HIGHLIGHTS
SUMMARY
| 1 Vol.:(0123456789) Northwestern North Pacific subtropical gyre Kuroshio Extension Kuroshio STMW 25N 20N 125E temperature is determined by a combination of sea surface c ooling12 and entrainment of low-level cold water into the ML in association with ML d eepening16 in the cold season. The influence of warm-season atmospheric forcing on the Kuroshio and on STMW has also been examined. Akitomo et_al17 implied influences of warm-season atmospheric forcing on Kuroshio transport by showing that the Kuroshio transport fluctuates in response to annual-mean WSC variations over the North Pacific. The . . .
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