@article{fdi:010065396, title = {{O}cean swell variability along the northern coast of the {G}ulf of {G}uinea}, author = {{T}oualy, {E}. and {A}man, {A}. and {K}offi, {P}. and {M}arin, {F}r{\'e}d{\'e}ric and {W}ango, {T}. {E}.}, editor = {}, language = {{ENG}}, abstract = {{T}his study analyses a 4.5 year ({S}eptember 2009-{M}arch 2014) time-series of remotely-sensed data of altimeter significant wave heights to describe the temporal and spatial variability of ocean swells along the northern coast of the {G}ulf of {G}uinea. {T}he {NOAA} {WAVEWATCH} {III} ({NWW}3) wave model data were used with altimeter data to determine the origin of the swells that occur along the coast of {C}ote d'{I}voire in {W}est {A}frica. {W}e show that the ocean swells along the northern coast of the {G}ulf of {G}uinea are generated in the {S}outhern {O}cean and then propagate from south to north in the {S}outh {A}tlantic {O}cean, before turning south-west to north-east close to the coast. {T}his finding corroborates previous studies in this area. {T}he remotely-sensed and {NWW}3 significant wave height data captured the strong swells observed along the coast of {C}ote d'{I}voire from the period 28 {A}ugust-3 {S}eptember 2011, which were responsible for an extreme erosion event of more than 12 m along that country's coastline. {T}his extreme event was triggered by a strong storm in the region between 40 degrees and 60 degrees {S} that occurred eight days previously in the {S}outh {A}tlantic. {T}he waves propagated as swells at a speed of about 875 km day(-1) before reaching the northern {A}frican coast.}, keywords = {peak direction ; peak period ; propagation ; storms ; time-series ; wave ; {GUINEE} {GOLFE} ; {COTE} {D}'{IVOIRE} ; {ATLANTIQUE} {SUD} ; {OCEAN} {AUSTRAL}}, booktitle = {}, journal = {{A}frican {J}ournal of {M}arine {S}cience}, volume = {37}, numero = {3}, pages = {353--361}, ISSN = {1814-232{X}}, year = {2015}, DOI = {10.2989/1814232x.2015.1074940}, URL = {https://www.documentation.ird.fr/hor/fdi:010065396}, }