FN Archimer Export Format
PT J
TI Equatorward shift of the subarctic boundary in the northwestern Pacific during the last deglaciation
BT 
AF YAMAMOTO, M
   SUEMUNE, R
   OBA, T
AS 1:1;2:1;3:1;
FF 1:;2:;3:;
C1 Hokkaido Univ, Grad Sch Environm Earth Sci, Kita Ku, Sapporo, Hokkaido 0600810, Japan.
C2 UNIV HOKKAIDO, JAPAN
IF 2.491
TC 47
UR https://archimer.ifremer.fr/doc/00230/34087/32518.pdf
LA English
DT Article
CR MD 122 / WEPAMA
BO Marion Dufresne
AB We have generated a high-resolution record of alkenone sea surface temperature (SST) between 10-24 ka from Core MD01-2421 off central Japan, in the northwestern Pacific. The cooling by 5 degrees C from 21 ka to 12.8 ka implies the equatorward shift of the subarctic boundary in the northwestern Pacific by similar to 2.8 degrees in latitude. This shift was a result of the stronger summer Okhotsk High. The Okhotsk High was likely enhanced by the combined effects of El Nino-like conditions in the tropical Pacific and the heating of the land surface of northeastern Siberia.
PY 2005
PD MAR
SO Geophysical Research Letters
SN 0094-8276
PU Amer Geophysical Union
VL 32
IS L05609
UT 000227640800004
BP 1
EP 4
DI 10.1029/2004GL021903
ID 34087
ER

EF