FN Archimer Export Format
PT J
TI Central Mediterranean rainfall varied with high northern latitude temperatures during the last deglaciation
BT 
AF Columbu, Andrea
   Spötl, Christoph
   Fohlmeister, Jens
   Hu, Hsun-Ming
   Chiarini, Veronica
   Hellstrom, John
   Cheng, Hai
   Shen, Chuan-Chou
   De Waele, Jo
AS 1:1,2;2:3;3:4;4:5,6;5:7;6:8;7:9;8:5,6;9:7;
FF 1:;2:;3:;4:;5:;6:;7:;8:;9:;
C1 Department of Chemistry, Life Sciences and Environmental Sustainability. Earth Sciences Division, University of Parma, Parma, Italy
   Department of Earth Sciences, University of Pisa, Pisa, Italy
   Institute of Geology, University of Innsbruck, Innsbruck, Austria
   German Federal Office for Radiation Protection (BfS), Berlin, Germany
   High-Precision Mass Spectrometry and Environment Change Laboratory (HISPEC), Department of Geosciences, National Taiwan University, Taipei, Taiwan ROC
   Research Center for Future Earth, National Taiwan University, Taipei, Taiwan ROC
   Department of Biological, Geological and Environmental Sciences, University of Bologna, Bologna, Italy
   School of Earth Sciences, University of Melbourne, Melbourne, Australia
   Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an, China
C2 UNIV PARMA, ITALY
   UNIV PISA, ITALY
   UNIV INNSBRUCK, AUSTRIA
   BFS, GERMANY
   UNIV NATL TAIWAN, TAIWAN
   UNIV NATL TAIWANH, TAIWAN
   UNIV BOLOGNA, ITALY
   UNIV MELBOURNE, AUSTRALIA
   UNIV XI AN JIAO TONG, CHINA
IN DOAJ
IF 7.9
TC 6
UR https://archimer.ifremer.fr/doc/00789/90049/95640.pdf
   https://archimer.ifremer.fr/doc/00789/90049/95641.pdf
   https://archimer.ifremer.fr/doc/00789/90049/95642.pdf
   https://archimer.ifremer.fr/doc/00789/90049/95643.xlsx
   https://archimer.ifremer.fr/doc/00789/90049/95644.xlsx
LA English
DT Article
CR IMAGES 1-MD101
BO Marion Dufresne
AB Similarly to the effects of current climate change, the last deglaciation (Termination I) rapidly altered northern latitude temperatures and ice-sheet extent, as well as the Atlantic Meridional Overturning Circulation. However, it is still unclear how these changes propagated and impacted the central Mediterranean continental rainfall variability. This prevents a full understanding on how global warming will affect Mediterranean areas in the future. Here, we present a high-resolution reconstruction of rainfall changes in the central Mediterranean across Termination I, based on a novel δ18O time series from a southern Italian stalagmite. Across Termination I the availability of Atlantic moisture varied in response to northern latitude temperature increases (decreases) and ice-sheet decreases (increases), promoting a higher (lower) intensity of the Atlantic Meridional Overturning Circulation, and resulting in a relatively wetter (drier) climate in the Mediterranean. In the light of future warming, this study emphasises the role of high-latitude climate changes in causing rainfall variation in highly populated Mediterranean areas. 
PY 2022
PD AUG
SO Communications Earth & Environment
SN 2662-4435
PU Springer Science and Business Media LLC
VL 3
IS 1
UT 000842208100001
DI 10.1038/s43247-022-00509-3
ID 90049
ER

EF