ENSO and Pacific Decadal Variability in the Community Climate System Model Version 4
Top Cited Papers
- 10 April 2012
- journal article
- Published by American Meteorological Society in Journal of Climate
- Vol. 25 (8), 2622-2651
- https://doi.org/10.1175/jcli-d-11-00301.1
Abstract
This study presents an overview of the El Niño–Southern Oscillation (ENSO) phenomenon and Pacific decadal variability (PDV) simulated in a multicentury preindustrial control integration of the NCAR Community Climate System Model version 4 (CCSM4) at nominal 1° latitude–longitude resolution. Several aspects of ENSO are improved in CCSM4 compared to its predecessor CCSM3, including the lengthened period (3–6 yr), the larger range of amplitude and frequency of events, and the longer duration of La Niña compared to El Niño. However, the overall magnitude of ENSO in CCSM4 is overestimated by ~30%. The simulated ENSO exhibits characteristics consistent with the delayed/recharge oscillator paradigm, including correspondence between the lengthened period and increased latitudinal width of the anomalous equatorial zonal wind stress. Global seasonal atmospheric teleconnections with accompanying impacts on precipitation and temperature are generally well simulated, although the wintertime deepening of the Al... AbstractThis study presents an overview of the El Niño–Southern Oscillation (ENSO) phenomenon and Pacific decadal variability (PDV) simulated in a multicentury preindustrial control integration of the NCAR Community Climate System Model version 4 (CCSM4) at nominal 1° latitude–longitude resolution. Several aspects of ENSO are improved in CCSM4 compared to its predecessor CCSM3, including the lengthened period (3–6 yr), the larger range of amplitude and frequency of events, and the longer duration of La Niña compared to El Niño. However, the overall magnitude of ENSO in CCSM4 is overestimated by ~30%. The simulated ENSO exhibits characteristics consistent with the delayed/recharge oscillator paradigm, including correspondence between the lengthened period and increased latitudinal width of the anomalous equatorial zonal wind stress. Global seasonal atmospheric teleconnections with accompanying impacts on precipitation and temperature are generally well simulated, although the wintertime deepening of the Al...Keywords
This publication has 90 references indexed in Scilit:
- The Impact of Extratropical Atmospheric Variability on ENSO: Testing the Seasonal Footprinting Mechanism Using Coupled Model ExperimentsJournal of Climate, 2010
- Extratropical air-sea interaction, sea surface temperature variability, and the Pacific Decadal OscillationPublished by American Geophysical Union (AGU) ,2010
- Forecasting Pacific SSTs: Linear Inverse Model Predictions of the PDOJournal of Climate, 2008
- Extratropical Atmosphere–Ocean Variability in CCSM3Journal of Climate, 2006
- Tropical Pacific sea‐surface temperatures and preceding sea level pressure anomalies in the subtropical North PacificJournal of Geophysical Research: Atmospheres, 2003
- The Version-2 Global Precipitation Climatology Project (GPCP) Monthly Precipitation Analysis (1979–Present)Journal of Hydrometeorology, 2003
- The Atmospheric Bridge: The Influence of ENSO Teleconnections on Air–Sea Interaction over the Global OceansJournal of Climate, 2002
- Winter-to-winter recurrence of sea surface temperature, salinity and mixed layer depth anomaliesProgress in Oceanography, 2001
- Interdecadal Change of the Structure of the ENSO Mode and Its Impact on the ENSO Frequency*Journal of Climate, 2000
- A Mechanism for the Recurrence of Wintertime Midlatitude SST AnomaliesJournal of Physical Oceanography, 1995