Publications and Papers

Kopp, F. J., 1985: Deduction of Vertical Motion in the Atmosphere from Aircraft Measurements. J. Atmos. Oceanic Technol., 2, 68

http://dx.doi.org/10.1175/1520-0426(1985)002<0684:DOVMIT>2.0.CO;2

Kubesh, R. S., D. J. Musil, R. D. Farley, and H. D. Orville, 1988: The 1 August 1981 MOPE Storm: Observations and Modeling Resu

http://dx.doi.org/10.1175/1520-0450(1988)027<0216:TAMSOA>2.0.CO;2

Kusunoki, K., and H. Eito, 2003: Analytical Studies of Low-Level Internal Gravity Waves over the Kanto Plain Associated with a

http://dx.doi.org/10.1175/1520-0493(2003)131<0236:ASOLLI>2.0.CO;2

Lambrigtsen, B. H., and R. K. Kakar, 1985: Estimation of Atmospheric Moisture Content from Microwave Radiometric Measurements d

http://dx.doi.org/10.1175/1520-0450(1985)024<0266:EOAMCF>2.0.CO;2

LeMone, M. A., G. M. Barnes, J. C. Fankhauser, and L. F. Tarleton, 1988: Perturbation Pressure Fields Measured by Aircraft arou

http://dx.doi.org/10.1175/1520-0493(1988)116<0313:PPFMBA>2.0.CO;2

Agee, E. M., D. E. Brown, T. S. Chen, K. E. Dowell, 1973: A Height-Dependent Model of Eddy Viscosity in the Planetary Boundary

http://journals.ametsoc.org/doi/abs/10.1175/1520-0450%281973%29012%3C0409%3AAHDMOE%3E2.0.CO%3B2

Anonymous, 1969: Oceanographic-meteorological research in Barbados, Eos Trans. AGU, 50(8), 495, doi:10.1029/EO050i008p00495-05.

http://www.agu.org/pubs/crossref/1969/EO050i008p00495-05.shtml

Bean, B. R., R. Gilmer, R. L. Grossman, R. McGavin, and C. Travis, 1972: An Analysis of Airborne Measurements of Vertical Water

http://journals.ametsoc.org/doi/abs/10.1175/1520-0469%281972%29029%3C0860%3AAAOAMO%3E2.0.CO%3B2

Berg, L. K., and R. B. Stull, 2005: A Simple Parameterization Coupling the Convective Daytime Boundary Layer and Fair-Weather C

http://journals.ametsoc.org/doi/abs/10.1175/JAS3437.1

Betts, A. K., 1975: Parametric Interpretation of Trade-Wind Cumulus Budget Studies. J. Atmos. Sci., 32, 1934-1945, doi:10.1175/

http://journals.ametsoc.org/doi/abs/10.1175/1520-0469%281975%29032%3C1934%3APIOTWC%3E2.0.CO%3B2