FN Archimer Export Format
PT J
TI Millennial meridional dynamics of the Indo-Pacific Warm Pool during the last termination
BT 
AF LO, L.
   SHEN, C. -C.
   WEI, K. -Y.
   BURR, G. S.
   MII, H. -S.
   CHEN, M. -T.
   LEE, S. -Y.
   TSAI, M. -C.
AS 1:1;2:1;3:1;4:1,2;5:3;6:4;7:5;8:1;
FF 1:;2:;3:;4:;5:;6:;7:;8:;
C1 Natl Taiwan Univ, Dept Geosci, High Precis Mass Spectrometry & Environm Change L, Taipei 10617, Taiwan.
   Univ Arizona, Dept Phys, NSF Arizona Accelerator Mass Spectrometry Facil, Tucson, AZ 85721 USA.
   Natl Taiwan Normal Univ, Dept Earth Sci, Taipei 11677, Taiwan.
   Natl Taiwan Ocean Univ, Inst Appl Geosci, Keelung 20224, Taiwan.
   Acad Sinica, Res Ctr Environm Changes, Taipei 11529, Taiwan.
C2 UNIV NATL TAIWAN, TAIWAN
   UNIV ARIZONA, USA
   UNIV NATL TAIWAN NORMAL, TAIWAN
   UNIV NATL TAIWAN OCEAN, TAIWAN
   ACAD SINICA, TAIWAN
IF 3.382
TC 13
UR https://archimer.ifremer.fr/doc/00291/40206/38994.pdf
   https://archimer.ifremer.fr/doc/00291/40206/71309.pdf
LA English
DT Article
CR IMAGES 3-IPHIS-MD106
   IMAGES 4-MD111
   MD 122 / WEPAMA
   MD 148 / PECTEN
   MD 155 / MARCO-POLO2
BO Marion Dufresne
AB To develop an in-depth understanding of the natural dynamics of the Indo-Pacific Warm Pool (IPWP) during the last deglaciation, stacked north-(N-) and south-IPWP (S-IPWP) thermal and hydrological records over the past 23-10.5 ka were built using planktonic foraminiferal geochemistry data from a new core, MD05-2925 (9.3 degrees S, 151.5 degrees E, water depth 1661 m) in the Solomon Sea and eleven previous sites. Ice-volume-corrected seawater delta O-18 (delta O-18(SW-IVC)) stacks show that S-IPWP delta O-18(SW-IVC) values are indistinguishable from their northern counterparts through glacial time. The N-IPWP SST (sea surface temperature) stacked record features an increasing trend of 0.5 degrees C ka(-1) since 18 ka. Its S-IPWP counterpart shows an earlier onset of temperature increase at 19 ka and a strong teleconnection to high-latitude climate in the Southern Hemisphere. Meridional SST gradients between the N- and S-IPWP were 1-1.5 degrees C during the Bolling/Allerod period and 1 degrees C during both Heinrich event 1 and the Younger Dryas, due to a warmer S-IPWP. A warm S-IPWP during the cold events could weaken the southern hemispheric branch of the Hadley cell and reduce precipitation in the Asian monsoon region.
PY 2014
PD DEC
SO Climate Of The Past
SN 1814-9324
PU Copernicus Gesellschaft Mbh
VL 10
IS 6
UT 000347569500017
BP 2253
EP 2261
DI 10.5194/cp-10-2253-2014
ID 40206
ER

EF