@article{fdi:010068296, title = {{I}nfluence of oceanic intraseasonal {K}elvin waves on {E}astern {P}acific hurricane activity}, author = {{B}oucharel, {J}. and {J}in, {F}. {F}. and {E}ngland, {M}. {H}. and {D}ewitte, {B}oris and {L}in,, {II} and {H}uang, {H}. {C}. and {B}almaseda, {M}. {A}.}, editor = {}, language = {{ENG}}, abstract = {{R}ecent studies have highlighted the role of subsurface ocean dynamics in modulating eastern {P}acific ({EP}ac) hurricane activity on interannual time scales. {I}n particular, the well-known {E}l {N}ino-{S}outhern {O}scillation ({ENSO}) recharge-discharge mechanism has been suggested to provide a good understanding of the year-to-year variability of hurricane activity in this region. {T}his paper investigates the influence of equatorial subsurface subannual and intraseasonal oceanic variability on tropical cyclone ({TC}) activity in the {EP}ac. {T}hat is to say, it examines previously unexplored time scales, shorter than interannual, in an attempt to explain the variability not related to {ENSO}. {U}sing ocean reanalysis products and {TC} best-track archive, the role of subannual and intraseasonal equatorial {K}elvin waves ({EKW}) in modulating hurricane intensity in the {EP}ac is examined. {I}t is shown first that these planetary waves have a clear control on the subannual and intraseasonal variability of thermocline depth in the {EP}ac cyclone-active region. {T}his is found to affect ocean subsurface temperature, which in turn fuels hurricane intensification with a marked seasonal-phase locking. {T}his mechanism of {TC} fueling, which explains up to 30% of the variability of {TC} activity unrelated to {ENSO} (around 15%-20% of the total variability), is embedded in the large-scale equatorial dynamics and therefore offers some predictability with lead time up to 3-4 months at seasonal and subseasonal time scales.}, keywords = {{PACIFIQUE} ; {ZONE} {EQUATORIALE}}, booktitle = {}, journal = {{J}ournal of {C}limate}, volume = {29}, numero = {22}, pages = {7941--7955}, ISSN = {0894-8755}, year = {2016}, DOI = {10.1175/jcli-d-16-0112.1}, URL = {https://www.documentation.ird.fr/hor/fdi:010068296}, }