FN Archimer Export Format
PT J
TI Comment on "Asynchronous variation in the East Asian winter monsoon during the Holocene" by Xiaojian Zhang, Liya Jin, and Na Li
BT 
AF RASHID, Harunur
   MARCHE, Brittany
   VERMOOTEN, Marli
   PARRY, Devon
   WEBB, Michaela
   BROCKWAY, Brent
   LANGER, Keesha
AS 1:1;2:1;3:1;4:1;5:1;6:1;7:1;
FF 1:;2:;3:;4:;5:;6:;7:;
C1 Mem Univ Newfoundland, Earth & Environm Sci, Corner Brook, NF, Canada.
C2 UNIV NEWFOUNDLAND, CANADA
IF 3.454
TC 2
UR https://archimer.ifremer.fr/doc/00421/53265/54673.pdf
LA English
DT Article
CR IMAGES V LEG 1-MD114
   IMAGES V LEG 4-MD114
   OSIRIS 3 - MD 13
BO Marion Dufresne
DE ;East Asian winter monsoon;Holocene;subpolar North Atlantic Ocean;eastern tropical Indian Ocean
AB Comparing paleoproxy records throughout China and two climate models simulation results, Zhang et al. (2015) reported asynchronous Holocene spatiotemporal decline of the East Asian winter monsoon. Six sea surface temperature (SST) proxy records from the Atlantic Ocean and northern Indian Ocean and South China Sea were used to validate climate simulations results. However, the referred Mg/Ca SST record from the western Atlantic Ocean is simply nonexistent and the northeast Atlantic Mg/Ca SST data do not reflect winter SST as Zhang et al. (2015) argued to support the driving mechanisms. Furthermore, the western Indian Ocean SSTs data used in Zhang et al. (2015) do not reflect the winter SSTs or regional changes in the Holocene SSTs. Therefore, we question the validity of model simulation results and hence the reliability of conclusions in Zhang et al. (2015). 
PY 2016
PD FEB
SO Journal Of Geophysical Research-atmospheres
SN 2169-897X
PU Amer Geophysical Union
VL 121
IS 4
UT 000372977900014
BP 1611
EP 1614
DI 10.1002/2015JD023983
ID 53265
ER

EF