IB Geography: Extreme Environments

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What is a polar environment? And where?

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127 Terms

1

What is a polar environment? And where?

- Year round permanent snow/ice.
-In the high latitudes above 65-70*N and some parts of the southern hemisphere

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2

What is a glacial environment?

An area covered with snow and ice on a long term basis, where glacial process operate

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3

What is periglacial/tundra? And where?

- Areas found on the edge of glaciers or ice masses.

-Intense freeze-thaw cycles
- High latitudes and altitudes. eg Himilayas, Andies and Rockies

-Cover ¼ of the earth

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4

What is freeze thaw action?

The freezing and subsequent thawing of water

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5

Other than areas with a high latitude. where can snow/ice be found?

In mountains in non-tropical latitudes, where the altitude is so high that there is year round ice and snow

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6

How does Köppen-Geiger Climate Classification work?

Each country is coloured, depending on temperature, and given a letter based on its climate, precipitation and temperature

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7

Where are most glaciers found?

In Greenland, on the coast of South America and North America and in high mountains

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8

Polar characteristics (5)

- Year round permanent snow/ice
- Always below 0*C
- Precipitation below 200mm
- Extreme seasonality
- Flat relief

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9

Periglacial/tundra characteristics (5)

- Seasonal ice cover
- High precipitation
- Tundra biome
- Sporadic/discontinuous permafrost
- Usually flat relief, up to 12 degree gradient

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10

High mountains characteristics (5)

- Year round permanent snow/ice
- Cold all year due to altitude/snow line
- Extreme diurnal temp variation
- Limited biological activity
- High relief

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11

What is a glacier?

  • A huge mass of ice + compacted snow slowly flowing over land mass

  • in an area where snow accumulation exceeds melting and sublimation

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12

What is sublimation?

solid to gas

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13

What is the snow line?

The point above which snow and ice forms on a mountain

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14

Why is the snow line higher in hot countries?

Because you need to go higher up to reach temperatures cold enough for snow to form

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15

What are glaciers made of?

Fallen snow that has compacted into large thickened ice masses

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16

What is firn?

Snow that has survived one season

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17

What is ice?

Interconnected air pockets become sealed off, isolating any air into separate air bubbles

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18

How much of the earth surface is taken up by glaciers?

10%

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19

Why is the amount of solar radiation received by the Earth not distributed evenly?

Because the Earth is titled at an axis of 23.5 so when the earth rotates the sun doesn't hit the earth evenly

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20

What in insolation?

The solar radiation that reaches the earth's surface

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21

What is albedo?

The reflectivity of a surface

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22

Which is the most defective surface?

Dense, dry clean snow

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23

What is the albedo of snow?

86-95

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24

EG : low latitude but high altitude

Himalayas in Nepal - very close to equator but also very cold

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25

What is environmental lapse rate?

The temperature decreases by 6.5°C for about every 1000m you go up

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26

Why is air colder as you go up?

The pressure is lower, so is unable to hold as much heat

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27

Why does the tricellular model occur?

  • There is an uneven distribution of insolation

  • if this isn't corrected then the tropics would become too hot and the polar regions would be too cold

  • so the planet redistributes this heat to find an equilibrium

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28

How does the tricellular model work?

Warm air from the equator rises and cold air sinks, this forms a convection current, which triggers two other convection currents either side, distributing the heat from the equator to the polar regions

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29

What happens when warm air rises?

Low pressure and rainfall

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What happens when cold air sinks?

High pressure and lack of rainfall

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31

Where is the Hadley cell?

Nearest the equator

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32

Where is the Ferrel cell?

In the middle between latitudes 30-60°

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33

Where is the polar cell?

Nearest the polar regions

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34

Four main factors that affect the location of a desert

1. Pressure conditions
2. Distance from the sea
3. Rain shadow effect
4. Proximity to cold upwelling currents

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35

What is a fold mountain?

Mountain ranges that are formed at either a destructive or conservative plate boundary

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36

How are fold mountains formed?

Through orogeny. When an area of sea separates two plates, sediment settles and compresses becoming sedimentary rock. The plates then move towards each other and the rock folds

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37

What is a geosyncline?

A depression in the sea floor

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38

What is permafrost?

Ground that remains frozen and stays at or below 0°C for two or more years

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39

What is alpine or mountain permafrost? Example?

- Permafrost found in low latitude regions with a high elevation
- Andes

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40

What affects the thickness of permafrost? (5)

- Snow cover
- Temperature of air near the ground
- Vegetation cover
- Bodies of water (higher soil water content)
- Heat from the interior of the Earth

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What is the active layer of permafrost?

The uppermost ground layer which thaws in the summer and freezes in the winter

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42

How is vegetation affected by the active layer of permafrost?

Plants can only grow within the active layer, as the roots are unable to break through the foreign ground beneath the layer

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43

What is talik?

The layer of unfrozen ground below a lake

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44

What are the types of permafrost?

- Continuous
- Discontinuous
- Extensive
- Sporadic

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45

What is continuous permafrost? Location?

- Where permafrost is found underlying nearly all of the landscape, except under lakes that don't freeze all the way to the bottom
- In regions with severe winter and temperatures below freezing

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46

What is discontinuous permafrost? Location?

- Permafrost that doesn't continuously cover an area - there are areas of unfrozen ground
-Regions with annual temperature slightly below 0°C

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47

Location of extensive discontinuous permafrost ?

Mean annual temperature ranges between 2°C and -4°C

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48

What is sporadic permafrost? Location?

- Permafrost that is found in isolated patches or islands
- Areas where the mean annual temperature ranges between 0°C and -2°C

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49

Why are high mountains difficult for human habitation? (3)

- Risk of landslides and avalanches
- Too cold
- Only a thin layer of soil so difficult for farming

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50

How do polar iceberg pose a threat to shipping lanes? Example?

- Icebergs break off and straying to areas where they aren't expected to be - can sink ships
- Large iceberg (80km long and 40km wide) broke off Larsen Ice Shelf in Antarctica

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51

Challenges due to cold temperatures in periglacial climates (5) 🌱 💧 🏚 🚽

- Low temperature reduce plant growth
- Long hours of darkness can limit plant growth
- Ground tends to be waterlogged
- Building construction can cause the ice to melt causing subsidence
- Makes it difficult to provide services such as water and sewage disposal

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52

What is subsidence?

When the ground sinks

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53

How have people adapted to living near glaciers? (3)

- Drinking water
- Irrigation
- People generate HEP from melt water

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54

Factors that affect population density (8)

- Climate
- Access
- Resources
- Facilities
- Remoteness
- Altitude
- Hazardous conditions
- Communication

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55

Types of periglacial regions

Arctic continental, Alpine and Arctic maritime

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56

What is pattered ground? Location?

- When rocks and pebbles line up on the ground to form a pattern
- S Iceland

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57

How does patterned ground form?

Underneath pebbles in the ground is an ice lens, and in the night when temperatures drop, this ice lens freezes and expands, pushing the pebble up. Eventually these pebbles reach the ground surface and roll down slopes, forming a pattern

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58

What are pingos? Size?

- Ice cored mounds that rise above a flat plain that consists of silt and sand
- Up to 60-70m

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59

Where are open system pingos formed? Eg?

- In valley bottoms
- E Greenland

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60

Where are closed system pingos found? Eg?

- Beneath lake beds
- Mackenzie delta, Canada

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61

What happens when a pingo collapses?

An incision is left behind and filled as a pond

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62

How do open system pingos form?

Water collected in a valley bottom with an area of talik, and water seeps into the talik. When temperatures drop, the talik expands and pushes the surface into a dome forming a pingo

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63

How do closed system pingos form?

Under a lake there will be talik, and when the lake drains this talik is exposed to the cold and thus shrinks. The water becomes concentration within the talik and freezes to form a lump of ice which forms a pingo

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64

What is thermokarst?

Irregular surfaces of marshy hollows and small hummocks formed by freezing and thawing, and subsequent subsidence

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65

What is plucking? Where does it occur?

- When meltwater from a glacier freezes around a lump of rock, and when the ice moves downhill the rock is ripped from the back wall
- Base and sides of glacier

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66

What is abrasion?

When rock frozen to the base and back of a glacier scratches the bed rocks leaving striations

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67

What is basal debris?

Debris at the base of the glacier

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68

What affects the rate of erosions processes? (4)

- Presence of basal debris
- Underlying geology
- Ice thickness
- Debris size and shape

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69

Where are cirques found?

- North or east facing slopes of mountains
- Accumulation is greater than ablation

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70

How are cirques formed?

1. A periglacial hollow is enlarged by freeze thaw and removal by snow melt
2. Ice accumulates in this hollow
3. Having reached a critical weight, the ice moves out in a rotational manner, eroding the floor by plucking and abrasion
4. Meltwater trickling down allows the cirque to grow by freeze thaw

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71

Bergschrund

A crevasse at the head of a glacier

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72

Crevasse

A deep crack or fissure in the ice of a glacier

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73

Arête

A jagged, narrow ridge that separates two adjacent glacier valleys or cirques

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74

Truncated spurs

Eroded triangular shaped cliffs in glaciated valleys

<p>Eroded triangular shaped cliffs in glaciated valleys</p>
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75

Ribbon lakes

Long thin lake that fills the floor of a glaciated valley

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76

Hanging valley

u-shaped valley left by a melted tributary glacier that enters a larger glacial valley above its base, high up on the valley wall

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77

Lateral moraine

Moraine along the side of a glacier

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78

What is meant by drift?

All the glacial and fluvioglacial deposits left after the ice has melted

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79

Characteristics of glacial deposits

- Angular
- Unsorted
- Mixed sizes and rock type
- Striations

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80

Erratics

Boulders transported by a glacier with foreign geology

<p>Boulders transported by a glacier with foreign geology</p>
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81

Drumlin

A long mound of till that is smoothed in the direction of the glacier's flow

<p>A long mound of till that is smoothed in the direction of the glacier's flow</p>
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82

Medial moraine

- A moraine formed when two valley glaciers come together to form a single ice stream
- Forms in the middle of the glacier

<p>- A moraine formed when two valley glaciers come together to form a single ice stream<br>- Forms in the middle of the glacier</p>
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83

Up valley of a moraine

Side of the moraine in contact with the ice, usually the steeper side

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84

Frost heave

When water freezes and it pushes particles in the soil upwards

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85

Solifluction

The slow, downslope flow of soil saturated with water in areas surrounding glaciers at high elevations

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86

Thermokarst

Depressions caused by the melting of permafrost

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87

How can human activity lead to thermokarst?

Fires, removal of vegetation

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88

Rain shadow effect

A side of the mountain that is kept dry and shielded by the mountain

<p>A side of the mountain that is kept dry and shielded by the mountain</p>
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89

Physical factors increasing the chance of a flash flood in hot environments? (3)

- High intensity rainfall
- Impermeable land
- Lack of vegetation

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90

Human factors that cause desertification (5)

- Overgrazing
- Mismanagement of water supplies
- Deforestation
- Over population
- Global warming

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91

Reasons why people are in hot arid areas

- Tourism
- Jobs
- Resource abundance (Mining/mineral deposits e.g. uranium mining in Niger)/Aquifers
- Family + friends
- Military
- People enjoy the hot environment

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92

Wadis

Dry gullies that have been eroded by flashfloods

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Alluvial fan

Cones of sediment deposited by rivers when they move from the mountains to an open plain

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94

Yardangs

Wind eroded rocks, where alternating vertical strata of hard and soft rocks produce a series of ridges

<p>Wind eroded rocks, where alternating vertical strata of hard and soft rocks produce a series of ridges</p>
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95

Zeugens

Wind eroded rock structures consisting of horizontal layers of hard and soft rock

<p>Wind eroded rock structures consisting of horizontal layers of hard and soft rock</p>
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96

Barchan Dunes

Solitary crescent-shaped mounds of sand with downwind pointing tips. Occur when there is a limited sand supply, little vegetation and constant wind direction

<p><u>Solitary crescent-shaped </u>mounds of sand with <u>downwind pointing tips</u>. Occur when there is a <strong>limited sand supply, little vegetation and constant wind direction</strong></p>
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97

Types of weathering in the desert

Salt crystallisation and disintegration

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98

Salt crystallisation

Breakdown of rock by solutions of salt:
in temps around 26-28C sodium sulphate and sodium carbonate expand by 300%, and when the water evaporates this salt leaves pressure on the rock

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99

Disintegration

Similar to freeze thaw

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100

Exotic river

Comes from a different climate zone

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