Tech in the Indian Ocean map. Musonic flows of the Indian Ocean

surface leaks Indian Ocean

Top flows of the Pacific Ocean.

Pacific Ocean To reach a lot of knots from entering the skid, to cross the latitudinal streams of water in conjunction with the cym in the new one. In the oceans there are 2 majestic rings of the ruins of the waters: pivnichnu and pivdennu. Pivnichne circle includes Pivnichne passatna with a broach, Kurosio, Pivnichnotikhookeansky and californian current. Pivdenne kolce store pivdenne passatna, skidno-australiyke, stretching out ancient wines and peruvians. These technologies infuse heat into the ocean and the nature of the adjacent continents for the re-generation of heat. Thus, the flow of warm water flows from the remote tropical coasts of the mainland to the lower ones, in connection with the cym in low latitudes. Zakhidna chastina the ocean is often warmer than the ocean. In the middle high latitudes - navpaki, the lower part of the warmer than the back.

In the private part of the ocean of monsoons, there is a seasonal cycle of leaks. The levy will rise up in the middle of the winter months in a stretch, taking a cob in Bengalsky zatotsi. Pivdennish 10 pn. There is a current to cross in Zakhidna in a stretch, so that the ocean flows from the Nikobar Islands to the shores of Western Africa, it develops. One bottle of water in Chervona more, іnsha per day up to 10 pd. and quickly, filling up skidny straight yes an ear of Mіzhpasatnі prototypes. Remaining overwhelmed the ocean and the shores of Sumatri, once again, it is a part of the waters to the Andaman Sea, and the main part is straight through the Malimi Sondski Islands and the northern coast of Australia to the Pacific Ocean. Vlіtku u-v the monsoon will secure the transfer of the mass of surface waters to the skid, and the equatorial leak of the weak. The lithuanian monsoon stretches out to repair the coast of Africa with the straining Somali plin, until a current from the Red Sea will come in the area of ​​Aden. At the Bengali summer monsoon, I hold out a bit of time for pivnich; In general, the system of leaks in the Indian Ocean is to blame for the presence of two head gyres. At the winter hour (during the winter season), a private cycle is seen, so that the monasteries become Somal and Equatorial leaks. A lot of pivnіchno іvnіchnoіy pіvnіchno іvkulі monson stretching out, swelling prototypal zmіst, get angry with Equatorial and very daringly. In the result of the winter cycle, it will stop during the first week of the Easter Passatnoy current. Another, pivdenny circuit is adopted by the flows of Pivdenny Pasatnoy, Madagascar, Agulians, Western and Western-Australian. In the Arabian Sea, Bengal and Great Australian outflows and in Antarctic waters, there are many circuits.

The upper currents of the Indian Ocean are a witness and a vision. Classification and special features of the category "Top currents of the Indian Ocean" 2014 rock, 2015.

In the Indian Ocean, surface flows can be divided into three types: monthly flows, winter events and sea flows. Oglyadova flow map for lit and winter pivnichnoy pivkuli, yes I'll put in a picture Flows to the ocean: in addition, the picture of the private part of the ocean and the Golkovy current will add to the view of the flow of the Indian Ocean. Muson currents of the Indian Ocean... Mіzh 10 ° S NS. and on the mainland of Asia over the Indian Ocean, we can see some periodical winter mussons, which we are going through the birch trees in the NE, and in the morning, in the spring from SW in the northern hemisphere and from the NW and SE in NS. The very appearance of periodic winds over the whole part of the ocean and the establishment here of a system of periodic leaks in the surface balls of the ocean, now again a great deal of winds, as a cause of leaks, are confirmed. The prevalence of ocean currents from the winds is even worse, and before that, not only in the area of ​​monetary flows, but in other areas of the ocean. Musonic flows of the Indian Ocean in the winter of the winter season . Musonic flows in the winter of a private party for a private party from an eq. (Over the ocean dme NE muson). At the beginning of the meeting, the NE Mason has been established, the surface of the leaks in the whole hour will be wrong and will be repaired only in the fall of the leaves. At the Bengal, but the current in the private part is wrong, and in the first part of the Moluccan canal to Ceylon, and for the first time from the new current to go to W for 50-70 nautical miles. In the Arabian Sea, stretching along the W and WSW, from the average speed of 10-20 nautical miles, and going to the coast of Africa (the coast of Somalia), it is possible to reach the speed of 50-70 nautical miles. The Somal current, having overtaken the ekvator, is being built from the head of the Equatorial current, which drags on from now on, and is wrapped in E, making the Equatorial prototype. Vono overflows the ocean mіzh 0 і 10 ° S. NS. і bіlya shores of Sumatri will be able to reach a significant discount (40-60 nautical miles); here, in part, go to N, and the head rank of zagortaє on S і is found with Equatorial Plin (div. fig. 179, p. 406). The muson leaks of the winter half of the rock from the birch forest repair the weak (muson dme is correct only until the end of the fierce one), and in the morning a change of leaks will be repaired. Musonic flows in summer drinks . During the winter season, the flow of an approximately ringing straight line arises. Bilya coast of Africa Equatorial stretching, developing the mainland, expanding, and one of the yogy sides on the N vdovzh of the Somal coast. If you overwhelm the ekvator, you will lose more speed and strength from the infusion of fresh SW here to the monkey, so that you can become the SE continuation for the monkey and the new drink. The speed of the central part of the monetary currents (bridging the coast of Africa) in the middle is close to 40 nautical miles, and the most up to 80-120 nautical miles. Between Africa and Ceylon, stretching out on the route with a speed of 25-50 nautical miles. On the first day of Ceylon, the speed of the day grows and trails, reaching 70-80 nautical miles; drive to the coast of Sumatri, by stretching the harness on S and come to the equal. At the same time, Bengal's current flows are straight on NE and the speed of 10-40 nautical miles. Such a character will last the whole hour from grass to spring; in the stinks they fix the weakness and grow the mens by the pickling ones in front of the Arabian Sea and the Bengal flood, and in the fall of the leaves they will fix the flow of the vicious strains. All the monetary flows of the Indian Ocean lie until the currents are warm and purely drifting, ruined by monstrous winds. The situation, which will lead to its establishment and the achievement of the greatest strength, or so close 2.5-3 months, is completely drawn to the minds of Ekman's drift theory of leaks. Species and emergencies, rush in the monetary currents, crops' tied to their hikes in flowing outlines and growing shores in this part of the Indian Ocean, deceased flow. The preliminaries of the peculiarities of the cycle of flows (for example, of the Somali), vibrated by the last hour, showed that, in between the accuracy of the obvious material, the stink of the stench at all was suggested to the minds of the theory of the drift of Ekman, i.e. E. The current period of the Indian Ocean ... Equatorial current in the Indian Ocean only in the early winter, and the first cordon of the fall is close to 10 ° S. NS. In such a rank, it is not meaningful that it is in relation to the other oceans, which is the heritage of the season at 10 ° S. NS. strongly rooted area of ​​musons. In the Indian Ocean SE they lie at 10 ° pivdennish, lower in two oceans, then the area reaches the equator, and the equatorial stretch of the Indian Ocean can lie at 10 ° pivdennish. Since the Equatorial current in the SE region has passed again, I have crossed over again in the fact that the Equatorial current in the region has drifted and is ruined by the passat. Equatorial heat flowing from Australia to Madagascar during the winter of the winter season with a big shine; Average sailing is close to 35 nautical miles, and the most - 50-60 nautical miles. Pivdenna between the leaks is not very significant. Not far from Madagascar, there is a stretch, one can pass to the island from the island and from Cape Delgado (10 ° S.) A part of the current, which is right on the pivnich bridle of the coast of Africa, in the winter pivnichnoe pivkuli not reach the adequate, but. Having set up a mousse with a stretch, go over from the wine to the winter, and with it at once approved the Equatorial prototype, about which it is already said. Another part of the winter season of the Equatorial current, which is seen from Cape Delgado (low coast of Africa, 10 ° S). the average speed is close to 40 nautical miles, and a large one in winter up to 100 nautical miles (on the other side of the channel, nearer to Madagascar, during the less time it is correct, it is not easy to go to N and may have a compensatory character). Mozambic current, moving along the S coast of Africa, crossing the Golkovy Misu (from 30 ° S lat.) - one of the strongest and most violent currents in the oceans. The average speed of the current is close to 50 nautical miles, and the most is up to 100 nautical miles (during the last few hours, in the whole hour in the region of the Mozambic current it is dim E and SE three). Vushko stretching out on the meridian misu of the same day (approximately at 20 ° E) Zagorta on the S and E _і and on the sides with our jars of the Agulhas jar, so that the dough lie on the inner circle towards the misu (about 36 ° S). go to W, and then go to E at 38 ° S). Here the heat is flowing through the cold waters, flowing from the Atlantic Ocean and paternal latitudes For some reason, the temperature on the surface on the nearby buildings does not rise steadily by 4-8 ° (for the first time from the Newfoundland bank, the temperature rises to 15 °). Farther on the edge of the waters of the Golkovo current, wandering with cold water, how to sail out of the Atlantic Ocean, and setting it cold across the length of the Indian Ocean, as well as on the way out of the wide current 10-25 sea mils. Equatorial, yak drove towards 20 ° S. NS. in the middle of the spectacular coast of the island. Madagascar The speed of the current flow is small, about 10-25 nautical miles. With its warm waters, wandering around the cold Cross-flow, amalgamating all the winter surroundings of the rest of the temperature of the water. We went to Australia, a part of the Crosscurrent, and we went to the road for the first day out of it, and partly turned to N to the north-Australian current with the news of 15-30 nautical miles, stretching through absolutely a little bit of temperature. stretching out into the Atlantic Ocean. On the way to the path, the Western Australian outburst leak on the W and even the ear of an equatorial leak, the colossal surface waters in the winter season in the Indian Ocean are frozen. Near the part of the ocean, which lies between the ancient outskirts of the Zond archipelago and Australia, as well as the coastlines of the last one to Torres Street, to catch the tidal leaks. These seas of the Indian Ocean... The Indian Ocean is surrounded by seas, there are only two of them: the Red Sea and the Perska inflow. The Red Sea does not seem to have the right character, but it rises in flowing winds, reaching up to 30-40 nautical miles in some cases. In Bab-el-Mandebskiy prototypes there are two flows, like before, like in the Dardanelles or the Bosphorus. The channel reaches a depth of about 200 m and in a new way from the surface to a depth of close to 120 m and a leak from the Aden inflow in the Chervona Sea is up to 2-2.5 nautical miles per year. Below 120 m, the ringing current from the Red Sea is approximately the same. The tide-long leaks and then there are, like in Gibraltari, and the slowing down of their flow to the strength and weakening of the permanent leaks. At the Persian, the flow stretches out through the ocean, and in winter from the inflow into the ocean. Tides and long-lasting currents are of great importance here.