5.2 World fisheries Flashcards

1
Q

Ocean structure

A

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

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2
Q

Distribution of major fish populations are found in

A

They are found in shallow continental shelves

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3
Q

Why continentental shelf can be rich in fisheries?

A
  • 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
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4
Q

Surface currents

A

movement of the surface water of the sea in a constant direction.

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5
Q

Warm ocean currents-

A

warm water is moving from the tropics towards poles

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6
Q

Cold ocean current-

A

water from colder areas is moving from poles towards the equator.

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7
Q

Prevailing wind:

A

the direction from which the wind nearly always blows in a particular area.

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8
Q

Circulation of ocean currents in north of the equator

A

current circulations are mainly clockwise.

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9
Q

Circulation of ocean currents in south of the equator

A

South of equator, the circulation of currents in all three oceans ( Pacific, Indian, Antarctic) is mainly anticlockwise.

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10
Q

example of cold current

A

peru current (beside S USA)
west australia current

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11
Q

example of warm current

A

South equatorial current
east australia current

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12
Q

factors affecting ocean currents

A

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

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13
Q

Upwelling

A
  • 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
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14
Q

Downwelling

A

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

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15
Q

effect on climate of cold currents-

A

cold and dry, drought,
fog and mist

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16
Q

effect on climate of warm currents-

A

warm and heavy rainfall

17
Q

El Niño Southern Oscillation (ENSO) meaning:

A

the change in the prevailing winds that leads to change in the pattern of currents in the oceans of the South Pacific.

18
Q

Effect of EL Nino southern oscillation (ENSO):

A
  • Warm nutrient-poor water comes into the region from the equator.
  • Results in no upwelling of the cold, nutrient-rich water that supports the anchovy fishery(Peruvian).
  • No nutrients mean the phytoplankton do not grow well, so there’s less food for the fish, resulting in fewer fisheries as they migrate somewhere else
  • The effects of El-Nino include the reversal of wind patterns across the Pacific, drought in Australia, and unseasonal heavy rain in South America.
  • Much of the production of the anchovy fishery was used for fishmeal which is used to feed farmed fish, thus countries where this is important, are affected by a crash in the anchovy fishery.