Last millennium Northern Hemisphere summer temperatures from tree rings: Part II, spatially resolved reconstructions
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F86652079%3A_____%2F17%3A00521427" target="_blank" >RIV/86652079:_____/17:00521427 - isvavai.cz</a>
Alternative codes found
RIV/60460709:41320/17:75463 RIV/00216224:14310/17:00122714
Result on the web
<a href="https://www.sciencedirect.com/science/article/abs/pii/S0277379117301592?via%3Dihub" target="_blank" >https://www.sciencedirect.com/science/article/abs/pii/S0277379117301592?via%3Dihub</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1016/j.quascirev.2017.02.020" target="_blank" >10.1016/j.quascirev.2017.02.020</a>
Alternative languages
Result language
angličtina
Original language name
Last millennium Northern Hemisphere summer temperatures from tree rings: Part II, spatially resolved reconstructions
Original language description
Climate field reconstructions from networks of tree-ring proxy data can be used to characterize regional scale climate changes, reveal spatial anomaly patterns associated with atmospheric circulation changes, radiative forcing, and large-scale modes of ocean-atmosphere variability, and provide spatiotemporal targets for climate model comparison and evaluation. Here we use a multiproxy network of tree-ring chronologies to reconstruct spatially resolved warm season (May August) mean temperatures across the extratropical Northern Hemisphere (40-90 degrees N) using Point-by-Point Regression (PPR). The resulting annual maps of temperature anomalies (750-1988 CE) reveal a consistent imprint of volcanism, with 96% of reconstructed grid points experiencing colder conditions following eruptions. Solar influences are detected at the bicentennial (de Vries) frequency, although at other time scales the influence of insolation variability is weak. Approximately 90% of reconstructed grid points show warmer temperatures during the Medieval Climate Anomaly when compared to the Little Ice Age, although the magnitude varies spatially across the hemisphere. Estimates of field reconstruction skill through time and over space can guide future temporal extension and spatial expansion of the proxy network. (C) 2017 Elsevier Ltd. All rights reserved.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10508 - Physical geography
Result continuities
Project
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Continuities
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Others
Publication year
2017
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Quaternary Science Reviews
ISSN
0277-3791
e-ISSN
—
Volume of the periodical
163
Issue of the periodical within the volume
MAY 2017
Country of publishing house
GB - UNITED KINGDOM
Number of pages
22
Pages from-to
1-22
UT code for WoS article
000401204200001
EID of the result in the Scopus database
2-s2.0-85014656159