Imprints of climate signals in a 204 year δ18O tree-ring record of nothofagus pumilio from Perito Moreno Glacier, Southern Patagonia (50◦S)

Grießinger J, Langhamer L, Schneider C, Saß B, Steger D, Skvarca P, Braun M, Meier W, Srur AM, Hochreuther P (2018)

Publication Status: Published

Publication Type: Journal article, Original article

Publication year: 2018

Journal

Publisher: Frontiers Media S.A.

Book Volume: 6

Article Number: 27

DOI: 10.3389/feart.2018.00027

Abstract

A 204 year-long record of delta O-18 in tree-ring cellulose of southern beech (Nothofagus pumilio) from a site near Perito Moreno Glacier (50:S) in Southern Patagonia was established to assess its potential for a climate reconstruction. The annually resolved oxygen isotope chronology is built out of seven individual tree-ring delta O-18 series with a significant mean inter-series correlation (r = 0.61) and is the first of its kind located in Southern America south of 50 degrees S. Over a common period from 1960 to 2013 of available stationary and high-resolution gridded CRU TS v. 4.01 data, the delta O-18 chronology exhibits a strong sensitivity toward hydroclimatic as well as temperature parameters as revealed by correlation analyses. Among these, positive correlations with maximum temperature in the first part of the summer season (CRU r(ONDJ) = 0.51, p < 0.01) and negative correlations with precipitation in the latter half of the vegetation period (CRU r(ONDJ) = -0.54, p < 0.01) show the highest sensitivities. A strong supra-regional influence of the Southern Annular Mode (SAM) is clearly recorded in this chronology as indicated by significant positive correlations during the vegetation period (r(ONDJ) = 0.62, p < 0.01). This indicates that the presented delta O-18-chronology shows great promise to reconstruct the influence and variability of the SAM within the last two centuries in southern South America. The modulation of positive and negative anomalies within this series can be interlinked to changes in moisture source origin as revealed by backward trajectory modeling. Additionally, these anomalies can be directly associated to positive or negative phases of the Antarctic Oscillation Index (AAOI) and therefore the strength of the Westerlies. Aligned by the analysis on the influence of different main weather types on the delta O-18 chronology it is shown that such time-series hold the potential to additionally capture their respective influence and change during the last centuries.

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Involved external institutions

Glaciarium, Centro de Interpretación de Glaciares Argentina (AR) Consejo Nacional de Investigaciones Científicas y Técnicas (CONICET) / National Scientific and Technical Research Council Argentina (AR) Humboldt-Universität zu Berlin Germany (DE) Leopold-Franzens-Universität Innsbruck / University of Innsbruck Austria (AT)

How to cite

APA:

Grießinger, J., Langhamer, L., Schneider, C., Saß, B., Steger, D., Skvarca, P.,... Hochreuther, P. (2018). Imprints of climate signals in a 204 year δ18O tree-ring record of nothofagus pumilio from Perito Moreno Glacier, Southern Patagonia (50◦S). Frontiers in Earth Science, 6. https://dx.doi.org/10.3389/feart.2018.00027

MLA:

Grießinger, Jussi, et al. "Imprints of climate signals in a 204 year δ18O tree-ring record of nothofagus pumilio from Perito Moreno Glacier, Southern Patagonia (50◦S)." Frontiers in Earth Science 6 (2018).

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