| Special Topic: Kuroshio |
Okinawa is Sandwiched
by Two Currents
- Confirmed by long-term mooring observations southeast
of Okinawa Island - |
 |
As a possible "branch current" of the Kuroshio,
new current system is found southeast of Okinawa Island. We
are pleased to introduce the project by JCOPE group of Climate
Variations Observational Program. |
|
Frontier Observational Research
System for Global Change (FORSGC)
Climate Variations Observational Research Program
Drs.Kaoru Ichikawa,Hiroshi Ichikawa,Xia Hua Zhu |
Missing Volume Transport of the Kuroshio
The Kuroshio, one of the strongest current in the world, flows in
the East China Sea and south of the Japanese main island. Because
large amount of warm water is carried from the tropics, the Kuroshio
has great impacts on climate changes in a wide area including Japan.
In addition, the Kuroshio strongly affects efficiency of maritime
transports and fisheries.
Although its existence has long been recognized, detailed quantitative
measurements of the Kuroshio volume transport (the amount of sea
water carried by the Kuroshio) have started only 10-20 years before.
The results revealed that the Kuroshio volume transport in the downstream
(south of Japan) is twice larger than that in the upstream (East
China Sea). Analogizing rivers, this suggests existence of a "branch
current" which merges into the Kuroshio south of Japan. Recently,
a northeastward subsurface current was found southeast of Amami-Ohshima
Island by mooring observations, so the "branch current"
is expected to flow northward east of the Nansei islands. High-resolution
numerical models also support this idea.
Northeastward Current Southeast of Okinawa Island
However, existence of a northeastward current was not certain in
the southeast of Okinawa Island, the upstream of Amami-Ohshima Island.
Plenty of meso-scale eddies that are slowly propagated from the
east in the Pacific cause high temporal variability in the east
of the Nansei islands, which prevents us from obtaining mean velocity
field without long-term observations.
The Japanese Coastal Ocean Predictability Experiment Group (JCOPE;
Climate Variations Observational Research Program, Frontier Observational
Research System for Global Change), therefore, started long-term
observations deploying many Inverted Echo Sounder with Pressure
gauge (PIES)*1 and Moored Acoustic Doppler Current Profiler
(MADCP)*2 mooring systems southeast of Okinawa Island
(Figs. 1 and 2). Based on nine-month records of the mooring observations
from November 2000 to September 2001, a time series of the volume
transport across the observation line southeast of Okinawa Island
(indicated by a broken line in Fig. 1) is obtained (Fig. 3). As
expected from active meso-scale eddies, its temporal variability
is found very high; the volume transport was sometimes southwestward,
but turned to northwestward only a few month later, reaching to
20.8 million m3/s.
Removing these variations by averaging over a long period, the temporal
mean current is first obtained southeast of Okinawa Island, manifesting
northeastward 6.1 million m3/s volume transport. This
corresponds to carry 5 cups of Tokyo Dome Stadium of sea water northeastward
in every second. In other words, there would exist 10,000 of the
Shinano Rivers, the largest river in Japan.
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Fig. 1 Mooring stations southeast of Okinawa Island. |

| Fig. 2 |
Schematic diagram explaining PIES and MADCP observations.
In the analysis, ship and satellite data are associated. |
|
| Fig. 3 |
Time series of the volume transport across the observation
line, based on the moored PIES and MADCP data. |
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Revealing the Current System East of Nansei
Islands
Large amount of sea water is confirmed to be carried northeastward
in the southeast of Okinawa Island, as well as Amami-Ohshima Island.
The obtained mean volume transport (6.1 million m3/s) accounts for
a quarter of the Kuroshio volume transport in the East China Sea,
so that the observation line is considered to have captured a part
of the current that merges into the Kuroshio south of Japan.
In order to investigate connection of the current to the Kuroshio
east of Taiwan, the JCOPE Group deployed mooring observation systems
southeast of Miyako Island, the further upstream of Okinawa Island,
in December, 2002 (Fig. 4). In addition, to study seasonal and interannual
changes of the current and to obtain offshore velocity field and
precise vertical velocity profiles, many observations are being
conducted cooperating with other institutes such as Nagasaki Marine
Observatory, Nagasaki University and Kagoshima University.
In near future, the entire current system east of the Nansei islands
would be described more precisely. This should greatly help us to
trace paths of the warm water and materials carried by the Kuroshio,
which would eventually aid to estimate climate changes and to increase
efficiency in maritime transport and fisheries.
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| Fig. 4 |
Schematic diagram of the Kuroshio (blue arrow) and the possible
northeastward current east of the Nansei islands (yellow arrow).
Many researchers have suggested existence of the latter. In
this region, however, the mean current is difficult to be obtained
due to high temporal variability caused by meso-scale eddies. |
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| *1 |
PIES is an echo sounder moored at the bottom and transmits
sound pulses upward. It measures travel time of a sound pulse
reflected from the sea surface. Since speed of the sound strongly
depends on water temperature, vertical temperature profile can
be estimated from the measured travel time. The PIES is a very
handy instrument easily deployed and recovered. |
| *2 |
MADCP is an ADCP instrument designed to measure vertical
velocity profile in a long-term mooring system. The ADCP measures
drifting velocity of small particles (e.g. planktons) in the
sea water, using the Doppler frequency shift. Because the swimming
velocity of planktons is negligible with respect to the velocity
of the sea water, the obtained drifting velocity of small particles
represents the current velocity. |
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