Ocean Currents, Tides, Coral Reefs, Continental Shelf & EEZ
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.
▶ മലയാളത്തിൽ വായിക്കുകComplete 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
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