Articles | Volume 2, issue 3
https://doi.org/10.5194/wcd-2-759-2021
https://doi.org/10.5194/wcd-2-759-2021
Research article
 | 
06 Aug 2021
Research article |  | 06 Aug 2021

Resampling of ENSO teleconnections: accounting for cold-season evolution reduces uncertainty in the North Atlantic

Martin P. King, Camille Li, and Stefan Sobolowski

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Cited articles

Abid, M. A., Kucharski, F., Molteni, F., Kang, I.-S., Tompkins, A. M., and Almazroui, M.: Separating the Indian and Pacific Ocean impacts on the Euro-Atlantic response to ENSO and its transition from early to late winter, J. Climate, 34, 1531–1548, https://doi.org/10.1175/JCLI-D-20-0075.1, 2021. a, b, c
Ayarzagüena, B., Ineson, S., Dunstone, N. J., Baldwin, M. P., and Scaife, A. A.: Intraseasonal effects of El Nino-Southern Oscillation on North Atlantic climate, J. Climate, 31, 8861–8873, https://doi.org/10.1175/JCLI-D-18-0097.1, 2018. a, b, c, d, e
Baldwin, M. P., Birner, T., Brasseur, G., Burrows, J., Butchart, N., Garcia, R., Geller, M., Gray, L., Hamilton, K., Harnik, N., Hegglin, M. I., Langematz, U., Robock, A., Sato, K., and Scaife, A. A.: 100 years of progress in understanding the stratosphere and mesosphere, Meteor. Mon., 59, 27.1–27.62, https://doi.org/10.1175/AMSMONOGRAPHS-D-19-0003.1, 2019. a
Bladé, I., Newman, M., Alexander, M. A., and Scott, J. D.: The late fall extratropical response to ENSO: Sensitivity to coupling and convection in the tropical West Pacific, J. Climate, 21, 6101–6118, https://doi.org/10.1175/2008JCLI1612.1, 2008. a
Brönnimann, S., Xoplaki, E., Casty, C., Pauling, A., and Luterbacher, J.: ENSO influence on Europe during the last centuries, Clim. Dynam., 28, 181–197, https://doi.org/10.1007/s00382-006-0175-z, 2007. a
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Short summary
We re-examine the uncertainty of ENSO teleconnection to the North Atlantic by considering the November–December and January–February months in the cold season, in addition to the conventional DJF months. This is motivated by previous studies reporting varying teleconnected atmospheric anomalies and the mechanisms concerned. Our results indicate an improved confidence in the patterns of the teleconnection. The finding may also have implications on research in predictability and climate impact.