How ENSO behaves as a result of a warming planet, however, is still uncertain. One window to determine its sensitivity to climate change is a look into the past. Because the instrumental record is too short for getting a reliable picture of natural variations in ENSO magnitude and frequency, climate scientists rely on geological and biological clues, such as from lake sediment cores, corals, or tree rings as proxies for past ENSO behavior.
The problem has been, though, that reconstructions of ENSO from such paleo-proxies have not been telling the same story.
Some of these discrepancies in ENSO reconstructions arise because the methods typically applied to combine individual paleo-proxy records do not handle small dating uncertainties amongst the proxies well.
The usual approach has been to combine the individual ENSO proxies and then to calculate the activity of this combined ENSO signal. McGregor and his team found that by turning this analysis around -- first calculating the activity of ENSO in each of the individual paleo-climate reconstructions and then combining the activity time series -- yields a much more consistent and robust view of ENSO's past activity.
The scientists confirmed this new approach with virtual ENSO data obtained from two multi-century-long climate model simulations.
Applying their improved method of reconstructing ENSO activity by synthesizing many different existing proxies and comparing these time series with instrumental data, the scientists found that ENSO was more active during 1979-2009 than during any 30-year period between 1590 and 1880.
The results have been published in journal Climate of the Past.
--ANI (Posted on 29-10-2013)