Periodicities in mid- to late-Holocene peatland hydrology identified from Swedish and Lithuanian tree-ring data

被引:8
|
作者
Edvardsson, Johannes [1 ,2 ]
Adolphi, Florian [2 ]
Linderholm, Hans W. [3 ]
Corona, Christophe [4 ,5 ]
Muscheler, Raimund [2 ]
Stoffel, Markus [1 ,6 ,7 ]
机构
[1] Univ Bern, Inst Geol Sci, Dendrolab Ch, Baltzerstr 1 3, CH-3012 Bern, Switzerland
[2] Lund Univ, Dept Geol, Quaternary Sci, Solvegatan 12, SE-22362 Lund, Sweden
[3] Univ Gothenburg, Dept Earth Sci, Box 460, S-40530 Gothenburg, Sweden
[4] CNRS, UMR6042, GEOLAB, Maison Sci Homme 4,Rue Ledru, F-63057 Clermont Ferrand 2, France
[5] Univ Blaise Pascal, Maison Sci Homme 4,Rue Ledru, F-63057 Clermont Ferrand 2, France
[6] Univ Geneva, Inst Environm Sci, Climat Change & Climate Impacts, Blvd Carl Vogt 66, CH-1205 Geneva, Switzerland
[7] Univ Geneva, Dept Earth Sci, Rue Maraichers 13, CH-1205 Geneva, Switzerland
关键词
Wavelet analysis; Spectral analysis; NAO; AMO; Solar variability; Lunar nodal tides; Sweden; Lithuania; NORTH-ATLANTIC OSCILLATION; SCOTS PINE GROWTH; CLIMATIC INFLUENCE; SOLAR-ACTIVITY; RAISED BOGS; LUNI-SOLAR; SEA-LEVEL; VARIABILITY; TEMPERATURE; INDICATORS;
D O I
10.1016/j.quascirev.2016.02.020
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
Twenty-five tree-ring width (TRW) chronologies, developed from moisture sensitive peatland trees in Sweden and Lithuania, and representing eight periods during the mid-Holocene to present, were analysed regarding common periodicities (cycles). Periods of 13-15, 20-22, and 30-35 years were found in most chronologies, while 8-10, 18-19, and 60-65 year periodicities were observed as well, but less commonly. Similar periodicities, especially about 15 and 30 years in duration, were detected in both living and subfossil trees, indicating that the trees have responded to similar forcing mechanisms on those timescales through time. Some of the detected periods may be related to solar variability and lunar nodal tides, but most of the detected periodicities are more likely linked to hydrological changes in the peatlands associated to atmospheric patterns such as the North Atlantic Oscillation (NAO), or variations in sea surface temperatures (i.e. the Atlantic Multidecadal Oscillation, AMO). However, no significant relationships between tree growth, NAO and AMO could be formally established, possibly due to hydrological lag and feedback effects which are typical for peatlands but render in-depth assessments rather difficult. (C) 2016 Elsevier Ltd. All rights reserved.
引用
收藏
页码:200 / 208
页数:9
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