The barometric tides at Zürich and on the summit of Säntis

Details The barometric tides at Zürich and on the summit of Säntis The barometric tides at Zürich and on the summit of Säntis

Dec 1975

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1975papge.113..355h&link_type=abstract

Pure and Applied Geophysics PAGEOPH, Volume 113, Issue 1, pp.355-364

Physics

Geophysics

1

Scientific paper

Lunar barometric tidal determinations ( L 2) have been made by the Chapman-Miller method for Zürich (493 m) and Säntis (2000 m) based on 49 years' data. The seasonal variations of L 2 are much larger at Zürich than on the Säntis summit. However, a comparison with the five other pairs of stations for which tidal determinations at different altitudes, but short horizontal distances, are available do not indicate that this result is as an altitude effect, nor do they show any other systematic differences between L 2 at the lower and the higher station. The solar tidal determinations agree well with those made by Eggenberger (1944) and fit in with those obtained for other stations. From the difference between the pressure oscillations at Zürich and on Säntis the corresponding meantemperature oscillations of the air column between the two stations has been computed.

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