Linking pollen deposition, snow accumulation and isotopic composition on the Alto dell'Ortles glacier (South Tyrol, Italy) for sub-seasonal dating of a firn temperate core
Daniela Festi1, Luca Carturan2, Werner Kofler1, Giancarlo dalla Fontana2, Fabrizio de Blasi2, Federico Cazorzi3, Edith Bucher4, Volkmar Mair5, Paolo Gabrielli6,7, and Klaus Oeggl11Institute of Botany, University of Innsbruck, Sternwartestraße 15, A-6020 Innsbruck, Austria 2Department of Land, Environment, Agriculture and Forestry, University of Padova, Viale dell'Università 16, 35020 Legnaro (PD) Italy 3Department of Agriculture and Environmental Sciences, University of Udine, via delle Scienze 208, 33100 Udine, Italy 4Autonome Provinz Bozen Südtirol, Landesagentur für Umwelt, Biologisches Labor, Unterbergstraße 2, 39055 Leifers, BZ, Italy 5Autonome Provinz Bozen Südtirol, Amt für Geologie und Baustoffprüfung, Eggentalerstraße 48, 39053 Kardaun (BZ), Italy 6Byrd Polar and Climate Research Center, The Ohio State University, 1090 Carmack Road, Columbus, Ohio 43210-1002, USA 7School of Earth Sciences, 275 Mendenhall Laboratory, The Ohio State University, 125 South Oval 8 Mall, Columbus, OH 43210, USA
Received: 28 Sep 2016 – Accepted for review: 22 Nov 2016 – Discussion started: 22 Nov 2016
Abstract. Dating of ice cores from temperate non-polar glaciers is challenging and often problematic. Yet, a proper timescale is essential for a correct interpretation of the proxies measured in the cores. Here, we introduce a new method developed to obtain a sub-seasonal timescale relying on statistically measured similarities between pollen spectra obtained from core samples, and daily airborne pollen monitoring samples collected in the same area. This approach was developed on a 10 m core retrieved from the temperate firn portion of Alto dell'Ortles glacier (Eastern Italian Alps), for which a five-year annual/seasonal timescale already exists. The aim was to considerably improve this timescale, reaching the highest possible temporal resolution, and testing the efficiency and limits of pollen as a chronological tool. A test of the new timescale was performed by comparing our results to the output (date of layer formation) of the mass balance model EISModel, during the period encompassed by the timescale. The correspondence of the results supports the new sub-seasonal timescale based on pollen analysis. This comparison also allows to draw important conclusions on the post depositional effects of meltwater percolation on the pollen content of the firn core, as well as on the climatic interpretation of the pollen signal. Finally, we provide an example of useful application of the timescale related to the direct comparison of measured meteorological parameters and the stable isotopes composition of the core.
Festi, D., Carturan, L., Kofler, W., dalla Fontana, G., de Blasi, F., Cazorzi, F., Bucher, E., Mair, V., Gabrielli, P., and Oeggl, K.: Linking pollen deposition, snow accumulation and isotopic composition on the Alto dell'Ortles glacier (South Tyrol, Italy) for sub-seasonal dating of a firn temperate core, The Cryosphere Discuss., doi:10.5194/tc-2016-221, in review, 2016.