Welcome; learn the Ocean 
Currents 
Pacific Ocean, 
Atlantic Ocean 
& 
Indian Ocean
OCEAN CURRENTS 
WORLD
Currents in the pacific ocean 
There are two Equatorial currents in the 
Pacific Ocean. One in the north of the 
equator and the other south of the equator
Pacific ocean currents 
● The north equatorial current starts from 
the west coast of central America and 
flows towards the east coast of Asia. 
After reaching the Philippine islands,it 
turns north ward and moves along the 
east coast of Philippines,Taiwan and 
Japan. This is the Kuroshio current.
Pacific ocean currents 
●As it reaches the south east coast of Japan,the 
currents come under the influence of the 
Westerlies and flows across the north pacific 
ocean from west to east as the north pacific 
current. It reaches the cost of the British 
Columbia (North America) and divides into two 
currents. One branch turns north and flows 
along the coasts of Canada and Alaska. The 
current is called British Columbian current. It is 
warm compared with the temperature of the sea 
in this region.
Pacific ocean currents 
The second branch of the North Pacific 
current flows southwards along the west 
coast of north America, as the California 
current, and eventually , and merges 
with equatorial current. As the California 
current is comparatively cooler than the 
sea through which it flows, it is 
considered to be a cold current.
Pacific ocean currents 
A cold current called Oyashio flows 
along the shores of Kamchatka 
peninsula. The cold Okhotsk current 
flows along Sakhalin coast and 
merges with the Oyashio in the sea 
near Hokkaido.
Pacific ocean currents 
The south equatorial current starts 
south of the equator off the north west 
coast of south America. Flowing from 
east to west, it approaches the north 
east tip of Australia and the Guinea 
island. Here, it bifurcates and the main 
branch turns southwards. It flows along 
east coast of Australia as the warm east 
Australian current.
Pacific ocean currents 
Near Tasmania it meets the south Pacific current 
which flows from west to east across the south 
pacific ocean. This current turns north at the 
southern tip of south America, and flows along the 
west coast of south America and the cold Peruvian 
(Humboldt) current and finally merges with the south 
equatorial current. 
Between the two equatorial currents, a counter 
equatorial current flows from west to east. This 
counter current is caused by accumulation of water 
in the western part of the ocean brought by the two 
equatorial currents.
CURRENTS IN THE ATLANTIC 
There are two equatorial currents in the 
Atlantic ocean. The north equatorial 
current, which starts off the west coast of 
equatorial Africa, is driven to towards the 
north-east cost of south America by the 
trade winds. South of the equator, the 
south equatorial current begins to flow 
from the west African coast towards south 
America.
CURRENTS IN THE ATLANTIC 
It bifurcates on approaching the north east 
corner of Brazil (Cape Sao Roque). One 
branch flows along the north eastern cost of 
south America and joins the north equatorial 
current, which splits into two as it enters the 
Caribbean sea. The trade winds push one 
branch into the Gulf of Mexico and raise the 
water level in the gulf. In order to equalize the 
water level of the gulf of Mexico and the 
Atlantic ocean a current flows out through the 
Strait of Florida.
CURRENTS IN THE ATLANTIC 
The second branch of the north equatorial 
current passes along the eastern side of the West 
Indies and joins the current that comes out of 
the Gulf of Mexico. The combined current turns 
north and moves along the south-east coast of 
USA. From Cape of Florida up to Hatteras. 
This current is called Florida Current.
CURRENTS IN THE ATLANTIC 
Beyond cape Hatteras, upto the Grand 
Banks of Newfoundland, this current is 
known as the famous Gulf Stream. 
Driven by the westerlies, the gulf 
stream turns to the right and flows 
eastwards across the north Atlantic 
ocean, as the north Atlantic drift.
CURRENTS IN THE ATLANTIC 
After entering the eastern part of north 
Atlantic, it bifurcates, and the main branch 
continues its onward movements as far as 
the British Isles, retaining the name of the 
North Atlantic drift. Ahead of British Isles, 
the current assumes the name Norwegian 
current and enters the Arctic ocean after 
flowing past Norway
CURRENTS IN THE ATLANTIC 
The second branch of the North Atlantic 
Drift flows south between Spain and 
Azores Archipelago(Group of islands) 
and ends up in the region where the 
north equatorial current begins. It is 
known as the cold Canaries current.
CURRENTS IN THE ATLANTIC 
From the Arctic ocean a cold current flows 
south along the west coast of green land. 
This current is known as the Labrador 
Current, meets the warm Gulf Stream in the 
sea near the islands of Newfoundland. The 
mixing of waters of the Gulf Stream with the 
cold Arctic waters of the Labrador current 
often leaves to the formation of fogs which 
envelope the sea for hours together.
CURRENTS IN THE ATLANTIC 
These fogs present navigational hazards to 
shipping owing to the presence of icebergs 
which are carried down by the Labrador 
current. But the meeting of warm and cold 
currents provides ideal conditions to 
facilitate the growth of many verities of 
fish. The Grant Banks of Newfoundland is 
one of the world's most important fishing 
banks.
CURRENTS IN THE ATLANTIC 
We noted earlier, that the south equatorial 
current bifurcates near the north-east Brazilian 
coast. 
One of the two branches joins the north 
equatorial current and the other one moves 
south along the coast of Brazil. This current has 
been given the name of that country. The warm 
Brazil current goes south and ultimately joins 
the south Atlantic current which flows from west 
to east.
CURRENTS IN THE ATLANTIC 
When the south Atlantic current reaches 
the southern tip of Africa, it sends an off-shoot 
northwards along the west coast of 
southern Africa. It is the cold Benguela 
current and it ends up in the south equatorial 
current. 
A counter equatorial current flows along 
the equatorial region of the Atlantic 
between the two equatorial current
CURRENTS IN THE INDIAN OCEAN 
In the Indian Ocean, especially in the 
northern part ,winds play a dominant 
role in controlling the Ocean currents. A 
complete seasonal reversal of the 
current direction is effected by the 
monsoon winds in the northern part of 
the Ocean
CURRENTS IN THE INDIAN OCEAN 
In winter the North and South equatorial 
currents flow in the Indian Ocean from east 
to west. A counter equatorial current flows 
between the two equatorial currents from 
west to east. The North East Monsoon 
winds drive the north equatorial current 
along the Bay of Bengal cost of India and 
also along the coasts of lands lying around 
the Arabian sea.
CURRENTS IN THE INDIAN OCEAN 
In summer, a strong monsoon 
current sets in from west under the 
influence of south west monsoon 
winds. This current completely 
wipes out both the north equatorial 
and the counter equatorial currents.
CURRENTS IN THE INDIAN OCEAN 
In the southern Indian Ocean the general 
pattern of the currents is like of the Pacific 
and Atlantic ocean. The south equatorial 
current, fed by the branch of the south 
equatorial current of the Pacific Ocean and 
driven by the trade winds flowing from east 
to west turn southwards after reaching the 
east cost of Africa. It then flows south along 
the Mozambique 
coast and through the Mozambique channel, 
bearing the name Mozambique warm 
current.
CURRENTS IN THE INDIAN OCEAN 
It proceeds further southwards and gets 
strengthened by the branch of the south 
equatorial current flowing past the east 
cost of Island of Madagascar. Along the 
south eastern cost of Africa the 
combined current is called the 
Aguilhaus current. It pushes on as a 
warm current and merges with the west 
wind drift.
CURRENTS IN THE INDIAN OCEAN 
The west wind drift flowing in the belt of 
Brave west winds also called “Roaring 
Forties” across the southern ocean from 
west to east, reaches the south western 
corner of Australia. At this point it sends 
one of its branches northwards along the 
west cost of Australia as a cold current. This 
current called the west Australian current 
flows northward and joins the south 
equatorial current.
Prepared by 
JEYANTHY.R 
H.S.A.(SS) 
GMMGHSS 
PALAKKAD

Ocean currents

  • 1.
    Welcome; learn theOcean Currents Pacific Ocean, Atlantic Ocean & Indian Ocean
  • 11.
  • 20.
    Currents in thepacific ocean There are two Equatorial currents in the Pacific Ocean. One in the north of the equator and the other south of the equator
  • 21.
    Pacific ocean currents ● The north equatorial current starts from the west coast of central America and flows towards the east coast of Asia. After reaching the Philippine islands,it turns north ward and moves along the east coast of Philippines,Taiwan and Japan. This is the Kuroshio current.
  • 22.
    Pacific ocean currents ●As it reaches the south east coast of Japan,the currents come under the influence of the Westerlies and flows across the north pacific ocean from west to east as the north pacific current. It reaches the cost of the British Columbia (North America) and divides into two currents. One branch turns north and flows along the coasts of Canada and Alaska. The current is called British Columbian current. It is warm compared with the temperature of the sea in this region.
  • 23.
    Pacific ocean currents The second branch of the North Pacific current flows southwards along the west coast of north America, as the California current, and eventually , and merges with equatorial current. As the California current is comparatively cooler than the sea through which it flows, it is considered to be a cold current.
  • 24.
    Pacific ocean currents A cold current called Oyashio flows along the shores of Kamchatka peninsula. The cold Okhotsk current flows along Sakhalin coast and merges with the Oyashio in the sea near Hokkaido.
  • 25.
    Pacific ocean currents The south equatorial current starts south of the equator off the north west coast of south America. Flowing from east to west, it approaches the north east tip of Australia and the Guinea island. Here, it bifurcates and the main branch turns southwards. It flows along east coast of Australia as the warm east Australian current.
  • 26.
    Pacific ocean currents Near Tasmania it meets the south Pacific current which flows from west to east across the south pacific ocean. This current turns north at the southern tip of south America, and flows along the west coast of south America and the cold Peruvian (Humboldt) current and finally merges with the south equatorial current. Between the two equatorial currents, a counter equatorial current flows from west to east. This counter current is caused by accumulation of water in the western part of the ocean brought by the two equatorial currents.
  • 28.
    CURRENTS IN THEATLANTIC There are two equatorial currents in the Atlantic ocean. The north equatorial current, which starts off the west coast of equatorial Africa, is driven to towards the north-east cost of south America by the trade winds. South of the equator, the south equatorial current begins to flow from the west African coast towards south America.
  • 29.
    CURRENTS IN THEATLANTIC It bifurcates on approaching the north east corner of Brazil (Cape Sao Roque). One branch flows along the north eastern cost of south America and joins the north equatorial current, which splits into two as it enters the Caribbean sea. The trade winds push one branch into the Gulf of Mexico and raise the water level in the gulf. In order to equalize the water level of the gulf of Mexico and the Atlantic ocean a current flows out through the Strait of Florida.
  • 30.
    CURRENTS IN THEATLANTIC The second branch of the north equatorial current passes along the eastern side of the West Indies and joins the current that comes out of the Gulf of Mexico. The combined current turns north and moves along the south-east coast of USA. From Cape of Florida up to Hatteras. This current is called Florida Current.
  • 31.
    CURRENTS IN THEATLANTIC Beyond cape Hatteras, upto the Grand Banks of Newfoundland, this current is known as the famous Gulf Stream. Driven by the westerlies, the gulf stream turns to the right and flows eastwards across the north Atlantic ocean, as the north Atlantic drift.
  • 32.
    CURRENTS IN THEATLANTIC After entering the eastern part of north Atlantic, it bifurcates, and the main branch continues its onward movements as far as the British Isles, retaining the name of the North Atlantic drift. Ahead of British Isles, the current assumes the name Norwegian current and enters the Arctic ocean after flowing past Norway
  • 33.
    CURRENTS IN THEATLANTIC The second branch of the North Atlantic Drift flows south between Spain and Azores Archipelago(Group of islands) and ends up in the region where the north equatorial current begins. It is known as the cold Canaries current.
  • 34.
    CURRENTS IN THEATLANTIC From the Arctic ocean a cold current flows south along the west coast of green land. This current is known as the Labrador Current, meets the warm Gulf Stream in the sea near the islands of Newfoundland. The mixing of waters of the Gulf Stream with the cold Arctic waters of the Labrador current often leaves to the formation of fogs which envelope the sea for hours together.
  • 35.
    CURRENTS IN THEATLANTIC These fogs present navigational hazards to shipping owing to the presence of icebergs which are carried down by the Labrador current. But the meeting of warm and cold currents provides ideal conditions to facilitate the growth of many verities of fish. The Grant Banks of Newfoundland is one of the world's most important fishing banks.
  • 36.
    CURRENTS IN THEATLANTIC We noted earlier, that the south equatorial current bifurcates near the north-east Brazilian coast. One of the two branches joins the north equatorial current and the other one moves south along the coast of Brazil. This current has been given the name of that country. The warm Brazil current goes south and ultimately joins the south Atlantic current which flows from west to east.
  • 37.
    CURRENTS IN THEATLANTIC When the south Atlantic current reaches the southern tip of Africa, it sends an off-shoot northwards along the west coast of southern Africa. It is the cold Benguela current and it ends up in the south equatorial current. A counter equatorial current flows along the equatorial region of the Atlantic between the two equatorial current
  • 39.
    CURRENTS IN THEINDIAN OCEAN In the Indian Ocean, especially in the northern part ,winds play a dominant role in controlling the Ocean currents. A complete seasonal reversal of the current direction is effected by the monsoon winds in the northern part of the Ocean
  • 40.
    CURRENTS IN THEINDIAN OCEAN In winter the North and South equatorial currents flow in the Indian Ocean from east to west. A counter equatorial current flows between the two equatorial currents from west to east. The North East Monsoon winds drive the north equatorial current along the Bay of Bengal cost of India and also along the coasts of lands lying around the Arabian sea.
  • 41.
    CURRENTS IN THEINDIAN OCEAN In summer, a strong monsoon current sets in from west under the influence of south west monsoon winds. This current completely wipes out both the north equatorial and the counter equatorial currents.
  • 42.
    CURRENTS IN THEINDIAN OCEAN In the southern Indian Ocean the general pattern of the currents is like of the Pacific and Atlantic ocean. The south equatorial current, fed by the branch of the south equatorial current of the Pacific Ocean and driven by the trade winds flowing from east to west turn southwards after reaching the east cost of Africa. It then flows south along the Mozambique coast and through the Mozambique channel, bearing the name Mozambique warm current.
  • 43.
    CURRENTS IN THEINDIAN OCEAN It proceeds further southwards and gets strengthened by the branch of the south equatorial current flowing past the east cost of Island of Madagascar. Along the south eastern cost of Africa the combined current is called the Aguilhaus current. It pushes on as a warm current and merges with the west wind drift.
  • 44.
    CURRENTS IN THEINDIAN OCEAN The west wind drift flowing in the belt of Brave west winds also called “Roaring Forties” across the southern ocean from west to east, reaches the south western corner of Australia. At this point it sends one of its branches northwards along the west cost of Australia as a cold current. This current called the west Australian current flows northward and joins the south equatorial current.
  • 47.
    Prepared by JEYANTHY.R H.S.A.(SS) GMMGHSS PALAKKAD