Rind et al. 1984

Rind, D., R. Suozzo, A. Lacis, G. Russell, and J. Hansen, 1984: 21 Layer Troposphere-Stratosphere Climate Model. NASA TM-86183. National Aeronautics and Space Administration.

Our global climate model (Model II) is extended through the stratosphere by increasing the vertical resolution and raising the model top to the 0.01 mb (75 km) level. The inclusion of a realistic stratosphere is necessary for investigation of the climate effects of stratospheric perturbations, such as changes of ozone, aerosols or solar ultraviolet irradiance, as well as for studying the effect on the stratosphere of tropospheric climate changes.

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Rind, D., Suozzo, R., Lacis, A., Russell, G., and Hansen, J.: 21 Layer Troposphere-Stratosphere Climate Model, NASA TM-86183, National Aeronautics and Space Administration, Washington, D.C., 1984.

Rind, D., R. Suozzo, A. Lacis, G. Russell, and J. Hansen (1984), 21 Layer Troposphere-Stratosphere Climate Model, NASA TM-86183, National Aeronautics and Space Administration, Washington, D.C.

Rind, D., R. Suozzo, A. Lacis, G. Russell, and J. Hansen, 1984: 21 Layer Troposphere-Stratosphere Climate Model. NASA TM-86183. National Aeronautics and Space Administration.

Rind, D., Suozzo, R., Lacis, A., Russell, G., & Hansen, J. 1984, 21 Layer Troposphere-Stratosphere Climate Model, NASA TM-86183 ( (Washington, D.C.: National Aeronautics and Space Administration).

Rind D, Suozzo R, Lacis A, Russell G, Hansen J. 21 Layer Troposphere-Stratosphere Climate Model. NASA TM-86183. Washington, D.C.: National Aeronautics and Space Administration; 1984.

D. Rind, R. Suozzo, A. Lacis, G. Russell, J. Hansen, 21 Layer Troposphere-Stratosphere Climate Model (NASA TM-86183, National Aeronautics and Space Administration, Washington, D.C., 1984).