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Volumn 31, Issue 4, 2001, Pages 962-971

What is the "Near-inertial" band and why is it different from the rest of the internal wave spectrum?

Author keywords

[No Author keywords available]

Indexed keywords

MIXING; WATER WAVES; WAVE PROPAGATION;

EID: 0035303089     PISSN: 00223670     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0485(2001)031<0962:WITNIB>2.0.CO;2     Document Type: Article
Times cited : (191)

References (38)
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    • D'Asaro, E.A.1
  • 5
    • 0029480597 scopus 로고
    • Upper-ocean inertial currents forced by a strong storm. Part III: Interaction of inertial currents and mesoscale eddies
    • (1995) J. Phys. Oceanogr , vol.25 , pp. 2953-2958
    • D'Asaro, E.A.1
  • 16
    • 0016458920 scopus 로고
    • The propagation of wind-generated inertial oscillations from the surface into the deep ocean
    • (1975) J. Mar. Res , vol.33 , pp. 15-51
    • Kroll, J.1
  • 31
    • 0000292572 scopus 로고
    • Doppler sonar observations of internal waves: The wavenumber frequency spectrum
    • (1984) J. Phys. Oceanogr , vol.14 , pp. 1249-1270
    • Pinkel, R.1
  • 36
    • 0343986274 scopus 로고    scopus 로고
    • Internal wave-wave interactions. Part II: Spectral energy transfer and turbulence production
    • (1999) J. Phys. Oceanogr , vol.29 , pp. 2905-2919
    • Sun, H.1    Kunze, E.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.