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Journal article

The eddy-driven jet and storm-track responses to boundary-layer drag: insights from an idealized dry GCM study

Abstract:
Simulations using a dry, idealized general circulation model (GCM) are conducted to systematically investigate the eddy-driven jet’s sensitivity to the location of boundary-layer drag. Perturbations of boundary-layer drag solely within the baroclinic zone reproduce the eddy-driven jet responses to global drag variations. The implications for current theories of eddy-driven jet shifts are discussed. Hemispherically-asymmetric drag simulations in equinoctial and solstitial thermal conditions show that perturbations of surface drag in one hemisphere have negligible effects on the strength and latitude of the eddy-driven jet in the opposite hemisphere. Jet speed exhibits larger sensitivities to surface drag in perpetual winter simulations, while sensitivities in jet latitude are larger in perpetual summer simulations. Near-surface drag simulations with an Earth-like continental profile show how surface drag may facilitate tropical-extratropical teleconnections by modifying waveguides through changes in jet latitude. Longitudinally confined drag simulations demonstrate a novel mechanism for localizing storm tracks. A theoretical analysis is used to show that asymmetries in the Bernoulli function within the baroclinic zone are important for the eddy-driven jet latitude responses because they directly modulate the sensitivity of the zonal-mean zonal wind to drag in the boundarylayer momentum balance. The simulations contained herein provide a rich array of case studies against which to test current theories of eddy-driven jet and storm-track shifts; and the results affirm the importance of correct, well-constrained locations and intensities of boundary-layer drag in order to reduce jet and storm-track biases in climate and forecast models.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1175/JAS-D-18-0086.1

Authors


More by this author
Institution:
University of Oxford
Division:
MPLS
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Oxford college:
Wolfson College
Role:
Author
ORCID:
0000-0001-6378-7419
More by this author
Institution:
University of Oxford
Division:
MPLS Division
Department:
Physics
Sub department:
Atmos Ocean & Planet Physics
Role:
Author


Publisher:
American Meteorological Society
Journal:
Journal of the Atmospheric Sciences More from this journal
Volume:
76
Issue:
4
Pages:
1055–1076
Publication date:
2019-02-06
Acceptance date:
2019-02-01
DOI:
EISSN:
1520-0469
ISSN:
0022-4928


Keywords:
Pubs id:
pubs:968755
UUID:
uuid:2f37569e-75f3-4885-b997-4feb7d752b99
Local pid:
pubs:968755
Source identifiers:
968755
Deposit date:
2019-02-04

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