Slope and ocean tings Flashcards

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1
Q

Slope elements + characteristics

A

Crest - horizontal shape - lies on top of hill - soil creep, 0 degrees
Free face - almost vertical slope - mass wasting + undercutting, 90 degrees, sheer cliffs + falls
Talus slope - concave - 35 degrees, deposition+erosion of litter(large rocks) and scree(small rocks), 35 degrees
Knick Point between Talus slope and Pediment
Pediment - Concave slope - abrasion + attrition of small pebbles. Deposition, 0-5 degrees

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2
Q

Parallel slope retreat

A

slope angle and length remains constant and retreats parallel to
itself. pediment increases in length over time.

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3
Q

Major oceans

A

Pacific, Atlantic, arctic, indian

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4
Q

Importance of oceans

A

Moisture for the atmosphere

Renewable oxygen supply for the atmosphere

Protein foods

Energy supply

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5
Q

Renewable o2?

A

Can hold a lot of o2, allows o2 transfer between water and air, greenhouse gases like co2 make it harder o2 gaseous exchange

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6
Q

Ocean as protein

A

Fish major contributor to protein. Fish require plankton which survive conditions rich in nitrates and phosphates and have an abundance of sunlight. These favorable nutrients found eastern side of boundary currents like the Benguela. These currents typically flow near ocean floor and due to upwelling creates good environment for fish

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7
Q

Ocean as energy

A

Tidal Power

Wind Turbines in oceans

Oil and gas from oceanic areas

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8
Q

Ocean currents

A

Warm - Agulhas, Kuroshio(near jpn), N atlantic drift, E australian etc
Cold - Benguela, Oyashio(jpn) , Peru, Canary

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9
Q

Ocean Gyre

A

large system of circular o currents formed by global wind patterns and Coriolis force. Movement of gyres circulates o water around planet

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10
Q

Oceanic circulation

A

As result of salinity changes in ocean which affects water density(due to increased rainfall, temp etc) natural drift in oceans.Less saline tropical water filters down to more saline nutrient rich polar
waters.

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11
Q

Thermohaline circulation

A

Begins in polar regions. Ocean water gets very cold, sea ice forms, surrounding water saltier , increases in density and sinks. Winds drive ocean currents in the upper 100 meters of the ocean’s
surface.

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12
Q

Upwelling

A

Wind blows along shore, Ekman transport pushes surface water out to sea, upwelling along coast, Where the warm surface wind meets the cold upwelled water fog will occur due to condensation.

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13
Q

Air masses that originate over oceans

A

Maritime air masses

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14
Q

Role of oceans in moderating temp

A

Ocean receives same amount of insolation as land but water high albedo so most gets reflected. Oceans retain heat longer than land but take twice as long to heat up due to water temp being twice as much as land. Ocean currents + tides distribute heat over large area

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15
Q

Anomalies in terms of oceans

A

Positive anomaly - ocean current temp higher than actual temp of region
negative - opposite of positive

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16
Q

Role of oceans in world trade

A

Transport of goods. primary resources, manufactured goods, oil etc traded in containers. Man made canals, trade routes

17
Q

Problems with oceans as world trade

A

Water pollution(oil, lead , sewerage etc)

18
Q

Oceans as climate controllers

A

Oceans have moderating effect on temp, they affect temp and rain

19
Q

Short def of upwelling

A

Cold water from deep thermohaline circulation rises to surface

20
Q

Impacts of La Nina

A

Subsidence and drier conditions in Africa and result in better rains but can also result in more flooding.

21
Q

Impacts of El Nino

A

rising air and wetter conditions. El nino events occur every few years and in between conditions are normal. can cause devastating droughts.

22
Q

ENSO

A

El Nino Southern Oscillation