Where is sulu sea located

One of the most interesting features of the Sulu Sea is the presence of various geographic structures including coral atolls and reefs. Most significant among these naturally formed structures is the Tubbataha Reef which is home to the Tubbataha Reefs Natural Park. Many years later in , the physical boundaries of the park were extended to cover about three times as much area as what was originally designated for the park.

Tubbataha Reefs Natural Park includes both a bird as well as a marine sanctuary which are located on two large atolls. The park is also a popular nesting site for local species of turtles and birds such as terns.

Other marine animals found at the park include hammerhead sharks, manta rays, clownfish, barracudas, giant kingfish, and moray eels. The Sulu Sea is well known for the important role it plays in terms of facilitating commerce and trading between the various local island communities.

The fishing industry is also a key element in the economic survival of an array of communities living in this part of the world. Other naturally sourced products found in the Sulu Sea include turtle eggs, shark fins, pearls, and sea cucumbers. Each year the lure of taking part in a unique one of a kind recreational activities attracts tourists from all over the globe to the Sulu Sea. Diving is especially popular in areas in which coral reefs are abundant.

The harder to reach areas of this body of water are accessible by boat only during the months of March until June.

The Sulu Sea, located between Borneo and the Philippines, is separated from the surrounding ocean by two chains of islands. There are no passages below m depth and the basin, which at the deepest is 5,m, is filled with warm low oxygen water. The near surface chlorophyll concentration has been examined with the aid of ocean colour sensors on board satellites. Direct comparisons between a field observation of chlorophyll and its remotely sensed values from OCTS Ocean Colour Temperature Scanner are found to be in satisfactory agreement.

An 8-month time series of chlorophyll near the centre of the Sulu Sea has been used to show that the chlorophyll level is significantly higher than the level in the adjacent South China Sea. This was most pronounced at the period of change between the monsoons. The greater primary productivity may provide the explanation for the higher deposition rate of carbon in the Sulu Sea.

Although the Sulu Sea is more productive than the adjacent South China Sea, the central area can still be classified as a desert. Estimates of the new primary production in the central Sulu Sea seem to be just sufficient to support the current fishery.

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