Accéder au contenu Accéder au menu principal Accéder à la recherche
Accéder au contenu Accéder au menu principal
UQAM logo
Page d'accueil de l'UQAM Étudier à l'UQAM Bottin du personnel Carte du campus Bibliothèques Pour nous joindre

Service des bibliothèques

Centre pour l’étude et la simulation du climat à l’échelle régionale (ESCER)
UQAM logo
Centre pour l’étude et la simulation du climat à l’échelle régionale (ESCER)
  • Bibliographie
  • Accueil
  1. Vitrine des bibliographies
  2. Centre pour l’étude et la simulation du climat à l’échelle régionale (ESCER)
  3. Late Holocene Sea Surface Instabilities in the Disko Bugt Area, West Greenland, in Phase With δ<sup>18</sup> O Oscillations at Camp Century
  • Accueil

Bibliographie complète

Retourner à la liste des résultats
  • 1
  • ...
  • 475
  • 476
  • 477
  • 478
  • 479
  • ...
  • 888
  • Page 477 de 888

Late Holocene Sea Surface Instabilities in the Disko Bugt Area, West Greenland, in Phase With δ<sup>18</sup> O Oscillations at Camp Century

RIS

Format recommandé pour la plupart des logiciels de gestion de références bibliographiques

BibTeX

Format recommandé pour les logiciels spécialement conçus pour BibTeX

Type de ressource
Article de revue
Auteurs/contributeurs
  • Allan, Estelle (Auteur)
  • De Vernal, Anne (Auteur)
  • Knudsen, Mads Faurschou (Auteur)
  • Hillaire‐Marcel, Claude (Auteur)
  • Moros, Matthias (Auteur)
  • Ribeiro, Sofia (Auteur)
  • Ouellet‐Bernier, Marie‐Michèle (Auteur)
  • Seidenkrantz, Marit‐Solveig (Auteur)
Titre
Late Holocene Sea Surface Instabilities in the Disko Bugt Area, West Greenland, in Phase With δ<sup>18</sup> O Oscillations at Camp Century
Résumé
Abstract Palynological analyses of sediment core MSM343310 from Disko Bugt (68°38′861°N, 53°49′493°W) document decadal‐ to centennial‐scale variability of sea surface conditions during the last ~ 3,600 years. Dinocyst fluxes (>10 4 cysts/cm 2  yr −1 ) indicate a very high productivity. Dinocyst assemblages dominated by Islandinium minutum , Brigantedinium spp., Islandinium ? cezare , and the cyst of Pentapharsodinium dalei suggest low surface salinity and marked shifts in summer sea surface temperature. The application of the modern analog technique to dinocyst assemblages, using an updated reference data set with new sites from the West Greenland margin, led to reconstruct decadal‐centennial‐scale variations in sea surface salinity and temperature, in phase with the δ 18 O variations in the Camp Century ice core. At ~ 1.5 ka BP, the seasonal sea ice cover records an important regime change, from winter‐only sea ice to more unstable conditions marked by successive cooling pulses with sea ice cover of up to 8 months/yr. The data suggest a close relationship between hydrographic conditions and regional climate over Greenland. Our record shows variations with a mean 200 years periodicity until ~2 ka BP, which supports the hypothesis of climate variations driven by solar variability. After 1.5 ka BP, our data show a variability characterized by a 60–70 year periodicity, which suggests linkages with the Atlantic Multidecadal Oscillation and southwestward migration of the atmospheric polar front. The most recent part of the record, from ~1900 CE to 2007 CE, is characterized by assemblages reflecting warmer surface conditions and reduced sea ice cover. , Key Points Sea surface salinity changes are used as indicators of fresh‐meltwater events and sea ice cover as a diagnostic feature of regional climate Changing sea surface conditions from Disko Bugt are closely related with regional climate over Greenland A marked change in surface waters at about 1.5 ka BP corresponds to enhanced sea ice cover and the onset of unstable conditions
Publication
Paleoceanography and Paleoclimatology
Volume
33
Numéro
2
Pages
227-243
Date
02/2018
Abrév. de revue
Paleoceanog and Paleoclimatol
Langue
en
DOI
10.1002/2017PA003289
ISSN
2572-4517, 2572-4525
URL
https://agupubs.onlinelibrary.wiley.com/doi/10.1002/2017PA003289
Consulté le
11/11/2024 19:29
Catalogue de bibl.
DOI.org (Crossref)
Autorisations
http://onlinelibrary.wiley.com/termsAndConditions#vor
Référence
Allan, E., De Vernal, A., Knudsen, M. F., Hillaire‐Marcel, C., Moros, M., Ribeiro, S., Ouellet‐Bernier, M., & Seidenkrantz, M. (2018). Late Holocene Sea Surface Instabilities in the Disko Bugt Area, West Greenland, in Phase With δ18 O Oscillations at Camp Century. Paleoceanography and Paleoclimatology, 33(2), 227–243. https://doi.org/10.1002/2017PA003289
Auteur·e·s
  • De Vernal, Anne
Lien vers cette notice
https://bibliographies.uqam.ca/escer/bibliographie/VV42FRFE
  • 1
  • ...
  • 475
  • 476
  • 477
  • 478
  • 479
  • ...
  • 888
  • Page 477 de 888

UQAM - Université du Québec à Montréal

  • Centre pour l’étude et la simulation du climat à l’échelle régionale (ESCER)
  • bibliotheques@uqam.ca

Accessibilité Web