Revising midlatitude summer temperatures back to AD600 based on a wood density network

Publikationstyp:
Zeitschriftenaufsatz
Metadaten:
Autoren
  • Lea Schneider
  • Jason E Smerdon
  • Ulf Buentgen
  • Rob JS Wilson
  • Vladimir S Myglan
  • Alexander V Kirdyanov
  • Jan Esper
Autoren-URL
https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=fis-test-1&SrcAuth=WosAPI&KeyUT=WOS:000357511200038&DestLinkType=FullRecord&DestApp=WOS_CPL
DOI
10.1002/2015GL063956
eISSN
1944-8007
Externe Identifier
  • Clarivate Analytics Document Solution ID: CM2LI
ISSN
0094-8276
Ausgabe der Veröffentlichung
11
Zeitschrift
GEOPHYSICAL RESEARCH LETTERS
Schlüsselwörter
  • maximum latewood density
  • tree rings
  • millennial reconstruction
  • volcanic cooling
  • Little Ice Age
  • beta value
Paginierung
4556 - 4562
Datum der Veröffentlichung
2015
Status
Published
Titel
Revising midlatitude summer temperatures back to AD600 based on a wood density network
Sub types
  • Article
Ausgabe der Zeitschrift
42

Datenquelle: Web of Science (Lite)

Andere Metadatenquellen:
Abstract
<jats:title>Abstract</jats:title><jats:p>Annually resolved and millennium‐long reconstructions of large‐scale temperature variability are primarily composed of tree ring width (TRW) chronologies. Changes in ring width, however, have recently been shown to bias the ratio between low‐ and high‐frequency signals. To overcome limitations in capturing the full spectrum of past temperature variability, we present a network of 15 maximum latewood density (MXD) chronologies distributed across the Northern Hemisphere extratropics. Independent subsets of continental‐scale records consistently reveal high MXD before 1580 and after 1910, with below average values between these periods. Reconstructed extratropical summer temperatures reflect not only these long‐term trends but also distinct cooling pulses after large volcanic eruptions. In contrast to TRW‐dominated reconstructions, this MXD‐based record indicates a delayed onset of the Little Ice Age by almost two centuries. The reduced memory inherent in MXD is likely responsible for the rapid recovery from volcanic‐induced cooling in the fourteenth century and the continuation of warmer temperatures until ~1600.</jats:p>
Autoren
  • Lea Schneider
  • Jason E Smerdon
  • Ulf Büntgen
  • Rob JS Wilson
  • Vladimir S Myglan
  • Alexander V Kirdyanov
  • Jan Esper
DOI
10.1002/2015gl063956
eISSN
1944-8007
ISSN
0094-8276
Ausgabe der Veröffentlichung
11
Zeitschrift
Geophysical Research Letters
Sprache
en
Online publication date
2015
Paginierung
4556 - 4562
Datum der Veröffentlichung
2015
Status
Published
Herausgeber
American Geophysical Union (AGU)
Herausgeber URL
http://dx.doi.org/10.1002/2015gl063956
Datum der Datenerfassung
2023
Titel
Revising midlatitude summer temperatures back to A.D. 600 based on a wood density network
Ausgabe der Zeitschrift
42

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