relation><rights>info:eu-repo/semantics/openAccess</rights><rights>https://creativecommons.org/licenses/by/4.0/legalcode</rights><title>The Brewer‐Dobson Circulation During the Last Glacial Maximum</title><type>Journal:Article</type><type>Journal:Article</type><recordID>4091805</recordID></dc>
|
| format |
Journal:Article Journal Journal:eJournal |
| author |
Qiang, Fu White, Rachel H. Wang, Mingcheng Alexander, Becky Solomon, Susan Gettelman, Andrew Battisti, David S. Lin, Pu |
| title |
The Brewer‐Dobson Circulation During the Last Glacial Maximum |
| publishDate |
2020 |
| url |
https://zenodo.org/record/4091805 |
| contents |
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.
|
| id |
IOS17403.4091805 |
| institution |
Universitas PGRI Palembang |
| institution_id |
189 |
| institution_type |
library:university library |
| library |
Perpustakaan Universitas PGRI Palembang |
| library_id |
587 |
| collection |
Marga Life in South Sumatra in the Past: Puyang Concept Sacrificed and Demythosized |
| repository_id |
17403 |
| city |
KOTA PALEMBANG |
| province |
SUMATERA SELATAN |
| repoId |
IOS17403 |
| first_indexed |
2022-07-26T01:23:03Z |
| last_indexed |
2022-07-26T01:23:03Z |
| recordtype |
dc |
| merged_child_boolean |
1 |
| _version_ |
1739400902035374080 |
| score |
17.608942 |