|
This eco-region comprises the Chinese waters of
the Yellow Sea; North and South Korea; Japan,
north from the southernmost tip of Kyushu and
the Sea of Japan; Russia from the border with
North Korea north to the mouth of the Tumnin River;
the southern part of Sakhalin Island from Makaro
and Saritsa south.
The Yellow (Huanghai) Sea is a partially enclosed
body of water bounded by the Chinese mainland to the
west, the Korean Peninsula to the east, and a line
running from the north bank of the mouth of the Yangtze
River to the south side of Cheju Island. It is a shallow
sea with an average depth in the region of 44 metres,
sloping gently away from the Chinese coastline.
The Yellow River and the Yangtze have both formed
large deltas and deposit large amounts of sediment
into the sea. These deposits are mineral rich and
give the waters a yellow hue, hence the name. This
highly productive Sea is marked by seasonal variation,
and supports substantial populations of both cold
temperate (eel-pout, cod, flatfish, Pacific herring)
and warm water (skates, gurnard, jewfish, small yellow
croaker, spotted sardine, fleshy prawn, southern rough
shrimp) species.
There are eleven species of mammals including fin-less
porpoise, seals, and sea cow lions. Some whale species
may also be spotted here, although these are just
remnants of the the pods that used to migrate and
breed there.
The Yellow Sea is one of the most intensively exploited
areas in the world. There are over 270 fish species,
with about 100 species of fish and crustacea being
commercially harvested. This exploitation of the Seašs
resources means that over time, stocks some of the
more commercially valuable species have declined,
to be replaced by smaller, less valuable species.
The Sea of Japan (also known as the East Sea)
is another highly productive, semi-enclosed sea, connected
to the Sea of Okhotsk, the Northern Pacific Ocean
and the East China Sea through four shallow straits.
The shallowness of these straits limits the water
flow in and out of the Sea and contributes its semi-enclosed
character.
The Tsushima Current, a small branch of the
warm Kuroshio Current, enters the Sea of Japan through
the Tsushima Strait between Kyushu and Korea and flows
out to the Pacific through the Tsugaru and Soya Straits.
The average depth of the sea is 1350 metres. The northwestern
area of the Sea is colder than the remaining southerly
part, with sharp declines in temperature in the winter
and ice forming in the Tartarskiy Strait from November
to April. Seasonal temperature fluctuations are as
high as 20 degrees C in the northwestern portion,
and 14 degrees C in the southern portion, allowing
the region to support tropical to Arctic species.
Commercially important species include sardine, flounder,
Pacific cod, Pacific salmon, red sea bream, with the
Japanese sardine (Sardinops melanostica), one
of the most abundant pelagic fish in the Sea of Japan,
contributing more than 70 percent of the total catch.
The country that is Japan is actually an archipelago
that stretches over 3000 kilometres from north to
south. Because of this, northern Japan is located
in the North Temperate Zone, experiencing temperatures
that range from cool to cold, while the southern Japanese
islands, (outside this eco-region) are situated near
the Tropic of Cancer and enjoy tropical temperatures.
Summers are humid and hot, whilst areas impacted by
the Asian monsoons suffer severe weather, despite
the temperate latitude.
Most areas of Japan have a rainy season, known as
tsuyu, sometime during June and July, with occasional
typhoons, from August to October, bringing heavy rains
and high winds to some parts of the region. High levels
of land reclamation and coastal development has led
to the destruction of mangrove areas and harmed extensive
areas of coral reef in the south of Japan. Oil pollution
is a significant problem along major shipping routes
and an increasing number of accidents have occurred
in recent years.
The former Soviet Union and now Russia have reportedly
dumped radioactive waste in the Sea of Japan.
|