¡Nos trasladamos! E-Prints cerrará el 7 de junio.

En las próximas semanas vamos a migrar nuestro repositorio a una nueva plataforma con muchas funcionalidades nuevas. En esta migración las fechas clave del proceso son las siguientes:

Es muy importante que cualquier depósito se realice en E-Prints Complutense antes del 7 de junio. En caso de urgencia para realizar un depósito, se puede comunicar a docta@ucm.es.

The Stratospheric Pathway of La Niña



Downloads per month over past year

Iza San Juan, Maddalen and Calvo Fernández, Natalia and Manzini, Elisa (2016) The Stratospheric Pathway of La Niña. Journal of climate, 29 (24). pp. 8899-8914. ISSN 0894-8755

[thumbnail of calvofernandez36libre (embargar hasta 1 de junio de 2017).pdf]

Official URL: http://dx.doi.org/10.1175/JCLI-D-16-0230.1


A Northern Hemisphere (NH) polar stratospheric pathway for La Nina events is established during wintertime based on reanalysis data for the 1958-2012 period. A robust polar stratospheric response is observed in the NH during strong La Nina events, characterized by a significantly stronger and cooler polar vortex. Significant wind anomalies reach the surface, and a robust impact on the North Atlantic-European (NAE) region is observed. A dynamical analysis reveals that the stronger polar stratospheric winds during La Nina winters are due to reduced upward planetary wave activity into the stratosphere. This finding is the result of destructive interference between the climatological and the anomalous La Nina tropospheric stationary eddies over the Pacific-North American region. In addition, the lack of a robust stratospheric signature during La Nina winters reported in previous studies is investigated. It is found that this is related to the lower threshold used to detect the events, which signature is consequently more prone to be obscured by the influence of other sources of variability. In particular, the occurrence of stratospheric sudden warmings (SSWs), partly linked to the phase of the quasi-biennial oscillation, modulates the observed stratospheric signal. In the case of La Nina winters defined by a lower threshold, a robust stratospheric cooling is found only in the absence of SSWs. Therefore, these results highlight the importance of using a relatively restrictive threshold to define La Nina events in order to obtain a robust surface response in the NAE region through the stratosphere.

Item Type:Article
Additional Information:

© 2016 American Meteorological Society. We acknowledge the Japan Meteorological Agency for providing JRA-55 reanalysis data, the University of East Anglia Climatic Research Unit (CRU) for the TS3.21dataset, and the National Center for Environmental Prediction/Climate Prediction Center (NCEP/CPC) for the N3.4 index. M. I. and N. C. are supported by the Spanish Ministry of Economy and Competitiveness through the MATRES (CGL2012-34221) project and the European Project 603557 STRATOCLIM under Program FP7-ENV. 2013.6.1-2. The authors are grateful to R. García Herrera and D. Barriopedro for their helpful discussions and the editor and reviewers who helped improve the manuscript. This work was partially performed during a visit of M. I. at the Max Planck Institute for Meteorology, Hamburg, and M. I. acknowledges MPI-M for the support.

Uncontrolled Keywords:El niño; Southern-oscillation; Sudden warmings; North-Atlantic; Polar vortex; Winter; Reanalysis; Events; Enso; Teleconnections
Subjects:Sciences > Physics > Astrophysics
Sciences > Physics > Astronomy
ID Code:40978
Deposited On:07 Mar 2017 14:59
Last Modified:10 Dec 2018 15:04

Origin of downloads

Repository Staff Only: item control page