Low-Frequency Signals in Long Tree-Ring Chronologies for Reconstructing Past Temperature Variability

By J. Esper, E. Cook, F. Schweingruber. Science, 2002

1,482 citations recorded by the source corpus.

Subfields: Atmospheric Science, Global and Planetary Change

View Paper: https://www.semanticscholar.org/paper/223fd9957ae197bc1d6af5494545f01bfd0af434

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Citations in the corpus

Millennial temperature reconstruction intercomparison and evaluation (2006, neutral): “Correspondence to: M. N. Juckes (m.n.juckes@rl.ac.uk)”
Environmental variability and fisheries: what can models do? (2008, background): “The author wrongly assumed the LIA to have lasted from 1800 to 1880, while it is usually assumed to have lasted from the fifteenth to the nineteenth century (Houghton et al. 2001; Esper et al. 2002; Oerlemans 2005).”
Internal and forced climate variability during the last millennium: a model-data comparison using ensemble simulations (2005, background): “…averaged over the Northern Hemisphere display relatively warm conditions at the beginning of the 2nd millennium AD, albeit cooler than in the late 20th century (e.g., Jones et al. 1998; Mann et al., 1999; Crowley and Lowery, 2000; Briffa et al., 2001; Briffa and Osborn, 2002; Esper et al., 2002).”
A Test of Climate, Sun, and Culture Relationships from an 1810-Year Chinese Cave Record (2008, neutral): “Esper et al., 2002 T a n o m a ly ( o C ) -0.8 -0.4 0 NH temp.”
The influence of volcanic, solar and CO2 forcing on the temperatures in the Dalton Minimum (1790–1830): a model study (2005, background): “Several empirical temperature reconstructions (Jones et al. 1998; Mann et al. 1999; Esper et al. 2002) show a temperature depression in the Northern Hemisphere in the beginning of the nineteenth century, especially the reconstruction of Esper et al. (2002) .”
Are multiproxy climate reconstructions robust? (2005, background): “[2] Among several proxy-based approaches of reconstructing real or synthetic millennial climate [Overpeck et al., 1997; Jones et al., 1998; Briffa, 2000; Crowley and Lowery, 2000; Briffa et al., 2001, 2004; Esper et al., 2002; Zorita et al., 2003; Jones and Mann, 2004; von Storch et al., 2004] the m”
Detection of climate signal in dendrochronological data analysis: a comparison of tree-ring standardization methods (2004, background): “climate signal. Preserving the lowfrequency signal in tree-ring chronologies (Briffa et al., 1992; Esper et al., 2002 ) requires the use of standardization techniques that have not been extensively studied.”
Low‐frequency noise in δ13C and δ18O tree ring data: A case study of Pinus uncinata in the Spanish Pyrenees (2010, methodology): “The climatic component of the offset may be preserved via the application of RCS, a technique that allows deviations from the mean of all age‐aligned data to be retained in the detrended chronology [Esper et al., 2002].”
Reconstructing surface temperature changes over the past 600 years using climate model simulations with data assimilation (2010, background): “This renewed focus has led to numerous efforts employing climate “proxy” records to reconstruct climate at the hemispheric [e.g., Mann et al., 1999, 2008; Esper et al., 2002; Mann and Jones, 2003; Moberg et al., 2005; D’Arrigo et al., 2006; Juckes et al., 2007; Hegerl et al., 2007] and regional [Lut”
Description of the Earth system model of intermediate complexity LOVECLIM version 1.2 (2010, methodology): “…is: B2000 to Briffa (2000) calibrated by Briffa et al. (2004), BOS2001 to Briffa et al. (2001), DWJ2006 to D’Arrigo et al. (2006), ECS2002 to Esper et al. (2002), recalibrated by Cook et al. (2004a), HCA2006 to Hergel et al. (2006), JBB1998 to Jones et al. (1998) calibrated by Jones et al.…”
Climate and carbon-cycle variability over the last millennium (2010, neutral): “Experiment Warmest Coldest Reconstruction Warmest Coldest MWP period LIA period MWP period LIA period E1 1 1070–1099 1670–1699 JBB1988 1030–1059 1600–1629 E1 2 1100–1129 1670–1699 MBH1999 1150–1169 1660–1689 E1 3 1190–1219 1580–1609 ECS2002 980–1009 1600–1629 E1 4 1250–1279 1640–1669 B2000 980–1009 ”