FN Archimer Export Format
PT J
TI Contrasting northern and southern European winter climate trends during the Last Interglacial
BT 
AF Salonen, J. Sakari
   Sánchez-Goñi, Maria Fernanda
   Renssen, Hans
   Plikk, Anna
AS 1:1,2;2:2,3;3:4;4:5;
FF 1:;2:;3:;4:;
C1 Department of Geosciences and Geography, University of Helsinki, P.O. Box 64, FI-00014 Helsinki, Finland
   Environnements et Paléoenvironnements Océaniques et Continentaux (EPOC), UMR 5805, University of Bordeaux, F-33615 Pessac, France
   Ecole Pratique des Hautes Etudes, Paris Sciences et Lettres University (EPHE, PSL), F-33615 Pessac, France
   Department of Natural Sciences and Environmental Health, University of South-Eastern Norway, 3800 Bø i Telemark, Norway
   The Archaeologists, National Historical Museums, P.O. Box 5428, SE-11484 Stockholm, Sweden
C2 UNIV HELSINKI, FINLAND
   UNIV BORDEAUX, FRANCE
   EPHE, FRANCE
   UNIV SOUTH EASTERN NORWAY, NORWAY
   NHM SWEDEN, SWEDEN
IF 6.324
TC 4
UR https://archimer.ifremer.fr/doc/00702/81425/85822.pdf
   https://archimer.ifremer.fr/doc/00702/81425/85823.xlsx
   https://archimer.ifremer.fr/doc/00702/81425/85824.xlsx
   https://archimer.ifremer.fr/doc/00702/81425/85825.pdf
LA English
DT Article
CR IMAGES 1-MD101
   IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
   IMAGES V LEG 5
   MD 142 / ALIENOR 2
BO Marion Dufresne
AB The Last Interglacial (LIG; 130–115 ka) is an important test bed for climate science as an instance of significantly warmer than preindustrial global temperatures. However, LIG climate patterns remain poorly resolved, especially for winter, affected by a suite of strong feedbacks such as changes in sea-ice cover in the high latitudes. We present a synthesis of winter temperature and precipitation proxy data from the Atlantic seaboard of Europe, spanning from southern Iberia to the Arctic. Our data reveal distinct, opposite latitudinal climate trends, including warming winters seen in the European Arctic while cooling and drying occurred in southwest Europe over the LIG. Climate model simulations for 130 and 120 ka suggest these contrasting climate patterns were affected by a shift toward an atmospheric circulation regime with an enhanced meridional pressure gradient and strengthened midlatitude westerlies, leading to a strong reduction in precipitation across southern Europe. 
PY 2021
PD OCT
SO Geology
SN 0091-7613
PU Geological Society of America
VL 49
IS 10
UT 000705084600013
BP 1220
EP 1224
DI 10.1130/G49007.1
ID 81425
ER

EF