Rind and Donn 1975

Rind, D., and W.L. Donn, 1975: Further use of natural infrasound as a continuous monitor of the upper atmosphere. J. Atmos. Sci., 32, 1694-1704, doi:10.1175/1520-0469(1975)032<1694:FUONIA>2.0.CO;2.

This is a further study of the use of natural infrasound in the atmosphere to monitor tidal circulation in the lower thermosphere. The height of this circulation is determined with the use of a reference atmospheric model, which is then used to calibrate infrasound/microseism ratios in terms of height. Also, we show from continuous observation over six years at 41°N, 74°W that the winter semidiurnal tide is present at least 62% of the time and the diurnal, at least 42% of the time.

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Rind, D., and Donn, W.L.: Further use of natural infrasound as a continuous monitor of the upper atmosphere, J. Atmos. Sci., 32, 1694-1704, doi:10.1175/1520-0469(1975)032<1694:FUONIA>2.0.CO;2, 1975.

Rind, D., and W.L. Donn (1975), Further use of natural infrasound as a continuous monitor of the upper atmosphere, J. Atmos. Sci., 32, 1694-1704, doi:10.1175/1520-0469(1975)032<1694:FUONIA>2.0.CO;2.

Rind, D., and W.L. Donn, 1975: Further use of natural infrasound as a continuous monitor of the upper atmosphere. J. Atmos. Sci., 32, 1694-1704, doi:10.1175/1520-0469(1975)032<1694:FUONIA>2.0.CO;2.

Rind, D., & Donn, W.L. 1975, J. Atmos. Sci., 32, 1694, doi:10.1175/1520-0469(1975)032<1694:FUONIA>2.0.CO;2.

Rind D, Donn WL. Further use of natural infrasound as a continuous monitor of the upper atmosphere, J Atmos Sci 1975;32:1694-1704. doi:10.1175/1520-0469(1975)032<1694:FUONIA>2.0.CO;2.

D. Rind, W.L. Donn, J. Atmos. Sci. 32, 1694-1704, doi:10.1175/1520-0469(1975)032<1694:FUONIA>2.0.CO;2 (1975).