Arabian Sea. For half the year (April–October), the winds in this region are from the southwest, reversing in the other half of the year. Major seas contributing to Asian Drainage are Andaman Sea, Arabian Sea, Banda Sea, Barents Sea, Bering Sea, Black Sea, Caspian Sea, East Siberian Sea, Java Sea, Kara Sea, Laccadive Sea, Sea of Japan, Sea of Okhotsk. 7.4) and from altimetry (5–7 mm year−1, Fig. West of the Konkan–Saurashtra Coast, the Laxmi Basin in the bottom of the Arabian Sea (Plate 1.4 inset) was created as a result of symmetric sea-floor spreading. The variability in seasonal contrast during glacials and during interglacials suggests that interannual and interdecadal changes in monsoonal strength were also greater during glacial periods than during interglacials (Figure 4). The Indus River forms a wide delta near its mouth at the Arabian Sea on which continent? Palanisamy et al. The Arabian Sea Branch of the Southwest Monsoon first hits the Western Ghats of the coastal state of Kerala, thus making the area the first state in India to receive rain from the Southwest Monsoon. (a radiolarian) and pollen reveal that the south-west monsoon winds were more intense during interglacials (warm periods) and weaker during glacials (cold periods), recognized by the oxygen isotopic stratigraphy in the same samples. This substantiates that lower denitrification during glacial periods in the Arabian Sea could have resulted from a decrease in upwelling and the settling flux of organic material through the water column. About Arabian Sea: The Facts: Area: 1,491,000 sq mi (3,862,000 sq km). Pakistan. London, UK. (2014) compared two longest TGs: Malé and Gan (∼20 years of length, available from PSMSL dataset), with satellite altimetry and past SL reconstruction. What two seas border Saudi Arabia? A new ocean floor is forming as lavas well up from the interior and freeze in the cold ocean bottom. The sea is of geostrategic interest as it is the transit route for a major portion of the world's oil supply. The N2 fixation rates in the eastern AS varied from ∼0.1–34 mmol Nm−2day−1. In addition, the commerce flowing by ship from Asia to Europe also sails this sea. An Important Shipping Lane: The Arabian Sea is a body of water that is very important as a shipping lane. The floor of the Arabian Sea is moving northwards and plunging into the Oman Trench just south of the Makran coast of Pakistan (Plate. Periods with a pronounced OMZ (such as the present times) are characterized by shallow winter mixing, while annual surface-water productivity is high. The Arabian Sea is a region of the northern Indian Ocean bounded on the north by Pakistan, Iran, and the Gulf of Oman, on the west by the Gulf of Aden, Guardafui Channel and the Arabian Peninsula, on the southeast by the Laccadive Sea, on the southwest by the Somali Sea, and on the east by India.Its total area is 3,862,000 km 2 (1,491,000 sq mi) and its maximum depth is 4,652 meters (15,262 ft). The northern Arabian Sea is one of the few regions in the open ocean where thermocline water is severely depleted in oxygen. In the AS, oxygen-depleted waters ascend to very shallow depths (Naqvi et al., 2006a). The δ15N and organic carbon profiles indicate higher productivity and denitrification during the Holocene as compared to the last glacial period. The thermocline is also coincident with a strong oxycline, leading down into a deeper water mass having around 0.5 ml liter−1 dissolved O2. Arabia is the largest peninsula on Earth and it occupies an area of about 1,250,000 square miles. Islands : There are many groups of (2014) focused on the long-term SL rise in the northwestern Persian Gulf. (A) Oxygen isotope profiles of planktonic foraminifera (Pulleniatina obliquiloculata, δ18OP), and benthic foraminifera (Uvigerina excellens, δ18OB) and the difference between oxygen isotopes of planktonic and benthic foraminifera (Δδ18OB−P). The Third and Final Continent by Jhumpa Lahiri I left India in 1964 with a certificate in commerce and the equivalent, in those days, of ten dollars to my name. The DIN from rivers exported to the BOB is less (<0.5 Tg N a−1) compared to AS (Naqvi et al., 2010). During the period of Roman Empire, its name was Erythraean Sea. Their work suggests that RSL in this region is currently as much as ∼50 mm lower than it would be in the absence of global groundwater depletion. depth: 4,652 m (15,262 ft). The situation is being further aggravated in the Indus delta along Pakistan’s coast, in Sindh province. EUROPE In the south there are two big bays — the Arabian Sea and the Bay of Bengal. Commercial fishing is a major activity in the Arabian Sea with the leading species fished being sardines, prawns, and mackerel. The Southwest Monsoon spins up an anticyclonic gyre, though weaker than that of the Arabian Sea, which transports warm water of southern origin (Shetye, 1993), observable in satellite IR imagery, northward along the coasts of both India and Sri Lanka. Unnikrishnan and Shankar (2007) conducted complete reanalysis of these records. Consequently the Indian Oceanic Plate is converging towards the Malaysia–Indonesia–Thailand plate at the rate of 30 mm/year (Curray, 2005). One is in the northern part, in July–September, centered at 20°N 90°E. Locations, time spans and trends of RLR PSMSL tide gauges and SONEL GPS stations. Arabian Sea is only a part of the Indian Ocean that is located between the Arabian Peninsula and the Indian subcontinent. Thus, glacial decreases in productivity and denitrification in the Arabian Sea are attributed to the weakening of the summer monsoonal winds that drive seasonal upwelling and dominate mean annual export production. Shankar et al. (Also Read – 10 Largest islands of World) There are no islands in the middle of the Arabian Sea, where depths average in excess of 9,800 ft (3,000 m). This population increase and industrial development create major pollution problems. These rupture planes extend northwestwards through the coastal belt on to the offshore to form underwater basins (rifts) and ridges (horsts).