Variability of El Niño/Southern Oscillation activity at millennial timescales during the Holocene epoch

By C. Moy, G. O. Seltzer, D. Rodbell, David Morrill Anderson. Nature, 2002

1,776 citations recorded by the source corpus.

Subfields: Atmospheric Science, Earth-Surface Processes, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/a235b4624bd2f3fa564f3322b427a76b1e97e14a

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In Atmospheric Science

1. A. Timmermann
2. Hugues Goosse
3. E. Acuña
4. M. Thiel
5. Shang-Ping Xie
6. S. Lorenz
7. A. Clement
8. X. Crosta

In Earth-Surface Processes

1. Shang-Ping Xie

In Global and Planetary Change

1. A. Timmermann
2. Erasmo C. Macaya
3. W. Arntz
4. E. Acuña
5. M. Thiel
6. Shang-Ping Xie
7. Hugues Goosse
8. Paul A Hohenlohe

Citations in the corpus

• ENSO suppression due to weakening of the North Atlantic thermohaline circulation (2005, background): “This prediction may be testable in the near future using fossil coral data (Tudhope et al. 2001) or varved sediments (Rodbell et al. 1999; Rittenour et al. 2000; Moy et al. 2002).”
• Limits to gene flow in marine animals with planktonic larvae: models of Littorina species around Point Conception, California (2004, background): “Ocean current patterns vary not only on seasonal and annual scales, but also on evolutionary time scales (Moy et al., 2002), so that present-day population genetic structure may not represent equilibrium under observed gene flow conditions.”
• The humboldt current system of northern and central chile : Oceanographic processes, ecological interactions and socioeconomic feedback (2007, background): “The ENSO cycle has been a crucial factor in the global climate for at least the past 130,000 yr (Cane 2005), showing continuous, although variable, activity during the last 12,000 yr (Moy et al. 2002); regionally, it has had a major influence on the Chilean coast since the Holocene (e.”
• The Effect of Orbital Forcing on the Mean Climate and Variability of the Tropical Pacific (2007, positive): “Some of these simulations exhibit an early to mid-Holocene ENSO suppression, in accordance with the different paleoENSO reconstructions (Tudhope et al. 2001; Moy et al. 2002).”
• Evidence from wavelet analysis for a mid-Holocene transition in global climate forcing (2009, background): “(1999) and Moy et al. (2002) studied the lacustrine sediments from Laguna Pallcacocha located in Ecuador (4200 m asl, 2°46′S, 79°14′W) (Fig.”