Abstract
Some aero-meteorological stations give regular data on the heights of isobaric levels. These data also can be used for the determination of CR temperature effect by integral method, as was shown in Dorman (1960).
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Dorman, L.I. (2004). Development of the Theory and Methods of Determination of Cosmic Ray Variations of Atmospheric Origin. In: Cosmic Rays in the Earth’s Atmosphere and Underground. Astrophysics and Space Science Library, vol 303. Springer, Dordrecht. https://doi.org/10.1007/978-1-4020-2113-8_9
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