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Volumn 61, Issue 12, 2004, Pages 1454-1460

Why do baroclinic waves tilt poleward with height?

Author keywords

[No Author keywords available]

Indexed keywords

FRICTION; PERTURBATION TECHNIQUES; REGRESSION ANALYSIS; STORMS; WIND EFFECTS;

EID: 3242673504     PISSN: 00224928     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0469(2004)061<1454:WDBWTP>2.0.CO;2     Document Type: Article
Times cited : (10)

References (13)
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  • 2
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  • 3
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    • Chang, E.K.M.1
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    • Chang, E. K. M., 2001: GCM and observational diagnoses of the seasonal and interannual variations of the Pacific storm track during the cool season. J. Atmos. Sci., 58, 1784-1800.
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    • (1970) Geophys. Fluid Dyn. , vol.1 , pp. 91-122
    • Derome, J.1    Dolph, C.L.2
  • 6
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    • Long waves and cyclone waves
    • Eady, E. T., 1949: Long waves and cyclone waves. Tellus, 1, 35-52.
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    • Eady, E.T.1
  • 7
    • 0016473695 scopus 로고
    • The geostrophic momentum approximation and the semigeostrophic equations
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    • Hoskins, B.J.1
  • 8
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    • Reexamination of the structure of the ageostrophic wind in baroclinic waves
    • Kwon, H. J., and G.-H. Lim, 1999: Reexamination of the structure of the ageostrophic wind in baroclinic waves. J. Atmos. Sci., 56, 2512-2521.
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  • 9
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  • 10
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    • The structure of the ageostrophic wind field in baroclinic waves
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* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.