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NWP1 individuals are assumed to spawn at the front 19-21°C 19-21°Cen the cold southward flowing North China Coastal Current and a warm betweenof the northward flowing Kuroshio coldent, with the front southwardaccording to the strength oflowingorth ChiNorthastal Chinant [ 20, 59, 60].
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Branches of warm Atlantic currents push floating ice northward.
The warm Tsushima Current, a branch of the Kuroshio (Japan Current), passes north through the strait.
The closure of the Japan Sea caused fluctuations in sea temperatures, by halting the influx of the warm Tsushima Current, a branch of the Kuroshio Current that supplies a large amount of heat to northern areas [ 9].
A 60-foot tree had toppled away from his house, toward a neighbor's, and he was out sawing branches, keeping warm before heading back into a dark, cold house.
Indeed, there are more attorneys keeping seats warm in the three branches of the federal government than any other profession.
Entering the Sea of Japan through the Korea Strait, the Tsushima Current issues the East Korea Warm Current as a northern branch.
Irminger Current, branch of the warm North Atlantic Current, flowing generally westward along the south coast of Iceland.
The winds influence the water circulation of the Kuroshio (Japan Current), a northward-flowing branch of the warm North Equatorial Current that flows near Taiwan.
A branch of the warm North Atlantic Drift, however, moderates the climate and leaves an open passage that permits vessels to approach the western coasts during most months.
Note the large depolarization (warm color) at the main branch point ('hot spot' zone) in CA2 model.
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