Historical climatology in Greenland

Gavin Schmidt & Michael Mann

Extending the instrumental record of climate beyond the late 19th Century when many of the national weather centers were first started is an important, difficult and undervalued task. It often is more akin to historical detective work than to climatology and can involve long searches in dusty archives, the ability to read archaic scripts and handwriting, and even Latin translations (for instance, when going through the archives of the Paris Observatory) (sounds like a recent bestseller, only less lucrative, no?).

Why bother? Well, it is unfortunate, though probably not coincidental, that the modern record starts at the same time that significant modifications of atmopsheric composition (greenhouse gases, aerosols etc.) were occuring on a global scale. Thus this period is not ideal for assessing the magnitude of natural changes (both intrinsic and forced by natural processes like solar variability or volcanic eruptions) since there is likely a contamination from human-related causes. So extending instrumental records back as far as possible is an important approach to providing a context for modern changes.

A paper published earlier this year (Vinther et al, 2006) on extending the records around Southern Greenland was a great example of how this can be successfuly done, the problems that occur and the techniques that have been developed to deal with them. The authors painstakingly digitised older archived data (back to before 1800 in one case), worked out the conventions that were used, and with a knowledge of present day climate, pieced together series and spotted potential shifts in observing location or time of day that would otherwise contaminate the record.

Proxy records (ice cores, ocean sediments etc.) that are related to climate (in some imperfectly known way, but with non-climatic ‘noise’) go back further. But they need to be calibrated to the instrumental record in order to be used quantitatively. Given that proxy records don’t always extend to the present (due to collection dates, collection method, the physics or biology of the specific proxy) and that it is important to retain some instrumental data for validation of any calibration, there are only ~60-100 years of record left for the calibration – making it very difficult to assess how well the low frequency component (a few decades or longer) is represented (and much of the recent attention to recent proxy reconstructions really relates to exactly this point, rather than technical arguments about data processing). Of course, proxy records can also be usefully combined in a qualitative ways that don’t require calibration (such as Osborn and Briffa, 2006).

The work by Vinther and colleagues in Southern Greenland is therefore key to helping calibrate the Greenland ice core records, and impressively, the correlations to the older data are as good as to the recent record, allowing us to have a little more confidence in the even longer term proxy data for this region. So a good result then, and a paper worth reading for anyone who is actually interested in how these things are done.

Page 1 of 3 | Next page