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Publications and Papers
Johnson, R. H., 1981: Large-Scale Effects of Deep Convection on the GATE Tropical Boundary Layer. J. Atmos. Sci., 38, 2399-2413
http://journals.ametsoc.org/doi/abs/10.1175/1520-0469%281981%29038%3C2399%3ALSEODC%3E2.0.CO%3B2
Jorgensen, D. P., 1984: Mesoscale and Convective-Scale Characteristics of Mature Hurricanes. Part II. Inner Core Structure of H
http://journals.ametsoc.org/doi/abs/10.1175/1520-0469%281984%29041%3C1287%3AMACSCO%3E2.0.CO%3B2
Jorgensen, D. P., and M. A. Lemone, 1989: Vertically Velocity Characteristics of Oceanic Convection. J. Atmos. Sci., 46, 621-64
http://journals.ametsoc.org/doi/abs/10.1175/1520-0469%281989%29046%3C0621%3AVVCOOC%3E2.0.CO%3B2
Jorgensen, D. P., E. J. Zipser, and M. A. Lemone, 1985: Vertical Motions in Intense Hurricanes. J. Atmos. Sci., 42, 839-856, do
http://journals.ametsoc.org/doi/abs/10.1175/1520-0469%281985%29042%3C0839%3AVMIIH%3E2.0.CO%3B2
Kase, R., 1978: High frequency internal waves in the upper thermocline during GATE. Deep Sea Research, 25, 815-825, doi:10.1016
http://www.sciencedirect.com/science/article/pii/0146629178900255
Kedem, B., L. S. Chiu, and G. R. North, 1990: Estimation of mean rain rate: Application to satellite observations. J. Geophys.
https://doi.org/10.1029/JD095iD02p01965
Khain, A., D. Rosenfeld, and A. Pokrovsky, 2005: Aerosol impact on the dynamics and microphysics of deep convective clouds. Qua
http://onlinelibrary.wiley.com/doi/10.1256/qj.04.62/abstract
Khalsa, S. J. S., and J. A. Businger, 1977: The drag coefficient as determined by the dissipation method and its relation to in
https://doi.org/10.1007/BF00121467
Krishnamurti, T. N., H. L. Pan, C. B. Chang, J. Ploshay, D. Walker, and A. W. Oodally, 1979: Numerical weather prediction for G
http://onlinelibrary.wiley.com/doi/10.1002/qj.49710544617/abstract
Leary, C. A., and R. A. Houze Jr., 1979a: Melting and Evaporation of Hydrometeors in Precipitation from the Anvil Clouds of Dee
http://journals.ametsoc.org/doi/abs/10.1175/1520-0469%281979%29036%3C0669%3AMAEOHI%3E2.0.CO%3B2
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