Reduced ENSO Variability at the LGM Revealed by an Isotope-Enabled Earth System Model

Studying the El Nino Southern Oscillation (ENSO) in the past can help us better understand its dynamics and improve its future projections. However, both paleoclimate reconstructions and model simulations of ENSO strength at the Last Glacial Maximum (LGM; 21 ka B.P.) have led to contradicting result...

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Veröffentlicht in:	Geophysical research letters 2017-07, Vol.44 (13), p.6984-6992
Hauptverfasser:	Zhu, Jiang, Liu, Zhengyu, Brady, Esther, Otto-Bliesner, Bette, Zhang, Jiaxu, Noone, David, Tomas, Robert, Nusbaumer, Jesse, Wong, Tony, Jahn, Alexandra, Tabor, Clay
Format:	Artikel
Sprache:	eng
Schlagworte:	Annual variations Computer simulation direct model‐data comparison Dynamics Earth El Nino El Nino phenomena El Nino-Southern Oscillation event El Niño–Southern Oscillation Foraminifera Isotopes isotope‐enabled simulation Last Glacial Maximum Meteorology And Climatology Ocean temperature Oceanography Oxygen Oxygen isotopes Paleoclimate Records Simulation Southern Oscillation Thermocline Variability Variance analysis Vertical migration
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