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Marine Ecosystems Research Department - jamstec japan agency ...

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JAMSTEC 2002 Annual Report<br />

Frontier <strong>Research</strong> System for Global Change<br />

tend to increase on the warmer flank of major ocean<br />

fronts and decrease on the colder flank (Figure ).<br />

b. Theme : Regional Ocean Influences<br />

<strong>Research</strong> projects under Theme were conducted to<br />

do the following: understand Kuroshio-path dynamics;<br />

analyze mean states and mesoscale variability of the<br />

Kuroshio-Oyashio system (KOS) by using satellite<br />

altimeter, drifters, historical data, and an eddy-resolving<br />

model; model pathways between subtropical and subpolar<br />

gyres; improve and apply data-assimilation schemes<br />

for analyzing the KOS and mode waters; describe<br />

detailed circulations of the North and South Pacific lowlatitude<br />

boundary currents (LLWBCs) by using historical,<br />

existing, and model data; simulate LLWBCs and<br />

their climatic variability; study regional circulation and<br />

variability of the Indonesian Throughflow with a focus<br />

on variations in its vertical structure; and capture the<br />

oceanic response in the eastern Indian Ocean to active<br />

and break periods during the monsoon onset. Other studies<br />

included the influence of ocean stirring and mixing<br />

caused by eddying flows on the marine ecosystem; the<br />

damping of TIWs through negative atmospheric feedback;<br />

the monsoon's effect on the partitioning of North<br />

Equatorial Current transport into the Mindanao Current<br />

and Kuroshio and on the water-mass distribution<br />

between the tropical and subtropical North Pacific.<br />

Theme- researchers have also been closely<br />

involved in the establishment of the Asia-Pacific Data-<br />

<strong>Research</strong> Center (APDRC).<br />

c. Theme : Asian-Australian Monsoon System<br />

Theme- researchers investigated the following<br />

areas: the nonlinearity of El Niño and La Niña; the<br />

effect of thermocline and ocean-zonal-advective feedback<br />

on the time scales of various Pacific coupled<br />

modes; the impact of the late 's basic-state shift in<br />

the Pacific Ocean on different components of the<br />

40N<br />

Sea Surface Temperature<br />

(a) 1998<br />

(b) 2001<br />

35N<br />

140E<br />

30N<br />

130E<br />

140E<br />

130E<br />

30N<br />

130E 140E 130E<br />

140E<br />

15<br />

18 21 24 ˚C<br />

Surface Winds<br />

40N<br />

(c) 1998<br />

(d) 2001<br />

35N<br />

5 6 7 8 9 m / s<br />

Fig.23 April to June mean fields in SST and surface wind speed for 1998 (panels a and c) and for<br />

2001 (panels b and d) based on TRMM Microwave Imager data sets. The shift between<br />

Kuroshio's straight (panel a) and meandering path (panel b) is accompanied by large differences<br />

in SST. The high wind speed over the straight warm SST path is markedly reduced<br />

when the warm water is replaced by cool water in the meandering path.<br />

142

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