FN Archimer Export Format PT J TI Statistical processing of West Africa wave directional spectra time-series into a climatology of swell events BT AF OLAGNON, Michel KPOGO-NUWOKLO, Komlan GUEDE, Zakoua AS 1:1;2:1,2;3:1; FF 1:PDG-REM-RDT-LCSM;2:PDG-REM-RDT-LCSM;3:PDG-REM-RDT-LCSM; C1 Ifremer Ctr Brest, F-29280 Plouzane, France. Univ Abomey Calavi, Cotonou, Benin. C2 IFREMER, FRANCE UNIV ABOMEY CALAVI, BENIN SI BREST SE PDG-REM-RDT-LCSM IN WOS Ifremer jusqu'en 2018 copubli-int-hors-europe copubli-sud IF 2.508 TC 4 UR https://archimer.ifremer.fr/doc/00156/26695/24761.pdf LA English DT Article DE ;Joint probabilities;Metocean time-series;Swell spectral models;Ocean wave climate;Event tracking;Offshore fatigue design AB Accurate estimation of long-term sea conditions is a major issue for the design of coastal and offshore structures, for the preparation of marine operations, and for other applications such as marine energy, and coastal erosion. It requires, on the one hand, proper parametric models of the sea state spectra and the statistics of the parameters, and on the other hand, representations of their time evolutions. In some locations such as West Africa, sea conditions are complex with wave spectra showing many well separated peaks corresponding to several swells and wind sea. The present study focuses on swell at a West Africa location. First, a time-consistent triangular model is assessed for the spectral shapes of the swell components. Then statistical analysis of the time-histories of those components is carried out in connection with the storms at their source. A model that is triangular for Hs and a linear trend for period and direction is found appropriate for the time-histories of those parameters within a storm event. Using the empirical distributions of the characteristics of the individual events parameters, it is shown that arbitrary long durations of the swell climate may be reconstructed preserving the main observed statistical properties. PY 2014 PD FEB SO Journal Of Marine Systems SN 0924-7963 PU Elsevier Science Bv VL 130 UT 000328873600010 BP 101 EP 108 DI 10.1016/j.jmarsys.2013.07.003 ID 26695 ER EF