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—Ñ �ˉî 1991 ”N 6 ŒŽ 21 “ú

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• 007 �}1 ‰¡ŽR’·”V 1980:‘å‹C‹«ŠE‘w‚Ì�\‘¢‚ÉŠÖ‚·‚錤‹†-Šw‰ï�ÜŽó�Ü‹L”O�u‰‰-, “V‹C, 27, 5-12 (fig.4 and 5)
• 008 �}2 Stull R.Bl 1988:An introduction to boundary meteorology, Kluwer Academic Publishers, 666pp(fig.5.5)(Œ´“T:Louis et al 1983)
• 009 �}2.1 Gerber H. et al 1989:Evolution of a marine boundary-layer jet, J. Atom. Sci., 46, 1312-1326(fig.11)
• 010 �}3 Klemp J.B. and Wihelmson R.B. 1978:The simulation of three-dimensional convective storm dynamics, J. Atmos. Sci., 35, 1070-1096(fig.7) Smagorinsky J. 1963:General curculation experiments with the primitive equations: 1, The basic experiment, Mon. Wea. Rev., 91, 99-164
• 011 �}4 Frisch A.S.and Strauch R.G. 1976:Doppler radar measurements of turbulent kinetic energy dissipation rates in a northeastern Colorado convective storm, J. Appl. Meteor., 15, 1012-1017(fig.3)
• 012 �}5 �²“¡ŒO1991:personal comunication
• 013 �}8 Karacostas T.S. and Marwit‚šJ.D.1980:Turbulent kinetic energy budgets over mountainous terrain, J. Appl. Meteorol., 19, 163-174(fig.4)
• 014 �}9 ŽR’†‘åŠw 1991:personal comunication
• 015 �}9.1 Oort A.H.and Peixoto J.P.1983:Gloabal angular momentum and energy balance requirements from ovservations, in Theory of climate, Advances in Geophysics 25, Academic Press(fig.53)
• 016 �}10 Shay T.J. and Gregg M.C.1984:Turbulence in an oceanic convective mixed layer, Nature, 310, 282-285(fig.3)
• 017 �}11 Dillon et al 1981(fig.2)
• 018 �}12 Moum J.N.et al 1989:Mixing in the equatorial surface layer and thermocline, J. Geophys, Res, 94, 2005-21(fig.3.4)
• 019 �}13 “¯�ã(fig.5)
• 020 �}14 “¯�ã(fig.6)
• 021 �}14.1 Lewis M.R. et al 1986:Vertical nitrate fluxes in the oligotrophic ocean, Science, 234, 870-873(fig.1)
• 022 �}15 Dewey R.K. and Crawford W.R.1988:Bottom stress estimates from vertical dissipation rate profiles on the continental shelf, J. Phys. Oceanogr., 18, 1167-77(fig.4)