FN Archimer Export Format
PT J
TI Quaternary rainfall variability is governed by insolation in northern China and ice-sheet forcing in the South
BT 
AF Zhao, Debo
   Lu, Zhengyao
   Wan, Shiming
   Cheng, Hai
   Shi, Xuefa
   Li, Anchun
AS 1:1;2:2;3:1,3,4;4:5;5:6;6:1;
FF 1:;2:;3:;4:;5:;6:;
C1 Key Laboratory of Marine Geology and Environment, Institute of Oceanology, Chinese Academy of Sciences, Qingdao, 266071, China
   Department of Physical Geography and Ecosystem Science, Lund University, Sölvegatan 12, 22362, Lund, Sweden
   Laboratory for Marine Geology, Qingdao National Laboratory for Marine Science and Technology, Qingdao, 266061, China
   CAS Center for Excellence in Quaternary Science and Global Change, Xi’an, 710061, China
   Institute of Global Environmental Change, Xi’an Jiaotong University, Xi’an, 710054, China
   Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, Ministry of Natural Resources, Qingdao, 266061, China
C2 CHINESE ACAD SCI, CHINA
   UNIV LUND, SWEDEN
   QNLM, CHINA
   CHINESE ACAD SCI, CHINA
   UNIV XI AN JIAO TONG, CHINA
   FIO, CHINA
IN DOAJ
IF 7.9
TC 3
UR https://archimer.ifremer.fr/doc/00814/92588/98873.pdf
   https://archimer.ifremer.fr/doc/00814/92588/98874.pdf
   https://archimer.ifremer.fr/doc/00814/92588/98875.pdf
LA English
DT Article
CR IMAGES 4-MD111
BO Marion Dufresne
AB Quaternary Asian low-latitude hydroclimate cyclicity has long been attributed to insolation forcing, in contrast to the dominant ice-sheet and CO2 controls identified in mid-high-latitude regions. However, debates exist regarding these rainfall variations and forcings due to inconsistent reconstructions and simulations. Here, by combining rainfall proxy records with multi-model simulations, dominant 23 ka rainfall cycle in northern China and 100 ka rainfall cycle in southern China and Southeast Asia were found. We propose that rainfall mainly occurs in summer in the north, primarily driven by insolation. Rainfall in the south is largely forced by high-latitude ice sheets, with enhanced spring and autumn rainfall in southern China and weakened rainfall in western Maritime Continent during glacial periods. This study highlights the seasonal contributions to orbital-scale rainfall changes, and sheds light on the Asian hydroclimate conditions associated with high-low-latitude climate interactions. 
PY 2023
PD JAN
SO Communications Earth & Environment
SN 2662-4435
PU Springer Science and Business Media LLC
VL 4
IS 1
UT 000908702800002
DI 10.1038/s43247-022-00670-9
ID 92588
ER

EF