Letter | Published:

Seasonal Behaviour of Atmospheric Pressure Oscillations

Naturevolume 214pages4344 (1967) | Download Citation

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Abstract

IT is well known that the atmospheric pressure at any given point does not remain constant in time and is subject to periodic and non-periodic fluctuations. Statistical analyses have been used to establish them and many investigations have been published. This communication reports the results of a spectral density analysis performed for the barometric pressure data at the Langmuir Laboratory (33° 59′ N., 107° 11′ W., elevation 3,320 m above mean sea level), a research facility of the New Mexico Institute of Mining and Technology, and at the Institute campus at Socorro (34° 4′ N., 106° 54′ W., elevation 1,410 m above mean sea level). The Langmuir Laboratory is on a summit ridge of the Magdalena Mountains and the campus is 27 km east in the Riogrande Valley. A comparison of the results of these two stations provides an interesting example of atmospheric behaviour in a “mountain–valley” situation.

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References

  1. 1

    Blackmann, R. B., and Tukey, J. W., The Measurement of Power spectra (Dover publications, New York, 1958).

  2. 2

    Haurwitz, B., Bull. Amer. Met. Soc., 28, 319 (1947).

  3. 3

    Pyle, R. L., J. Meteorol., 16, 467 (1959).

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Author information

Author notes

    • BHARTENDU

    Present address: Meteorological Branch, Department of Transport, Toronto, Ontario

    • J. A. ALLEN

    Present address: University of Wyoming, Laramie, Wyoming

    • G. W. PALTRIDGE

    Present address: Radio and Space Research Station, Ditton Park, Slough

Affiliations

  1. New Mexico Institute of Mining and Technology, Socorro, New Mexico

    • BHARTENDU
    • , J. A. ALLEN
    • , G. W. PALTRIDGE
    •  & M. H. WILKENING

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https://doi.org/10.1038/214043a0

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