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Volumn 273, Issue 5273, 1996, Pages 335-337

The morphogenesis of bands and zonal winds in the atmospheres on the giant outer planets

Author keywords

[No Author keywords available]

Indexed keywords

ARTICLE; ATMOSPHERE; CHEMICAL COMPOSITION; MORPHOGENESIS; PHYSICAL MODEL; PRIORITY JOURNAL; SPACE; TURBULENT FLOW;

EID: 0030012565     PISSN: 00368075     EISSN: None     Source Type: Journal    
DOI: 10.1126/science.273.5273.335     Document Type: Article
Times cited : (105)

References (21)
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    • (1979) Geophysical Fluid Dynamics
    • Pedlosky, J.1
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    • Marcus, P.S.1
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    • note
    • D; the number is controlled by Lβ ≡ √Ua/Ω.
  • 14
    • 0022167076 scopus 로고
    • The potential vorticity q ≡ (ζ + f)/h is conserved following the motion of each fluid element, thus serving as a tracer for the flow, and is the dynamically significant quantity to view. See, for instance, B. J. Hoskins, M. E. McIntyre, A. W. Robertson, Q. J. R. Meteorol. Soc. 111, 877 (1985).
    • (1985) Q. J. R. Meteorol. Soc. , vol.111 , pp. 877
    • Hoskins, B.J.1    McIntyre, M.E.2    Robertson, A.W.3
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    • B. A. Smith et al., Science 246, 1422 (1989); L. M. Polvani, J. Wisdom, E. DeJong, A. P. Ingersoll, ibid. 249, 1393 (1990); M. Allison and J. T. Lumetta, Geophys. Res. Lett. 17, 2269 (1990).
    • (1989) Science , vol.246 , pp. 1422
    • Smith, B.A.1
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    • B. A. Smith et al., Science 246, 1422 (1989); L. M. Polvani, J. Wisdom, E. DeJong, A. P. Ingersoll, ibid. 249, 1393 (1990); M. Allison and J. T. Lumetta, Geophys. Res. Lett. 17, 2269 (1990).
    • (1990) Science , vol.249 , pp. 1393
    • Polvani, L.M.1    Wisdom, J.2    DeJong, E.3    Ingersoll, A.P.4
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    • B. A. Smith et al., Science 246, 1422 (1989); L. M. Polvani, J. Wisdom, E. DeJong, A. P. Ingersoll, ibid. 249, 1393 (1990); M. Allison and J. T. Lumetta, Geophys. Res. Lett. 17, 2269 (1990).
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    • Allison, M.1    Lumetta, J.T.2
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    • note
    • Anticyclones are eddies with negative vorticity in the northern hemisphere and positive vorticity in the southern hemisphere. Cyclones are the converse.
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    • R. Beebe, Chaos 4, 113 (1994).
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    • note
    • This work is supported by NSF. The computations were performed on the Cray C90 at the Pittsburgh Supercomputing Center. We are grateful to M. Allison for thoughtful suggestions on the manuscript and to A. Simon and R. Beebe for the zonal wind data in Fig. 2.


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.