Complete study notes on oceanography — warm and cold currents, types of tides, coral reefs, continental shelf, and Exclusive Economic Zone (EEZ). Essential for Kerala PSC Graduate Level exams.
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Oceanography questions appear regularly in Kerala PSC Geography sections. Focus areas include identification of warm vs. cold currents, tide types, and EEZ limits.
1. Ocean Currents — Overview
Feature
Detail
Definition
Large-scale continuous movement of ocean water in a definite direction
Caused by
Wind, temperature differences, salinity differences, Earth’s rotation (Coriolis effect), shape of coastlines
Coriolis effect
Deflects currents to the right in Northern Hemisphere, to the left in Southern Hemisphere
Warm currents
Flow from equator towards poles; raise temperature of coast
Cold currents
Flow from poles towards equator; lower temperature of coast
2. Major Warm Currents
Current
Ocean
Region
Gulf Stream
Atlantic
East coast of North America towards Europe
North Atlantic Drift
Atlantic
Extension of Gulf Stream towards NW Europe
Brazilian Current
Atlantic
East coast of South America
Mozambique Current
Indian
East coast of Africa
Agulhas Current
Indian
SE coast of Africa
Kuroshio (Japan Current)
Pacific
East coast of Japan
North Equatorial Current
All three oceans
Flows westward near equator
South Equatorial Current
All three oceans
Flows westward near equator
Alaska Current
Pacific
Southern coast of Alaska
3. Major Cold Currents
Current
Ocean
Region
Labrador Current
Atlantic
East coast of Canada
Canary Current
Atlantic
NW coast of Africa
Benguela Current
Atlantic
SW coast of Africa
Falkland Current
Atlantic
East coast of southern South America
Oyashio (Kamchatka Current)
Pacific
East coast of Russia/Japan
California Current
Pacific
West coast of North America
Peru (Humboldt) Current
Pacific
West coast of South America
West Wind Drift (Antarctic Circumpolar)
Southern Ocean
Circles Antarctica (largest ocean current by volume)
4. Effects of Ocean Currents
Effect
Example
Warming of coasts
Gulf Stream keeps Western Europe warm despite high latitude
Cooling of coasts
Peru Current keeps Peru/Chile coast cool and dry
Fog formation
Warm and cold current meeting — Grand Banks (Labrador + Gulf Stream)
Rich fishing grounds
Where warm and cold currents meet — Grand Banks, coast of Japan
Desert formation
Cold currents along west coasts — Atacama (Peru Current), Namib (Benguela Current)
El Nino
Warming of eastern Pacific; weakening of Peru Current; global weather disruption
La Nina
Opposite of El Nino; strengthening of cold conditions in eastern Pacific
5. Tides
Concept
Detail
Definition
Periodic rise and fall of sea level caused by gravitational pull of Moon and Sun
Primary cause
Moon’s gravitational pull (Moon is closer, so stronger tidal effect than Sun)
Sun’s tidal force
About 46% of Moon’s tidal force
Tidal cycle
Approximately 12 hours 25 minutes between successive high tides
High tide
Water level rises to maximum
Low tide
Water level falls to minimum
Types of Tides
Type
Cause
Occurrence
Spring tide
Sun, Moon, and Earth in a line (syzygy)
Full Moon and New Moon days; highest tidal range
Neap tide
Sun and Moon at right angles to Earth (quadrature)
First and Third Quarter Moon; lowest tidal range
Perigean tide
Moon closest to Earth (perigee)
Extra-high spring tides
Apogean tide
Moon farthest from Earth (apogee)
Lower than normal spring tides
Importance of Tides
Navigation: ships enter/leave harbours during high tide
Fishing: tidal zones rich in marine life
Tidal energy: potential renewable energy source (e.g., Gulf of Kutch in India)
Cleaning: tides flush out river mouths and harbours
6. Coral Reefs
Feature
Detail
Formed by
Coral polyps (tiny marine organisms) that secrete calcium carbonate
Require
Warm water (20-30 degrees C), shallow depth (less than 50m), clear saline water, adequate sunlight
Cannot grow in
Fresh water, deep water, muddy/polluted water, cold water
Types of Coral Reefs
Type
Description
Example
Fringing reef
Attached to shore; no lagoon or narrow lagoon
Reefs along coast of South Florida
Barrier reef
Separated from coast by wide, deep lagoon
Great Barrier Reef (Australia) — largest in the world
Atoll
Ring-shaped reef enclosing a lagoon; no central island
Lakshadweep Islands, Maldives
Coral Reefs in India
Location
Type
Gulf of Kutch
Fringing reef
Gulf of Mannar
Fringing reef
Andaman and Nicobar Islands
Fringing reef
Lakshadweep Islands
Atolls
Palk Bay
Patchy reef
7. Continental Shelf, Slope, and Ocean Floor
Zone
Depth
Description
Continental Shelf
0 to about 200 m
Gentle slope; extension of continent underwater; richest fishing and mineral zone
Continental Slope
200 m to about 3,000 m
Steep descent from shelf to ocean floor
Continental Rise
3,000 m to about 5,000 m
Gradual slope at base of continental slope
Abyssal Plain
3,000 m to 6,000 m
Flat, deep ocean floor
Ocean Trenches
Beyond 6,000 m
Deepest parts; Mariana Trench = 11,034 m (deepest point — Challenger Deep)
Mid-Ocean Ridges
Variable
Underwater mountain chains; Mid-Atlantic Ridge is longest
8. Exclusive Economic Zone (EEZ)
Concept
Detail
Defined by
UNCLOS (United Nations Convention on the Law of the Sea), 1982
Territorial Sea
Up to 12 nautical miles from baseline
Contiguous Zone
12 to 24 nautical miles
EEZ
Up to 200 nautical miles from baseline
Rights in EEZ
Sovereign rights over natural resources (fishing, mining, oil/gas); not full sovereignty
High Seas
Beyond 200 nautical miles; open to all nations
Continental Shelf claim
Can extend up to 350 nautical miles if geological criteria met
India’s EEZ
Approximately 2.02 million sq km
9. PSC Quick Revision — One-Liners
Gulf Stream warms Western Europe; Labrador Current cools eastern Canada
Warm and cold currents meeting = fog and rich fishing grounds
Spring tides occur during Full Moon and New Moon
Neap tides occur during Quarter Moon phases
Great Barrier Reef (Australia) is the largest coral reef system
Lakshadweep Islands are coral atolls
Mariana Trench (Challenger Deep) = deepest point in the ocean (11,034 m)
EEZ extends up to 200 nautical miles under UNCLOS
India’s EEZ is approximately 2.02 million sq km
Peru (Humboldt) Current is a cold current along South America’s west coast
El Nino = warming of eastern Pacific Ocean
Oceanography questions appear regularly in Kerala PSC Geography sections. Focus areas include identification of warm vs. cold currents, tide types, and EEZ limits.
1. Ocean Currents — Overview
Feature
Detail
Definition
Large-scale continuous movement of ocean water in a definite direction
Caused by
Wind, temperature differences, salinity differences, Earth’s rotation (Coriolis effect), shape of coastlines
Coriolis effect
Deflects currents to the right in Northern Hemisphere, to the left in Southern Hemisphere
Warm currents
Flow from equator towards poles; raise temperature of coast
Cold currents
Flow from poles towards equator; lower temperature of coast
2. Major Warm Currents
Current
Ocean
Region
Gulf Stream
Atlantic
East coast of North America towards Europe
North Atlantic Drift
Atlantic
Extension of Gulf Stream towards NW Europe
Brazilian Current
Atlantic
East coast of South America
Mozambique Current
Indian
East coast of Africa
Agulhas Current
Indian
SE coast of Africa
Kuroshio (Japan Current)
Pacific
East coast of Japan
North Equatorial Current
All three oceans
Flows westward near equator
South Equatorial Current
All three oceans
Flows westward near equator
Alaska Current
Pacific
Southern coast of Alaska
3. Major Cold Currents
Current
Ocean
Region
Labrador Current
Atlantic
East coast of Canada
Canary Current
Atlantic
NW coast of Africa
Benguela Current
Atlantic
SW coast of Africa
Falkland Current
Atlantic
East coast of southern South America
Oyashio (Kamchatka Current)
Pacific
East coast of Russia/Japan
California Current
Pacific
West coast of North America
Peru (Humboldt) Current
Pacific
West coast of South America
West Wind Drift (Antarctic Circumpolar)
Southern Ocean
Circles Antarctica (largest ocean current by volume)
4. Effects of Ocean Currents
Effect
Example
Warming of coasts
Gulf Stream keeps Western Europe warm despite high latitude
Cooling of coasts
Peru Current keeps Peru/Chile coast cool and dry
Fog formation
Warm and cold current meeting — Grand Banks (Labrador + Gulf Stream)
Rich fishing grounds
Where warm and cold currents meet — Grand Banks, coast of Japan
Desert formation
Cold currents along west coasts — Atacama (Peru Current), Namib (Benguela Current)
El Nino
Warming of eastern Pacific; weakening of Peru Current; global weather disruption
La Nina
Opposite of El Nino; strengthening of cold conditions in eastern Pacific
5. Tides
Concept
Detail
Definition
Periodic rise and fall of sea level caused by gravitational pull of Moon and Sun
Primary cause
Moon’s gravitational pull (Moon is closer, so stronger tidal effect than Sun)
Sun’s tidal force
About 46% of Moon’s tidal force
Tidal cycle
Approximately 12 hours 25 minutes between successive high tides
High tide
Water level rises to maximum
Low tide
Water level falls to minimum
Types of Tides
Type
Cause
Occurrence
Spring tide
Sun, Moon, and Earth in a line (syzygy)
Full Moon and New Moon days; highest tidal range
Neap tide
Sun and Moon at right angles to Earth (quadrature)
First and Third Quarter Moon; lowest tidal range
Perigean tide
Moon closest to Earth (perigee)
Extra-high spring tides
Apogean tide
Moon farthest from Earth (apogee)
Lower than normal spring tides
Importance of Tides
Navigation: ships enter/leave harbours during high tide
Fishing: tidal zones rich in marine life
Tidal energy: potential renewable energy source (e.g., Gulf of Kutch in India)
Cleaning: tides flush out river mouths and harbours
6. Coral Reefs
Feature
Detail
Formed by
Coral polyps (tiny marine organisms) that secrete calcium carbonate
Require
Warm water (20-30 degrees C), shallow depth (less than 50m), clear saline water, adequate sunlight
Cannot grow in
Fresh water, deep water, muddy/polluted water, cold water
Types of Coral Reefs
Type
Description
Example
Fringing reef
Attached to shore; no lagoon or narrow lagoon
Reefs along coast of South Florida
Barrier reef
Separated from coast by wide, deep lagoon
Great Barrier Reef (Australia) — largest in the world
Atoll
Ring-shaped reef enclosing a lagoon; no central island
Lakshadweep Islands, Maldives
Coral Reefs in India
Location
Type
Gulf of Kutch
Fringing reef
Gulf of Mannar
Fringing reef
Andaman and Nicobar Islands
Fringing reef
Lakshadweep Islands
Atolls
Palk Bay
Patchy reef
7. Continental Shelf, Slope, and Ocean Floor
Zone
Depth
Description
Continental Shelf
0 to about 200 m
Gentle slope; extension of continent underwater; richest fishing and mineral zone
Continental Slope
200 m to about 3,000 m
Steep descent from shelf to ocean floor
Continental Rise
3,000 m to about 5,000 m
Gradual slope at base of continental slope
Abyssal Plain
3,000 m to 6,000 m
Flat, deep ocean floor
Ocean Trenches
Beyond 6,000 m
Deepest parts; Mariana Trench = 11,034 m (deepest point — Challenger Deep)
Mid-Ocean Ridges
Variable
Underwater mountain chains; Mid-Atlantic Ridge is longest
8. Exclusive Economic Zone (EEZ)
Concept
Detail
Defined by
UNCLOS (United Nations Convention on the Law of the Sea), 1982
Territorial Sea
Up to 12 nautical miles from baseline
Contiguous Zone
12 to 24 nautical miles
EEZ
Up to 200 nautical miles from baseline
Rights in EEZ
Sovereign rights over natural resources (fishing, mining, oil/gas); not full sovereignty
High Seas
Beyond 200 nautical miles; open to all nations
Continental Shelf claim
Can extend up to 350 nautical miles if geological criteria met
India’s EEZ
Approximately 2.02 million sq km
9. PSC Quick Revision — One-Liners
Gulf Stream warms Western Europe; Labrador Current cools eastern Canada
Warm and cold currents meeting = fog and rich fishing grounds
Spring tides occur during Full Moon and New Moon
Neap tides occur during Quarter Moon phases
Great Barrier Reef (Australia) is the largest coral reef system
Lakshadweep Islands are coral atolls
Mariana Trench (Challenger Deep) = deepest point in the ocean (11,034 m)
EEZ extends up to 200 nautical miles under UNCLOS
India’s EEZ is approximately 2.02 million sq km
Peru (Humboldt) Current is a cold current along South America’s west coast