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Marine Ecosystems Research Department - jamstec japan agency ...

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Japan <strong>Marine</strong> Science and Technology Center<br />

Ocean Observation and <strong>Research</strong> <strong>Department</strong><br />

Unions, and the Intergovernmental Oceanographic<br />

Commission of UNESCO. The TRITON project<br />

is the CLIVAR observing system, and also contributes<br />

to the Global Ocean Observing System<br />

(GOOS) and Global Climate Observing System<br />

(GCOS). We also collaborate with the Agency for the<br />

Assessment and Application of Technology (BPPT),<br />

Indonesia, and the National Institute of Oceanography<br />

(NIO), India.<br />

JAMSTEC started the deployment at four TRITON<br />

sites along E by R/V Mirai in March . The<br />

originally planned TRITON array of sites in the<br />

Pacific and Indian Oceans was completed in August<br />

(Photo , Fig. ). The TRITON data combined<br />

with TAO data are distributed through GTS (Global<br />

Telecommunication System) and from the TRITON<br />

web page at JAMSTEC (http://www.<strong>jamstec</strong>.go.jp/<strong>jamstec</strong>/TRITON/)<br />

and the TAO web page at PMEL<br />

(http://www.pmel.noaa.gov/tao/).<br />

TAO/TRITON data have been used widely for monitoring<br />

the evolution of the - El Niño event<br />

as shown in Fig. and for initializing ENSO forecast<br />

models at operational weather and climate centers<br />

around the world. Warm water accumulated in the<br />

Photo 1 Scientists, marine technicians and crew on R/V Mirai celebrate<br />

the completion of originally planed TRITON array<br />

(August, 2002).<br />

Fig. 2 TRITON array as of August 2002.<br />

Five Day Zonal Wind, SST, and 20˚C Isotherm Depth Anomalies 2˚S to 2˚N Average<br />

Zonal Wind (m s -1 ) SST (˚C) 20˚C Isotherm Depth (m)<br />

2003 2002<br />

2001<br />

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140˚E 180˚ 140˚W 100˚W 140˚E 180˚ 140˚W 100˚W 140˚E 180˚ 140˚W 100˚W<br />

-8 -4 0 4 8 -3 -2 -1 0 1 2 3<br />

-80 -40 0 40 80<br />

TAO Project Office /PMEL/NOAA Jun 12 2003<br />

Fig. 3 Anomalies of zonal surface wind, sea surface temperature, and 20C isotherm depth along the equator.<br />

35

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