Persistent Positive North Atlantic Oscillation Mode Dominated the Medieval Climate Anomaly

Publikationstyp:
Zeitschriftenaufsatz
Metadaten:
Autoren
  • Valerie Trouet
  • Jan Esper
  • Nicholas E Graham
  • Andy Baker
  • James D Scourse
  • David C Frank
Autoren-URL
https://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=fis-test-1&SrcAuth=WosAPI&KeyUT=WOS:000264802100035&DestLinkType=FullRecord&DestApp=WOS_CPL
DOI
10.1126/science.1166349
eISSN
1095-9203
Externe Identifier
  • Clarivate Analytics Document Solution ID: 427TN
  • PubMed Identifier: 19342585
ISSN
0036-8075
Ausgabe der Veröffentlichung
5923
Zeitschrift
SCIENCE
Paginierung
78 - 80
Datum der Veröffentlichung
2009
Status
Published
Titel
Persistent Positive North Atlantic Oscillation Mode Dominated the Medieval Climate Anomaly
Sub types
  • Article
Ausgabe der Zeitschrift
324

Datenquelle: Web of Science (Lite)

Andere Metadatenquellen:
Abstract
<jats:p>The Medieval Climate Anomaly (MCA) was the most recent pre-industrial era warm interval of European climate, yet its driving mechanisms remain uncertain. We present here a 947-year-long multidecadal North Atlantic Oscillation (NAO) reconstruction and find a persistent positive NAO during the MCA. Supplementary reconstructions based on climate model results and proxy data indicate a clear shift to weaker NAO conditions into the Little Ice Age (LIA). Globally distributed proxy data suggest that this NAO shift is one aspect of a global MCA-LIA climate transition that probably was coupled to prevailing La Niña–like conditions amplified by an intensified Atlantic meridional overturning circulation during the MCA.</jats:p>
Autoren
  • Valérie Trouet
  • Jan Esper
  • Nicholas E Graham
  • Andy Baker
  • James D Scourse
  • David C Frank
DOI
10.1126/science.1166349
eISSN
1095-9203
ISSN
0036-8075
Ausgabe der Veröffentlichung
5923
Zeitschrift
Science
Sprache
en
Paginierung
78 - 80
Datum der Veröffentlichung
2009
Status
Published
Herausgeber
American Association for the Advancement of Science (AAAS)
Herausgeber URL
http://dx.doi.org/10.1126/science.1166349
Datum der Datenerfassung
2024
Titel
Persistent Positive North Atlantic Oscillation Mode Dominated the Medieval Climate Anomaly
Ausgabe der Zeitschrift
324

Datenquelle: Crossref

Abstract
The Medieval Climate Anomaly (MCA) was the most recent pre-industrial era warm interval of European climate, yet its driving mechanisms remain uncertain. We present here a 947-year-long multidecadal North Atlantic Oscillation (NAO) reconstruction and find a persistent positive NAO during the MCA. Supplementary reconstructions based on climate model results and proxy data indicate a clear shift to weaker NAO conditions into the Little Ice Age (LIA). Globally distributed proxy data suggest that this NAO shift is one aspect of a global MCA-LIA climate transition that probably was coupled to prevailing La Niña-like conditions amplified by an intensified Atlantic meridional overturning circulation during the MCA.
Addresses
  • Swiss Federal Institute for Forest, Snow, and Landscape Research (WSL), Zürcherstrasse 111, 8903 Birmensdorf, Switzerland. trouet@wsl.ch
Autoren
  • Valérie Trouet
  • Jan Esper
  • Nicholas E Graham
  • Andy Baker
  • James D Scourse
  • David C Frank
DOI
10.1126/science.1166349
eISSN
1095-9203
Externe Identifier
  • PubMed Identifier: 19342585
Open access
false
ISSN
0036-8075
Ausgabe der Veröffentlichung
5923
Zeitschrift
Science (New York, N.Y.)
Sprache
eng
Medium
Print
Paginierung
78 - 80
Datum der Veröffentlichung
2009
Status
Published
Datum der Datenerfassung
2009
Titel
Persistent positive North Atlantic oscillation mode dominated the Medieval Climate Anomaly.
Sub types
  • Research Support, Non-U.S. Gov't
  • Research Support, U.S. Gov't, Non-P.H.S.
  • Journal Article
Ausgabe der Zeitschrift
324

Datenquelle: Europe PubMed Central

Abstract
The Medieval Climate Anomaly (MCA) was the most recent pre-industrial era warm interval of European climate, yet its driving mechanisms remain uncertain. We present here a 947-year-long multidecadal North Atlantic Oscillation (NAO) reconstruction and find a persistent positive NAO during the MCA. Supplementary reconstructions based on climate model results and proxy data indicate a clear shift to weaker NAO conditions into the Little Ice Age (LIA). Globally distributed proxy data suggest that this NAO shift is one aspect of a global MCA-LIA climate transition that probably was coupled to prevailing La Niña-like conditions amplified by an intensified Atlantic meridional overturning circulation during the MCA.
Autoren
  • Valérie Trouet
  • Jan Esper
  • Nicholas E Graham
  • Andy Baker
  • James D Scourse
  • David C Frank
Autoren-URL
https://www.ncbi.nlm.nih.gov/pubmed/19342585
DOI
10.1126/science.1166349
eISSN
1095-9203
Ausgabe der Veröffentlichung
5923
Zeitschrift
Science
Sprache
eng
Country
United States
Paginierung
78 - 80
PII
324/5923/78
Datum der Veröffentlichung
2009
Status
Published
Datum, an dem der Datensatz öffentlich gemacht wurde
2009
Titel
Persistent positive North Atlantic oscillation mode dominated the Medieval Climate Anomaly.
Sub types
  • Journal Article
  • Research Support, Non-U.S. Gov't
  • Research Support, U.S. Gov't, Non-P.H.S.
Ausgabe der Zeitschrift
324

Datenquelle: PubMed

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