Ocean Currents
The general movement of a mass of oceanic water in a definite direction is called as “Ocean Currents”
Classifications of Ocean Currents
(01) On the basis of temperature
à Warm Currents: carry warm water away from North and South poles
(Those that flow from equatorial regions polewards have a higher surface temperature and is called as warm currents)
à Cold Currents: carry cold water away from North and South poles
(Those that flow from equatorial regions equatorwards have a lower surface temperature and is called as cold currents)
(02) On the basis of velocity, dimension and direction
àDrifts: The forward movement of surface water of the oceans under the influence of prevailing winds
à Currents: Involves the movement of oceanic water in a definite direction with greater velocity
à Streams: Involves movement of larger mass of ocean water like big rivers of the continent in a definite direction with greater velocity than drifts.
The direction of ocean currents is determined and detected by:
(i) prevailing winds
(ii) earth rotation
(iii) configuration of coastlines and
(iv) bottom reliefs of the oceans.
Generally, warm current is represented by solid line with arrow mark at the end (à) and
cold current is represented by dashed line with arrow mark at the end (- - ->)
Effects of Ocean Currents:
i) Modification in the coastal climate
ii) Effects on fishing
iii) Effects on trade and navigation
Major Currents:
#
|
Current
|
Type
|
Ocean
|
1
|
North Equatorial
|
Warm
| |
2
|
South Equatorial
|
Warm
| |
3
|
Counter-Equatorial Current
|
Warm
| |
4
|
Warm
| ||
5
|
Warm
| ||
6
|
Canary
|
Cold
| |
7
|
Cold
| ||
8
|
Cold
| ||
9
|
Cold
| ||
10
|
Benguela Current
|
Cold
| |
11
|
North Equatorial
|
Warm
| |
12
|
South Equatorial
|
Warm
| |
13
|
Counter Equatorial
|
Warm
| |
14
|
Kuroshio System
|
Warm
| |
15
|
Warm
| ||
16
|
Oyashio
|
Cold
| |
17
|
Cold
| ||
18
|
Cold
| ||
19
|
West Wind Drift
|
Cold
| |
20
|
North East Monsoon
|
Warm
| |
21
|
South West Monsoon
|
Warm
| |
22
|
Indian Counter
|
Warm
| |
23
|
Indian Equatorial
|
Warm
| |
24
|
Warm
| ||
25
|
West Wind drift
|
Cold
|
Currents of Atlantic Ocean :
#
|
Current
|
Type
|
Flows from
|
Deflection
|
1
|
North Equatorial
|
Warm
|
East to West
|
i)
ii) Caribbean Current
Caribbean current enters the Gulf of Mexico and becomes
Antilles Current diverted Northward and flows to east of West Indies islands and helps in formation of ‘
|
2
|
South Equatorial
|
Warm
|
West to East
(
|
i) Northward branch merges with North Equatorial Current near
ii) Second branch turns southward and continues as Brazil Warm Current
|
3
|
Counter-Equatorial Current
|
Warm
|
West to East
|
This current mixes with the equatorial currents in the West but it is more developed in East where it is known as Guinea Stream
|
4
|
Warm
|
North-Easterly
|
The Gulf Stream system largely modifies the weather conditions of the eastern coasts of the
i)
ii)
iii) North Atlantic Drift Current
| |
The origin of the Florida Current is attributed to the piling up of immense volume of water in the
Gulf Stream: The Florida Current after having the water of Antilles current is known as
| ||||
5
|
Warm
| |||
6
|
Canary
|
Cold
| ||
7
|
Cold
|
This current brings with it a large number of big icebergs as far south as
Dense fogs are also produced due to the convergence of Labrador cold current and the
| ||
8
|
Cold
|
South to North
|
This current brings numerous icebergs from the Antarctic area to the South American coast
| |
9
|
Cold
|
Eastward continuation of South Atlantic Drift. Also known as Westerlies Drift or the Antarctic Drift
| ||
10
|
Benguela Current
|
Cold
|
South to North
|
This current merges with South Equatorial Current
|
Currents of Pacific Ocean :
#
|
Current
|
Type
|
Flows from
|
Deflection
|
01
|
North Equatorial
|
Warm
|
Flows in westerly
| |
02
|
South Equatorial
|
Warm
|
East to West
| |
03
|
Counter Equatorial
|
Warm
|
West to East
| |
04
|
Kuroshio System
|
Warm
|
East to West
|
i) Kuroshio current
ii) Kuroshio Extension
iii) North Pacific Drift
iv)
v) Counter Kuroshio current
|
05
|
Warm
|
North to South
|
It raises the temperature of east Australian coast
| |
06
|
Oyashio
|
Cold
|
Flows in southerly
|
Also known as Kurile Cold Current
The convergence of Oyashio current and Kuroshio current causes dense fogs which becomes potential hazardous for navigation
|
07
|
Cold
|
Flows in eastward
| ||
08
|
Cold
|
South to North in western coast of
|
Also called as Humboldt Current
| |
09
|
West Wind Drift
|
Cold
|
West to East
|
One branch enters the Atlantic Ocean through
|
Currents of Indian Ocean :
The current systems of the Indian ocean are largely controlled and modified by landmasses and monsoon winds. Indian Ocean being surrounded by the Indian subcontinent, Africa and Australia does not present most favourable conditions for the development of permanent and consistent system of ocean currents. The current sin the northern Indian Ocean change their flow direction twice a year due to north-east and south-west monsoon winds.
#
|
Current
|
Type
|
Flows
|
Deflections
|
01
|
North East Monsoon
|
Warm
|
From land to ocean during winter season in Northern Hemisphere
| |
02
|
South West Monsoon
|
Warm
|
South west to north east
| |
03
|
Indian Counter
|
Warm
|
Easterly
| |
04
|
Indian Equatorial
|
Warm
|
East to West
|
i) southward deflection is called as Agulhas Current (warm)
|
05
|
Warm
|
East o West
| ||
06
|
West Wind drift
|
Cold
|
Westerly
|
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