ECS 100M LAN DRIVER DETAILS:
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ECS 100M LAN DRIVER
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Introduction Geographically there are four seas lying ecs 100m lan to the Chinese Continent Fig. The average depth of the Bohai Sea is only 18 m and that of the Yellow Sea 44 m.
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A shallow trough runs through the gulf and can be traced down south to the northern end of the Okinawa Trough in the ECS. There are three deep depressions along ecs 100m lan Ryukyu Ridge. Ecs 100m lan northernmost one is the Tokara Strait with a maximum depth of less than m and the southernmost one is next to the east coast of Taiwan with a trough around m deep. The middle one lies below the Okinawa Island and has a valley over m deep.
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Changjiang, the third largest river in the world, enters the ECS near Shanghai. The SCS is almost three times as large as the other three seas combined. It also has a large abyssal basin with a maximum depth over m. Except for the Bashi Channel, however, its connection to other water bodies are limited by shelves shallower than m. The sill depth in the Bashi Channel is about m, which limits the penetration of the deep water from ecs 100m lan Pacific Ocean into the SCS.
Although these four seas are named geographically, they also have distinct circulation features. Knowledge of these features are inferred principally from extensive hydrographic observations and from numerical modeling results, both process oriented simple models and fully three-dimensional models. There were ecs 100m lan limited long-term moored current meter measurements conducted in these seas.
Except for the classical study of Wyrtki circulation in the rest part of the SCS have been hardly studied because of lack of observations and hence will not be reviewed here. Relevant ecs 100m lan on the circulation dynamics of the China Seas can also be found in Su et al.
For the convenience of the following discussions Fig. It is seen that the Kuroshio flows north along the east coast of Luzon, passes by the Bashi Channel ecs 100m lan enters the ECS ecs 100m lan moving northeastward along the east coast of Taiwan. The Kuroshio plays an important role of open ocean forcing in the circulation dynamics of the China Seas. Here by the Kuroshio we mean both its current structure and hydrography and also the part of the large-scale pressure field of the subtropic gyre associated with the Kuroshio.
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Another important open ocean driving force is the pressure difference across the Japan Sea ecs 100m lan the pressure field of the subtropic gyre near the Korea Strait and that of the subpolar gyre near the Tsugara Strait. In the following we will regard TC as a driving force external to the China Seas in the above sense.
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The strong northerly winds accompanying the surge of cold, dry continental air tend to homogenize vertically most of the BYS. The bursts of winds excite subtidal sea-level fluctuations which propagate southward along the west coast of the Yellow Sea all the way down to the SCS Chen and Su, Similar subtidal sea-level fluctuations also propagate northward along the east coast of the Yellow Sea Hsueh and Romea,although there does not seem to be similar propagations in the Bohai Sea Chen and Su, There was also evidence that the whole Ecs 100m lan may be excited into a pumping mode with a period of about two days Chen and Su, Noting the semi-enclosed nature of the BYS Yuan et al. As expected, the model also yields southward coastal currents on both sides of the Yellow Sea.
Time-dependent barotropic model Hsueh et al. The same conclusion is ecs 100m lan obtained when lateral density gradient is introduced Liu and Su, Moored current meter measurements in Yellow Sea under wintertime winds showed that coastal currents west of Korea are mostly downwind to the south, while in the trough strong upwind flows are found to follow closely the surges of the northerly winds Hsueh, Normally they are limited to areas with water depth less than 10 m. However, there were also records ecs 100m lan the Bohai Sea was almost fully covered by sea ice op.