5.2 World fisheries Flashcards
Ocean structure
Continental shelf- shallowest part of a continental margin
continental slopes- where seafloor drops away quickly on edge of continental crust
continental rise- gentle slope at the base of continental slope
ocean floor
Distribution of major fish populations are found in
They are found in shallow continental shelves
Why continentental shelf can be rich in fisheries?
- it recieves more sunlight
- large abundance of oxygen
- large abundance of phytoplankton
- Abundance of CO2 for phtotsynthesis by phytoplankton
- Due to phaytoplankton on continental shelf it means abundance of food
Surface currents
movement of the surface water of the sea in a constant direction.
Warm ocean currents-
warm water is moving from the tropics towards poles
Cold ocean current-
water from colder areas is moving from poles towards the equator.
Prevailing wind:
the direction from which the wind nearly always blows in a particular area.
Circulation of ocean currents in north of the equator
current circulations are mainly clockwise.
Circulation of ocean currents in south of the equator
South of equator, the circulation of currents in all three oceans ( Pacific, Indian, Antarctic) is mainly anticlockwise.
example of cold current
peru current (beside S USA)
west australia current
example of warm current
South equatorial current
east australia current
factors affecting ocean currents
1) temperature of water
2) prevailing winds
3) rotation of earth (due to rotation, currents move clockwise in north hemisphere, anticlockwise in southern hemisphere)
4) Salinity of water: higher the salinity warmer the currents
Upwelling
- areas where minerals at the ocean floor (cold current) are brought up to the surface by currents.
- This layer is rich in nutrients which results in higher productivity
KEY TERMS- cold currents, upwelling, more nutrients, more phytoplanktons, more fishes
Downwelling
is where surface water (warm currents) is forced downwards, where it may deliver oxygen to deep water, downwelling leads to reduced productivity, as it extends the depth of nutrient-limited layer
KEYTERMS- Warm currents, downwelling, less nutrients, less phytoplanktons, less fishes
effect on climate of cold currents-
cold and dry, drought,
fog and mist