Abstract
The constants of the Chandlerian oscillation in the mean sea level are calculated for nine ports and the results compared with those of the International Latitude Service. The Chandler period is clearly observed and the amplitudes are large enough. The phase differences greatly depend upon the selected localities.
DOI: https://doi.org/10.3402/tellusa.v16i4.8988 | Journal eISSN: 3035-9554
Language: English
Page range: 513 - 516
Published on: Jan 1, 2012
Published by: Stockholm University Press
In partnership with: Paradigm Publishing Services
© 2012 Axel Jessen, published by Stockholm University Press
This work is licensed under the Creative Commons Attribution 4.0 License.