Author(s)

R. Onguene^1,2,3*, E. Pemha⁴, F. Lyard², Y. Du-Penhoat², G. Nkoue⁵, T. Duhaut³, E. Njeugna¹, P. Marsaleix³, R. Mbiake¹, S. Jombe⁶, D. Allain²

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.

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.

Tide, Cameroon Coast, Harmonic Analysis, Prediction

Onguene, R. , Pemha, E. , Lyard, F. , Du-Penhoat, Y. , Nkoue, G. , Duhaut, T. , Njeugna, E. , Marsaleix, P. , Mbiake, R. , Jombe, S. and Allain, D. (2015) Overview of Tide Characteristics in Cameroon Coastal Areas Using Recent Observations. Open Journal of Marine Science, 5, 81-98. doi: 10.4236/ojms.2015.51008.