%0 Journal Article
%9 ACL : Articles dans des revues avec comité de lecture répertoriées par l'AERES
%A Boucharel, J.
%A Jin, F. F.
%A England, M. H.
%A Dewitte, Boris
%A Lin,, II
%A Huang, H. C.
%A Balmaseda, M. A.
%T Influence of oceanic intraseasonal Kelvin waves on Eastern Pacific hurricane activity
%D 2016
%L fdi:010068296
%G ENG
%J Journal of Climate
%@ 0894-8755
%K PACIFIQUE ; ZONE EQUATORIALE
%M ISI:000386206100001
%N 22
%P 7941-7955
%R 10.1175/jcli-d-16-0112.1
%U https://www.documentation.ird.fr/hor/fdi:010068296
%> https://www.documentation.ird.fr/intranet/publi/2016/11/010068296.pdf
%V 29
%W Horizon (IRD)
%X Recent studies have highlighted the role of subsurface ocean dynamics in modulating eastern Pacific (EPac) hurricane activity on interannual time scales. In particular, the well-known El Nino-Southern Oscillation (ENSO) recharge-discharge mechanism has been suggested to provide a good understanding of the year-to-year variability of hurricane activity in this region. This paper investigates the influence of equatorial subsurface subannual and intraseasonal oceanic variability on tropical cyclone (TC) activity in the EPac. That is to say, it examines previously unexplored time scales, shorter than interannual, in an attempt to explain the variability not related to ENSO. Using ocean reanalysis products and TC best-track archive, the role of subannual and intraseasonal equatorial Kelvin waves (EKW) in modulating hurricane intensity in the EPac is examined. It is shown first that these planetary waves have a clear control on the subannual and intraseasonal variability of thermocline depth in the EPac cyclone-active region. This is found to affect ocean subsurface temperature, which in turn fuels hurricane intensification with a marked seasonal-phase locking. This 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.
%$ 032