El Niño/Southern Oscillation and tropical Pacific climate during the last millennium

By K. Cobb, C. Charles, Hai Cheng, R. Edwards. Nature, 2003

953 citations recorded by the source corpus.

Subfields: Atmospheric Science, Geology, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/e2fa56b3ceb4654af50a4f9cb239f5d76adb6991

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Atmospheric Science

1. A. Timmermann
2. Chunzai Wang
3. M. Wolff
4. F. Keyl
5. J. Picaut
6. M. Cane
7. R. Seager
8. Shang-Ping Xie

In Geology

1. M. Cane

In Global and Planetary Change

1. M. Cane
2. A. Timmermann
3. J. Picaut
4. Chunzai Wang
5. F. Keyl
6. M. Wolff
7. R. Seager
8. Shang-Ping Xie

Citations in the corpus

• Herbivory and plant growth rate determine the success of El Niño Southern Oscillation‐driven tree establishment in semiarid South America (2006, neutral): “, 2001), and although there are considerable uncertainties in the prediction of such future events (Collins, 2000; Cobb et al., 2003), ENSO events could increase in magnitude and frequency as result of global climate warming (Timmermann et al.”
• Volcanic and Solar Forcing of the Tropical Pacific over the Past 1000 Years (2005, background): “This evidence seems to substantiate previous claims of a relationship between tropical volcanic eruptions and El Niño events based on the relatively short instrumental record (Handler 1984), though such claims are controversial (e.g., Nicholls 1990; Robock 2000).”
• Environmental variability and fisheries: what can models do? (2008, background): “The origin of climatic cycles is assumed to be found in the astronomic oscillations (Milanković cycle, sun spot cycle and others) and the deviations of these (Royer 1993; Parker et al. 1995; Lean 2002; Berger et al. 2002; Cobb et al. 2003; Cane 2005).”
• The Effect of Orbital Forcing on the Mean Climate and Variability of the Tropical Pacific (2007, background): “Past ENSO variability has been reconstructed for time slices throughout the last 120 000 yr (Sandweiss et al. 1996; Hughen et al. 1999; Rodbell et al. 1999; Rittenour et al. 2000; Corrège et al. 2000; Cole 2001; Tudhope et al. 2001; Moy et al. 2002; Andrus et al. 2002; Cobb et al. 2003).”
• Understanding Enso Physics—A Review (2013, background): “…several articles discussing decadal variations of ENSO during the last millennium rely on either a single set of paleoclimate proxies over an extended period of time [e.g., Linsley et al., 2000] or several sets of proxies in the same location over separate periods of time [e.g., Cobb et al., 2003].”
• El Niño as a mediator of the solar influence on climate (2007, result): “[33] We turn to the paleoclimate record to test the idea of a solar-induced ‘‘thermostat.’’ Mann et al. [2005] show that their result is consistent with the Palmyra ENSO record of Cobb et al. [2003] : At times of increased irradiance, such as the Medieval Warm Period (900–1300 A.D.), the average co”
• The evolution of El Nino, past and future (2005, result): “[34] showed cooling in the eastern equatorial Pacific at times in the past when the global climate warmed due to increased solar radiation or reduced volcanism, a result reproduced in the modeling study of Mann et al.”