In which hemisphere is the Arabian Sea. Arabian Sea

The Arabian Sea is located between the Arabian and Hindustan peninsulas. Its area is 3683 thousand km2 and most of the sea is one of the oceanic trenches Indian Ocean... Therefore, the Arabian Sea is very deep, its average depth is 2734 m, and the maximum is 5203 m. The Arabian Sea has large bays - the Aden, which connects the Arabian and Red Seas, the Gulf of Oman through the strait and the Persian Gulf connected with it by the Strait of Hormuz. Fishing is developed in the Arabian Sea - there are more than 100 species of commercial fish, including sardines, tuna, marlin, sailfish, mackerel.

Fishing for shrimp, crab and lobster is important. Several shark species are found in the local waters, including the mako, black fin shark, tiger, blue and blunt sharks. Even swimming in shallow waters, these sharks, as a rule, do not attack people, on the contrary, when they meet a person, they try to retreat faster. People here are much more dangerous for sharks, because for the sake of edible fins that are exported, sharks in the Arabian Sea are hunted in huge quantities.

Fans of sport fishing or scuba diving are familiar with another inhabitant of local waters - a giant grouper from the serran family. This huge (2.5 m, 400 kg) fish lives in warm coastal waters and leads a solitary life, hunting lobsters, crabs, rays, young turtles and various fish. Groupers stick to their territory, which necessarily has some kind of cave or crevice large enough for the grouper to take refuge there to rest. Adult groupers, due to their impressive size, do not have enemies in nature, so they are clumsy and slow. It is the unhurriedness of the grouper that makes it such a desirable prey for amateur fishermen, and divers love to swim next to the good-natured giant. True, as with any wild animal, you need to be on the lookout with a grouper - there have been cases when these fish attacked scuba divers and inflicted serious and even fatal wounds.

A unique representative of the herring family, the dorab, lives in the Arabian Sea. This largest of all herrings (1 m, 4 kg) does not form large shoals like other herring, but occurs singly or in small groups. Dorabov is also called a toothed herring or wolf herring for two large, protruding upper teeth, resembling wolf fangs. Such teeth give out an active predator in the fish - and indeed, unlike most herring that feed on plankton, the fish prey on fish and crustaceans. Dorab is a fairly common fish, and its meat tastes great, so locals they often bring wolves to their table.

Sandy coast of the Arabian Sea

The Arabian Sea is located in the northwestern part of the Indian Ocean. It occupies the Arabian Basin, clearly distinguished by the outlines of the coast and the bottom relief. In the west, the borders of the sea are the shores of the Somali and Arabian peninsulas, in the north and northeast - the shores of the Indian subcontinent. The eastern border stands out along the Maldives ridge, almost all the peaks of which protrude above the water, forming islands. The Arabian-Indian ridge separating the sea from the rest of the ocean is taken as the southern border of the sea.

The depths above the ridge tops are 1500-2000 m, and the depth of its rift gorges is 3000-4000 m, in some places it increases to 5000 m.

Sea area - 4221 thousand km 2, volume - 14 005 thousand km 3 (excluding the bays of Aden, Oman and Persian, the area of ​​which is 611 thousand km 2, volume - 518 thousand km 3), average depth - 3006 m , maximum depth - 5803 m.

Indian Ocean

Climate

The main features of the climate of the Arabian Sea are determined by the characteristics of its geographic location... Atmospheric circulation is of a well-pronounced monsoon character; differences in seasons in the northern part are very pronounced.

The northeastern (winter) monsoon sets in November and lasts until March. Over the extreme northern regions of the Arabian Sea, the circulation of the northeastern monsoon is sometimes disturbed by the passage of the so-called western disturbances. At the same time, northwestern and western air flows prevail, the wind speed increases to 8-10 m / s, while in the field of an undisturbed monsoon flow, it is on average 3-7 m / s.

In summer, the circulation of the southwest monsoon dominates the Arabian Sea. From June to August, it accounts for 90-100% of all winds. The summer monsoon in this area in terms of calendar dates, intensity of manifestation, distribution in space is an extremely stable system, where wind speeds reach 15-20 m / s. The strongest winds are observed in the central and western parts of the sea, in the eastern - the speed is lower - 5-10 m / s. The short transitional seasons of the year (April and October) are distinguished by the greatest variety of synoptic conditions. During these months, the most characteristic atmospheric process is the passage of tropical disturbances over the Arabian Sea, the trajectories of which have a well-pronounced meridional component. This type of circulation is most often observed in the fall. In the spring, when it starts to warm up, shallow thermal depressions appear over Hindustan, causing the winds of the northern points. During the transitional months, especially in spring, baric fields are often formed over the northern part of the Indian Ocean, which determine weak winds (3-4 m / s) of variable directions.

The Arabian Sea, which is almost entirely located in the tropical zone, is characterized by high air temperatures: 22-26 ° in winter, 26-30 ° in summer, intense evaporation from its surface (1500-1750 mm per year in most of the water area and up to 2000 mm per year off the coast of the Somali Peninsula).

Precipitation generally falls very little - from 25 to 125 mm per year, but off the coast of the Indian subcontinent, their amount increases to 3000 mm per year.

The main feature of the climatic conditions associated with monsoons is the seasonal variability of meteorological characteristics, and, first of all, a sharp change in wind fields, which causes a response from the sea. The swell during the northeastern monsoon is small, the wave height does not exceed 1 m. In summer, during the southwestern monsoon, stronger waves develop, the frequency of waves with a height of 2 m or more is 45%. In the southwestern part of the sea, the wave height can reach 10-12 m, and the frequency of waves with a wave height of 5 m or more is about 25%.

Bottom relief

In terms of the bottom relief, the Arabian Basin is a vast plain with a depth of 4000-5000 m, slightly inclined towards the Arabian-Indian ridge. In the northwestern part of the sea, between the Oman and Arabian basins, there is the Murray ridge, which stretches from the continental slope to the southwest for almost 500 km. The depths above its peaks are 300-400 m.

The shelf and continental slope are well developed near the Indian subcontinent. The width of the continental shelf varies from 40 km in the south to 450 km against the Gulf of Cambay. The continental slope is well expressed in the relief by a relatively low scarp. Opposite the mouth of the Indus, the shelf and continental slope cuts through a deep and narrow submarine canyon. The upper reaches of the canyon juts out into the shelf for more than 100 km. Its depth in the direction from the coast increases from 100-200 to 1000-1500 m. The width of the canyon - up to 10 km, at the bottom - 3.5 - 5.0 km.

Along the northern and western coasts, the shelf is narrow - from 9-10 to 80 km. The continental slope near the Arabian Peninsula and in the northern part of the sea is a steep scarp with a smooth transverse profile.

The relief of the bottom and current of the Arabian Sea

Hydrology and water circulation

The greatest value of annual level fluctuations, caused by changes in atmospheric pressure, is observed in the north of the Arabian Sea and is 20 cm, with the low standing of the level confined to the northeastern monsoon, and high - to the southwestern.

The tides in the sea are irregular semidiurnal. The magnitude of the tides in Sigizia at Aden is 2.5 m and increases along the northern shores to the east, reaching 5.7 m at Bombay. Further south along the coast of the Indian subcontinent, the magnitude of the tides decreases to 1.1 m.

The main features of the circulation of the waters of the upper layer of the Arabian Sea are formed mainly under the influence of the monsoon system of winds. In summer, during the southwestern monsoon, an anticyclonic gyre is formed, elongated along 10 ° N. In the north east coast In Africa this season, the Somali current is formed, which is characterized by a high speed, in some cases exceeding 200 cm / s. In the Arabian Sea, the Somali current forks: one branch is directed to the northeast, along the coast of the Arabian Peninsula, the other, less clearly expressed, at 8 ° N. deviates to the east. As you move in. In the Arabian Sea, the Somali current is gradually weakening. Against the background of the general anticyclonic movement of waters, cyclonic eddies are observed near the Socotra and Lakkadiv islands.

Intense atmospheric and oceanic circulation during the southwestern monsoon determines the development of upwelling in some areas of the sea. Along the coast of Somalia, the Arabian Peninsula, west coast the Hindustan Peninsula, the waters rise, developing on the left side of a strong current. The most intense upwelling is expressed off the coast of Somalia up to 11 ° N, where the entire warm surface layer is replaced by water with temperatures below 20 ° on the surface. In the north, this upwelling area is limited by the flow of warm surface water from the Gulf of Aden, which separates the Somali upwelling and upwelling along the coast of the Arabian Peninsula. Summoned strong winds blowing parallel to the coast, upwelling along the Arabian Peninsula in volume may exceed the Somali.

In winter, during the northeastern monsoon, a restructuring of the water circulation occurs: the anticyclonic movement, characteristic of summer, is replaced by a cyclonic movement, well expressed in the central part of the sea. In the west, there is a flow of water from the Gulf of Aden. The winter monsoon, which is much weaker than the summer monsoon, does not cause a large surge. In coastal areas, there is a slight subsidence of cooled surface waters. Only under certain wind conditions that cause water displacement, upwelling can be observed in the northern part of the sea, off the coast of Pakistan. In the central part of the sea, deep waters rise in the center of the cyclonic circulation.

Seasonal changes in the structure of density currents extend to a horizon of about 300 m. From a horizon of 500 m and below, cyclonic water circulation prevails over most of the sea, the intensity of which is much weaker than the circulation in the overlying layers. Only to the east of about. Socotra has an anticyclonic circulation.

Water temperature and salinity

The Arabian Sea is one of the heat accumulators in. The influx of a large amount of solar energy to the sea surface determines its high upper layer in all seasons of the year.

In summer, spatial differences in surface temperature exceed 11 ° (from 28-29 ° in the open sea to 18-20 ° off the coasts of Oman and Somalia). In winter, the maximum surface temperature (28 °) is observed in the southern part of the sea; in the northern part and near the Arabian Peninsula, it drops to 24-25 °, and in the northeast of the sea - to 21-22 °.

Heat is transferred from the surface to the water column mainly as a result of convective mixing, which develops in the Arabian Sea, mainly due to salinization during evaporation (tropical type), as well as wind mixing. The depth of density convection is mainly limited to a layer 25-30 m thick.

The upper boundary of the seasonal thermocline in the northwestern part of the sea and off the coast of Oman is in the 20-30 m layer in summer; its position is affected by the influence of upwelling. In the open areas of the sea, the thermocline depth increases from north to south from 50 to 150 m. Near the African coast, under the influence of the Somali current, the waters are well mixed, the temperature jump is in the 100-200 m layer, and its vertical gradients are lower than in other areas of the sea.

In winter, the maximum vertical temperature gradients are observed in the middle of the cyclonic gyre in the central part of the sea in a layer of 75–125 m. In the northern, northeastern parts of the sea and off the coast of the Indian subcontinent, the gradients are less, and the thermocline is in the 100–150 m layer.

On the horizon of 100 m in summer, the temperature in the central part of the sea is 25 °, only near the coast of the Somali Peninsula is 12-14 °. "Cold" water (18-20 °) is located along the entire coast of Oman. Along the coast of the Indian subcontinent, the water temperature increases from the coast, where it is 20-21 ° (which is associated with the rise of waters) to the central part of the sea (24 °). In the southeastern part of the sea, the temperature in summer is 19-20 °, and in the Laccadives, 18-19 °. In winter, on the horizon of 100 m, the highest temperature is in the Laccadives (27 °); along the coast of the Indian subcontinent it is 24 °, in the central and western parts of the sea - from 21 to 23 °.

In the vertical structure of the waters of the Arabian Sea, there are surface Arabian, intermediate (Persian-Arabian and Red Sea-Arabian), deep North Indian and bottom water masses.

Water temperature and salinity on the surface of the Arabian and Andaman seas in summer

Surface Arabian water mass (from 0 to 100-150 m) is formed under the influence of salinization during evaporation mainly in the northern part of the sea, from where it spreads to the south. The core of this water mass, determined by the maximum salinity (36.2-36.7 ‰), deepens from 20 to 75 m in the direction from north to south. The surface water mass is characterized by temperatures of 21-25 ° in winter and 22-28 ° in summer. The content of nutrients in this water mass is higher than in other regions of the Indian Ocean.

Intermediate (from 200-250 to 1500 m) Arabian water mass is formed under the influence of advection of warm waters of increased salinity: transformed Red Sea waters coming from the Gulf of Aden; waters of the Persian and Oman gulfs and mixing them with the overlying waters. Waters of increased salinity spread over a vast area, and their influence - a slight increase in salinity - is traced not only in most of the Arabian Sea, but also in the western part of the Indian Ocean.

A distinctive feature of the Persian-Arabian water mass is the maximum salinity (36.25-36.5 ‰) at a horizon of about 250 m, which characterizes the waters formed in the Persian Gulf (where salinity varies from 37-38 ‰ at the entrance to the Gulf to 40-41 ‰ in its western and northwestern parts) and entering through the Gulf of Oman into northern part seas. The water temperature varies from 10 to 16 °. This water mass with a thickness of about 200 m in winter spreads over most of the sea area, and in summer, with the development of the Somali current, it shifts to the east and southeast. Its upper boundary is located at the horizon of 200-250 m, the lower one is at the horizon of 400 m.

The Red Sea-Arabian water mass stands out according to the maximum salinity of the Red Sea origin (salinity in the water column of the Red Sea is more than 40 ‰). It is characterized by a temperature from 10-12 ° at the upper border to 5 ° at the lower one. The maximum salinity (35.2-35.6 ‰) is most pronounced in the 500-800 m layer and spreads over the sea area up to 2 ° N. At the exit from the Gulf of Aden, the core of the maximum is located at the horizon of 800 m, in the central part of the sea - 600 m, and rises to 500 m in the direction to the north and south. The upper boundary of the Red Sea-Arabian water mass in different regions of the sea is located at horizons from than 500 to 550 m, the lower one is 1200 m on the horizon.

The intermediate water of the Arabian Sea has the highest nutrient concentrations for the Indian Ocean. In addition, a pronounced minimum of oxygen is observed in this water (0.1-0.5 ml / l). It is formed due to the high consumption of oxygen during oxidative processes, the sharp density stratification of waters, which prevents the flow of oxygen from the overlying layers, and the limited exchange at the intermediate horizons of the waters of the Arabian Sea with the waters of the adjacent part of the Indian Ocean, which is due to the presence of two zones of divergence at the southern boundary of the sea.

The layer from 1500 to 3500 m in the Arabian Sea is occupied by the deep North Indian water mass, formed from the highly saline waters of the Arabian Sea and the transformed Antarctic bottom waters. This water mass is characterized by a temperature from 3.5-4 ° at the upper boundary to 1.8-2 ° at the bottom. Salinity varies from 34.75 to 34.9 ‰. The oxygen content is higher than in intermediate water (2 - 3.5 ml / l).

Oxygen minimum in the Arabian Sea

The layer from 3500 m to the bottom is occupied by bottom waters. The main source of their formation is the Weddell Sea, from where they spread northward along western shores of all oceans, and in the Indian Ocean they fill all the basins to the most northern regions. The bottom waters of the Arabian Sea are characterized by a homogeneous distribution of hydrological characteristics: the temperature is in the range of 1.5-1.7 °, salinity is 34.74 ‰.

Economic value

Explorer submariner

The peculiarities of the structure and circulation of the waters of the Arabian Sea largely contribute to the fact that this sea belongs to the highly productive regions of the World Ocean.

The most favorable conditions for the development of phytoplankton are created in the summer in the sea shelf zone. This is ensured by the high content of nutrients entering the upper productive layer in the upwelling areas.

In winter, over most of the shelf zone, the water is much poorer in phytoplankton than in summer. A high biomass of phytoplankton remains in the winter season only near the Gulf of Oman and the mouth of the river. Ind.

In the central part of the sea, on the contrary, favorable conditions for the development of phytoplankton are created in winter, when the waters rise in the center of the cyclonic cycle. In summer, when the waters sink in the center of the anticyclonic circulation, the supply of mineral compounds of phosphorus and especially nitrogen is low. In this regard, the biomass and production of phytoplankton in summer is 5-6 times lower than in winter.

Sufficiently high values ​​of biomass and production of phyto- and zooplankton in the Arabian Sea are good prerequisites for the formation of commercial accumulations. The main environmental factor that directly limits the formation of such accumulations is the low oxygen content. For example, during the southwestern monsoon, when oxygen-depleted waters rise to the shelf, fish mostly disperse and leave these areas.

The commercial value of the Arabian Sea is determined by the large stocks of fish (over 1000 species) and crustaceans. However, most of the catches consist of five species of fish: two pelagic (two species of horse mackerel) and three near-bottom (Japanese crucian carp, saurida, sea bass). Of the rest of the bottom and bottom fish, the highest abundance is in the pair, rock perches (merrow), catfish, slabs (captain), etc.

In the shelf zone of the sea, the most numerous and widespread population of the Japanese carp.

In the central part of the sea, large fish such as yellowfin and bigeye tuna, as well as various shark species, are fished. Tuna are thermophilic fish, and their distribution is greatly influenced by the water temperature and the position of the thermocline, which limits their vertical movement. The catch of tuna in the Arabian Sea is 3-4 times less than in the equatorial zone of the Indian Ocean. Towards the south, where the upper boundary of the oxygen-deficient layer is deeper, the number of tunas increases.

The stocks of the main commercial fish in the Arabian Sea, especially off the eastern coast, are exploited quite intensively, and some commercial species are already in a depressed state. Commercial fish fauna is negatively affected by water pollution by oil products (especially in the northern part of the sea), agricultural and household wastewater. The marine environment in the shelf zone of the Arabian Sea is in need of restoration and protection.

ARABIAN SEA

ARABIAN SEA

semi-enclosed sea of ​​the Indian Ocean between the Arabian and Hindustan peninsulas. The greatest depth is 5803 m, the large bays of Oman, Aden. It is connected with the Red Sea by the Bab el-Mandeb Strait (length 900 km, width up to 300 km, depth up to 4525 m). water temperature 22-29 ° С, salinity more than 36 ppm. Tuna fishing, swordfish, shipping.

Concise Geographical Dictionary... EdwART. 2008.

Arabian Sea

(Arabian Sea), a semi-enclosed sea on the north. Indian Ocean , located between the peninsula Arabian and Hindustan ... Border to the southwest. - Cape Khafun (Somalia) - Addu atoll - west. edge Maldivian and Laccadives ... Pl. with Aden and The Omani Hall. 4832 thousand km², average depth 3006 m, naib. 5803 m. Surface temperature in winter is 24–25 ° С, in summer more than 28 ° С. The salinity of the surface is more than 36 ‰, in the rainy season less than 35 ‰. In the north there is a wide silt-covered shelf; near the coast there is a lot of sand brought by the wind from the desert. Two basins: Arabian on the NE. and Somali to the southwest, their bottom is lined with red clay. Main ports: Bombay (India), Karachi (Pakistan), Aden (Yemen). The most productive sea of ​​the Indian Ocean, commercial species - Indian mackerel and sardinella, anchovies, tuna and cuttlefish.

Dictionary of modern geographical names... - Yekaterinburg: U-Factoria. Under the general editorship of Acad. V. M. Kotlyakova. 2006 .

Arabian Sea

a semi-enclosed sea in the northern part of the Indian Ocean, between the Arabian and Hindustan peninsulas. The border in the south is the line running from Cape Khafun (Somalia) to Addu Atoll and further to the west. the edge of the Maldives and Lakkadives. Pl. 4832 thousand km², the greatest depth. 5803 m. Average annual water temperature from 24 to 28 ° C. Salinity 35–36 ‰. Irregular semi-daily tides, up to 5.1 m. The monsoons have a strong influence on the hydrological regime and weather. In the north of the sea there is a wide silt-covered shelf. Two basins: the Arabian (northeast) and the Somali (southeast). It washes the shores of India, Pakistan, Iran, Oman, Somalia and Yemen. The United United Arab Emirates, Saudi Arabia, Kuwait, Iraq. Ch. ports: Bombay (India), Karachi (Pakistan), Aden (Yemen). Fishing (Indian mackerel, sardinella, anchovies, tuna).

Geography. Modern illustrated encyclopedia. - M .: Rosman. Edited by prof. A.P. Gorkina. 2006 .

See what the "ARABIAN SEA" is in other dictionaries:

Beach in Goa ... Wikipedia

Modern encyclopedia

Part of the Indian ok., Between the Arabian Peninsula in the west and the Indian subcontinent in the east. 4832 thousand km & sup2. Depth up to 5803 m. Large bays: Aden, Oman, Kach, Cambey. Large islands: Socotra, Laccadives. The river flows in. Ind. Main ports: ... ... Big Encyclopedic Dictionary

Arabian Sea- Indian Ocean, between the Arabian and Hindustan peninsulas. The area is 4832 thousand km2. Depth up to 5803 m. Large bays: Aden, Oman. Large islands: Socotra, Laccadives. The Indus River flows in. Fishing (tuna, sword fish, etc.). Large ... ... Illustrated Encyclopedic Dictionary

Part of the Indian Ocean, between the Arabian Peninsulas in the west and the Indian subcontinent in the east. 4832 thousand km2. Depth up to 5803 m. Large bays: Aden, Oman, Kach, Cambey. Large islands: Socotra, Laccadives. The Indus River flows in. The main ... ... encyclopedic Dictionary

The Arabian Sea is also called the Persian, Oman, Eritrean, Indo-Arab and Green. This is a marginal sea located between the Hindustan and Arabian peninsulas. Conditional is southern border of this reservoir.

The map of the Arabian Sea shows that it is one of the most large seas on the planet. Its area is approximately 4832 sq. km. Average depth is 2734 m, and the maximum is 5203 m. The sea stretches in the subtropical and tropical zones of the northern hemisphere. Its waters wash the shores of countries such as Iran, Yemen, Djibouti, UAE, Oman, Pakistan, Lakshadweep Union Territory and India. The most large river, flowing into this body of water, is the Indus. There are several large islands... The island of Masira (possession of Oman) is considered famous, where a lot of sea turtles are observed in the summer.

Climatic features

A monsoon warm climate prevails in the Arabian Sea region. On weather the climate of Hindustan is strongly influenced. On average, the air temperature above the water area varies from +22 to +28 degrees. It does not depend on the season. Sea water has a salinity of about 36.5 ppm. During the summer months, the coast of the Arabian Sea is more humid. The water area is very often affected by typhoons.

Natural features

The Arabian Sea is famous for its variety of life forms. There are a lot of commercial fish here, among which sardines, tuna, mackerel, marlin and sailfish are of particular importance. For the economies of coastal countries, crustaceans are important: lobsters, crabs and shrimps. There are a lot of corals on the coast. It is also home to molluscs, fish, crustaceans and invertebrates. In the Arabian Sea, there are butterfly fish, lionfish, triggerfish, clownfish, flying fish, gobies, etc. The Arabian Sea is second only to the Red Sea in the richness of its fauna.

Significance of the sea

Coastal states are actively investing in tourism development. New resorts appear there from time to time. Oman is attractive for tourists, which is visited by more than 1 million foreigners annually. Commercial fishing for sardines, tuna, mackerel and other fish takes place in the sea. The water area is considered an important trading region. Major ports are Karachi, Bombay, Muscat, Aden. Transportation of "black gold" from states takes place across the Arabian Sea Persian Gulf to America, Europe, the Far East.

Going to India, travelers rarely look for information about the Arabian Sea, limiting themselves to an online excursion into the culture, cuisine and attractions of the country.
But why not get acquainted with some interesting facts about the sea that washes this magical land?

Few facts

Arabian Sea, formerly known in different countries under many other names, such as Eritrean, it is located between the Arabian and Hindustan peninsulas and has an area of ​​4832 thousand km. It is one of the largest seas in the world, into which many large bays and the Indus River flow into. Also, the shores are decorated with picturesque rocky bays. The Arabian Sea itself is part of the Indian Ocean.

Geographical excursion

There are practically no islands in the Arabian Sea, and most of the existing ones are located off the coast. The largest of them are Laccadives and Socotra. The climate near the sea is tropical monsoon, with humid, cloudy summers and clear cool winters with air temperatures of 25-29 and 20-25 degrees, respectively. The water temperature pleases all year round - 22-27 degrees in winter and 23-28 in summer with a peak of 29 degrees in May.
Due to the stable warm climate, many popular world resorts, including Indian ones, are located on the shores of the Arabian Sea. One of them is Goa, which attracts lovers of yoga and all kinds of spiritual practices, as well as simply creative people from all over the world. In addition, Goa is famous for beautiful beaches and an active nightlife.

The underwater world of the Arabian Sea

The underwater flora and fauna of the Arabian Sea is truly incredible. Warm waters are a paradise for diving enthusiasts: at the bottom of the sea there is another city, completely built of coral, inundated with many species of fish. However, in the hospitable warm waters dangers also lie in wait - many species of sharks are found here, so you need to be careful to get acquainted with the underwater beauty.
Of course, the resorts off the coast of the Arabian Sea are a Mecca for seafood lovers. The coastal restaurants serve delicious shrimp and mussels, crabs, squid and lobster, as well as a variety of seafood dishes. Also, fresh fish can be bought daily at any of the fish markets. Fishing is one of the main occupations of the inhabitants of the coastal states of India, including Goa.

Arabian Sea really beautiful, so when traveling in India, you should definitely get acquainted with its wonderful underwater world, secluded coves, cool bays and pristine sandy beaches.