Low-frequency summer temperature variation in central Sweden since the tenth century inferred from tree rings

The Holocene ◽  
2002 ◽  
Vol 12 (6) ◽  
pp. 667-671 ◽  
Author(s):  
Bjön E. Gunnarson ◽  
Hans W. Linderholm
2014 ◽  
Vol 44 (1-2) ◽  
pp. 75-93 ◽  
Author(s):  
Isabel Dorado Liñán ◽  
Eduardo Zorita ◽  
Jesús Fidel González-Rouco ◽  
Ingo Heinrich ◽  
Filipe Campello ◽  
...  

1994 ◽  
Vol 26 (1) ◽  
pp. 60 ◽  
Author(s):  
C. J. Earle ◽  
L. B. Brubaker ◽  
A. V. Lozhkin ◽  
P. M. Anderson

2019 ◽  
Vol 40 (3) ◽  
pp. 1561-1570
Author(s):  
Yu Liu ◽  
Ching‐Yao Li ◽  
Changfeng Sun ◽  
Huiming Song ◽  
Qiang Li ◽  
...  

Geophysics ◽  
1984 ◽  
Vol 49 (7) ◽  
pp. 1032-1040 ◽  
Author(s):  
Baxter H. Armstrong

Some one‐dimensional models of a heterogeneous solid are presented consisting of a succession of slabs with different anharmonic properties. The equation for the temperature variation in these models due to passage of a longitudinal elastic wave can be solved exactly in the approximation of weak attenuation. The solutions are given in terms of the forced oscillation plus the temperature wave solutions to the homogeneous equation needed to match the boundary conditions of continuity of temperature and thermal current. Thermoelastic attenuation due to this temperature variation is compared to that of Zener’s classical approach. For periodic arrangement of slab properties or upon use of Zener’s boundary condition of vanishing thermal current, the temperature‐wave approach reproduces Zener‐type attenuation. However, a succession of slabs with a random, uncorrelated distribution of the Gruneisen constant leads to a new result with attenuation proportional to the three‐halves power of the wave frequency in the low‐frequency limit. The results are discussed in the context of seismoacoustic wave attenuation.


2003 ◽  
Vol 18 (11) ◽  
pp. 2600-2607 ◽  
Author(s):  
D.D. Khalyavin ◽  
Jiaping Han ◽  
A.M.R Senos ◽  
P.Q. Mantas

Ba2MeWO6 (Me=Mg, Ni, Zn) double perovskites were prepared by the conventional solid-state reaction in a wide temperature range. Single-phase ceramics were obtained only at low temperatures approximately 1200°C, whereas a small amount of second phases existed in the samples sintered at higher temperatures. All the compounds are characterized by the cubic perovskite structure (space group Fm3m) with a complete NaCl type ordering between B-site ions. Anomalous temperature variation of the dielectric loss tangent found in the Ba2NiWO6 perovskite is supposed to be connected with a dielectric relaxation due to electronic hopping within thermally activated Ni3+-6W(6-1/6)+/W5+-6Ni(2+1/6)+ clusters. Dielectric measurements showed that the other two perovskites—Ba2ZnWO6 and Ba2MgWO6—exhibit a positive value of the temperature coefficient of permittivity. Such temperature variation is assumed to be caused by a considerable influence of the second polar mode involving B-site ion vibrations on the low-frequency dielectric properties.


Hydrobiologia ◽  
2008 ◽  
Vol 603 (1) ◽  
pp. 183-196 ◽  
Author(s):  
Martha E. Mather ◽  
Donna L. Parrish ◽  
Cara A. Campbell ◽  
James R. McMenemy ◽  
Joseph M. Smith

2016 ◽  
Author(s):  
Juhani Rinne ◽  
Mikko Alestalo ◽  
Jörg Franke

Abstract. Recently it has been shown that climate estimates derived from tree rings often tend to show erroneous long-term oscillations, i.e. there are spectral biases at low frequencies. The result is independent of parameter studied (precipitation or temperature) or measured proxy (tree ring widths or maximum latewood densities). In order to find reasons for such universal errors, a new reconstruction method is introduced where no age dependence of the tree rings is determined. The aim, however, is not to generate better reconstructions but to study error variances of long-term oscillations. It is shown that paucities and data gaps due to missing trees increase the risk for erroneous low-frequency variability. A general approximate formula is introduced in order to estimate the presence of such a risk. A case study using Torneträsk data from Northern Sweden illustrates how longer periods with missing trees cause paucities and gaps leading to erroneous climatic oscillations. Systematic underestimation of the temperature around AD 1600 and after 1950 (“divergence”) is in the study case explained by such data gaps and paucities.


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