@article{fdi:010054293,
  title = {{S}ea surface temperature variability in the subpolar {A}tlantic over the last two millennia},
  author = {{S}icre, {M}. {A}. and {H}all, {I}. {R}. and {M}ignot, {J}uliette and {K}hodri, {M}yriam and {E}zat, {U}. and {T}ruong, {M}. {X}. and {E}iriksson, {J}. and {K}nudsen, {K}. {L}.},
  editor = {},
  language = {{ENG}},
  abstract = {{A} decadal resolution time series of sea surface temperature ({SST}) spanning the last two millennia is reconstructed by combining a proxy record from a new sediment sequence with previously published data from core {MD}99-2275, north of {I}celand. {T}he alkenone based {SST} reconstruction is validated with historic observational data and compared to a new similar temporal resolution reconstruction obtained from sediment core {RAP}i{D}21-3{K}, in the subpolar {N}orth {A}tlantic. {T}he two {SST} paleorecords show consistent multidecadal scale coolings throughout the interval and similar expressions during the contrasted climatic periods 'colloquially known' as the {M}edieval {C}limatic {A}nomaly ({MCA}) and {L}ittle {I}ce {A}ge ({LIA}). {I}n order to further understand the temporal and spatial {SST} variations and investigate the influence of natural forcings on the observed {SST} changes during the last millennium, we compare our time series to simulations using the {I}nstitut {P}ierre-{S}imon {L}aplace {IPSLCM}4-v2 climate model. {T}his comparison highlights the potential importance of volcanism as a natural forcing driving coherent abrupt cooling events captured in the subpolar {N}orth {A}tlantic records.},
  keywords = {{ATLANTIQUE} {NORD}},
  booktitle = {},
  journal = {{P}aleoceanography},
  volume = {26},
  numero = {},
  pages = {{PA}4218},
  ISSN = {0883-8305},
  year = {2011},
  DOI = {10.1029/2011pa002169},
  URL = {https://www.documentation.ird.fr/hor/fdi:010054293},
}