Ensayos de la simulación del índice NAO de invierno con datos de CMIP5

  1. Nube González-Reviriego 1
  2. Concepción Rodríguez Puebla 1
  3. Belén Rodríguez-Fonseca 2
  1. 1 Universidad de Salamanca
    info

    Universidad de Salamanca

    Salamanca, España

    ROR https://ror.org/02f40zc51

  2. 2 Universidad Complutense de Madrid
    info

    Universidad Complutense de Madrid

    Madrid, España

    ROR 02p0gd045

Book:
Cambio climático. Extremos e impactos: [ponencias presentadas al VIII Congreso Internacional de la Asociación Española de Climatología]
  1. Concepción Rodríguez Puebla (coord.)
  2. Antonio Ceballos Barbancho (coord.)
  3. Nube González Reviriego (coord.)
  4. Enrique Morán Tejeda (coord.)
  5. Ascensión Hernández Encinas (coord.)

Publisher: Asociación Española de Climatología

ISBN: 978-84-695-4331-3

Year of publication: 2012

Pages: 116-123

Congress: Asociación Española de Climatología. Congreso (8. 2012. Salamanca)

Type: Conference paper

Abstract

Results from the IPCC AR4 report and other recent analyses of temperature and precipitation from CMIP3 dataset, agreed that Mediterranean region and Iberian Peninsula are highly vulnerable to the impacts of climate change. Due to the connections between those variables and Teleconnections patterns, is interesting to study them under increasing emission scenarios, to apply this study for regional downscaling. This work shows results of the North Atlantic Oscillation (NAO) pattern for winter season (DJF). This pattern was obtained from 500 hPa geopotential height data from the World Climate Research Programme ́s (WCRP ́s) Coupled Model Intercomparison Project phase 5 (CMIP5) with the experiments “Historical “ and “RCP 8.5”. We used Partial Least Squares Regression (PLS) procedure in order to obtain the patterns and indices, taking into account the patterns of the Climate Prediction Center (CPC) of NOAA as reference. Results focus on spatial and temporal analysis of the multi-model that was built with models that best reproduce the observed NAO according to the Taylor Diagram.