Kamenik, C., Van der Knaap, W. O., Van Leeuwen, J. F. N. and Goslar, T. 2009. Pollen/climate calibration based on a near-annual peat sequence from the Swiss Alps. J. Quaternary Sci., Vol. 24 pp. 529–546. ISSN 0267-8179.
Pollen/climate calibration based on a near-annual peat sequence from the Swiss Alps†
Article first published online: 15 MAY 2009
Copyright © 2009 John Wiley & Sons, Ltd.
Journal of Quaternary Science
Special Issue: Climates of the Past: Evidence from Natural and Documentary Archives
Volume 24, Issue 5, pages 529–546, July 2009
How to Cite
Kamenik, C., Van der Knaap, W. O., Van Leeuwen, J. F. N. and Goslar, T. (2009), Pollen/climate calibration based on a near-annual peat sequence from the Swiss Alps. J. Quaternary Sci., 24: 529–546. doi: 10.1002/jqs.1266
- Issue published online: 16 JUN 2009
- Article first published online: 15 MAY 2009
- Manuscript Accepted: 19 DEC 2008
- Manuscript Revised: 2 DEC 2008
- Manuscript Received: 2 APR 2008
- European Commission. Grant Numbers: Pine Project: EVK2-CT-2002-00136, Millennium Project: 017008-2
- the Swiss National Centre of Competence in Climate Research (Swiss National Science Foundation)
- calibration in time;
- pollen accumulation rates;
- high-resolution dating
The objective of this study was to develop a high-resolution pollen-based climate inference model (using ‘calibration in time’) for the mire Mauntschas (SE Swiss Alps, 1818 m above sea level). We focused on 11 types of pollen and spores (referred to as pollen for simplicity) for which we produced 150 year (a) time series of accumulation rates and percentages. Dating of these series was based on 29 14C dates from pure Sphagnum, spheroidal carbonaceous particles, larch bud moth events, and an age–depth model that took into account probabilities of calibrated 14C ages, the degree of curvature of the age–depth line and changes in concentrations of all major pollen types. Time resolution was 1–5 a. We first smoothed the series using a 3 a triangular filter, thus removing time-resolution dependent changes in variability, and minimising effects of potential dating uncertainties. Using redundancy analysis, we then studied the simultaneous response of the selected pollen to 288 different combinations of monthly temperature or precipitation data measured at Sils Maria (1798 m above sea level), located 9 km from Mauntschas. From AD 1954 to 2002, mean May–August air temperature from the same year explained most (18.1%) of the variation in pollen accumulation rates. The amount of explained variation dropped to 9.9% after detrending all data with a 50 a high-pass filter, which possibly removed non-climatic trends. Temperature explained more variation among PAR than among pollen percentages; however, during the verification period (AD 1864–1953) the former were potentially affected by dating uncertainties and could not be used. For developing a pollen-based temperature inference model, we tested ordinary least squares regression, time series regression, ridge regression, principal components regression, and partial least squares regression. During the well-dated calibration period (AD 1954–2002), ordinary least squares regression based on percentages of six pollen types turned out to be the most parsimonious model, having a cross-validated root mean square error of prediction of 0.23°C for mean April–November temperature. A comparison of reconstructed with measured temperature from Sils Maria during the verification period showed that the model best reflected long-term (at least decadal-scale) temperature changes. Copyright © 2009 John Wiley & Sons, Ltd.