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http://www.scirp.org/journal/PaperInformation.aspx?PaperID=53131#.VLXUEMnQrzE
Author(s)
R. Onguene1,2,3*, E. Pemha4, F. Lyard2, Y. Du-Penhoat2, G. Nkoue5, T. Duhaut3, E. Njeugna1, P. Marsaleix3, R. Mbiake1, S. Jombe6, D. Allain2
Affiliation(s)
1Multidisciplinary Climate Change Research Laboratory, University of Douala, Douala, Cameroon.
2LEGOS/OMP UMR 5566 (CNES-CNRS-IRD-UPS), Toulouse, France.
3Laboratoire d’Aérologie, CNRS and Toulouse University, Toulouse, France.
4Laboratory of Applied Mechanics and Hydraulic, Faculty of science, University of Yaounde I, Yaounde, Cameroon.
5Faculty of Science, University of Douala, Douala, Cameroon.
6DOUALA Harbour, Douala, Cameroon.
2LEGOS/OMP UMR 5566 (CNES-CNRS-IRD-UPS), Toulouse, France.
3Laboratoire d’Aérologie, CNRS and Toulouse University, Toulouse, France.
4Laboratory of Applied Mechanics and Hydraulic, Faculty of science, University of Yaounde I, Yaounde, Cameroon.
5Faculty of Science, University of Douala, Douala, Cameroon.
6DOUALA Harbour, Douala, Cameroon.
ABSTRACT
Time series of sea level heights have been collected at different stations along the Cameroon coast. The dataset covers a period ranging from 2007 to 2012. Tide data measured by float type recorders have
been digitalized and quality-controlled with tools developed at
Laboratoire d’Etudes Géophysique et Océanographie Spatiale (LEGOS).
Short gaps in the data have been interpolated while large gaps were not.
Tide constituents were retrieved through harmonic analysis using 123
waves having a period ranging from long ones to eighth-diurnal ones. The
reconstructed signal is used to assess the quality of both the data and
the analysis and the erroneous records were examined and corrected. The
effect of the hourly averaging of the raw data on the quality of the
analysis is also investigated. The tide constituents having the largest
amplitudes are, as expected, the semi-diurnal, diurnal, fourth-diurnal
and long term constituents. The major components of semi-diurnal waves
are the M2 and S2 tides. The M2 tide height ranges between 0.5 and 0.85
m. The maximum height is found at Cameroon estuary and the minimum at
the Kribi station located in the South coast. The S2 constituent varies
similarly as the M2 constituent. Its amplitude ranges between 0.18 and
0.52 m. The lowest S2 amplitude occurs also at Kribi station. In the
Dibamba estuary the spectrum shows a larger number of significant
semi-diurnal and fourth-diurnal waves than other zones. Concerning
diurnal waves, the dominant one is the K1 tide and its amplitude is
homogeneous along the coast. The influence of the long-term components
is the strongest in the Cameroon estuary due to important fluctuations
of the rivers run-off.
Cite this paper
References
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