Halpern, D., 1980: Variability of near-surface currents in the Atlantic North Equatorial Countercurrent during GATE. J. Phys. Oceanogr., 10(8), pp.1213-1220.

Hallock, Z., 1980: On wind-excited, equatorially trapped waves in the presence of mean currents. In Düing, Walter, Ed.,1980: Equatorial and A-Scale Oceanography, GATE, V2. 356 pp. Supplement 2 to Deep Sea Research Part A, v. 26, pp. 261-284. https://doi.org/10.1016/B978-1-4832-8366-1.50032-7

Gunther, H., 1980: Convective-mesoscale wave disturbance during GATE investigated by spectral methods. Beitr. Atm. Phys. (Contr. To Atmos. Phys.), 53, 74-89.

Grube, P.G., 1979. Convection induced temperature change in GATE (Doctoral dissertation, Colorado State University. Libraries)

Grose, P.L., 1980. Transition in water mass properties between 200 and 500 meters depth in the GATE B-array. In Siedler, Gerold, and John D. Woods, 1980: Oceanography and Surface Layer Meteorology of the B/C-Scale, GATE, Pergamon press, 294 pp. Supplement 1 to Deep-Sea Research Part A (pp. 147-160). https://doi.org/10.1016/B978-1-4832-8366-1.50013-3

Griffith, K.T., S.K. Cox, and R. G. Knollenberg., 1980: Infrared radiative properties of tropical cirrus clouds inferred from aircraft measurements, J. Atmos. Sci, 37, 1077-1087.

Greenhut, G.K., 1981. Analysis of aircraft measurements of momentum flux in the subcloud layer over the tropical Atlantic Ocean during GATE. Bound.-Layer Meteor., 20(1),.75-100.

Greenhut, G.K., 1978. Correlations between rainfall and sea surface temperature during GATE. J. Phys. Oceanog., 8(6), 1135-1138.

Govind, P. K. (1975). Dropwindsonde instrumentation for weather reconnaissance aircraft. J. Appl. Meteor. Climat., 14(8), 1512-1520. https://doi.org/10.1175/1520-0450(1975)014<1512:DIFWRA>2.0.CO;2

Goerss, J.S., 1979. Drift analysis of GATE ship surface measurement systems. Bull. Amer. Met. Soc., 60(9), 1077-1083.