3.1.4.1 Glaciers as natural systems Flashcards

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1
Q

Inputs

A
Energy 
- solar radiation 
- geothermal heat
Mass 
- direct snowfall 
- blown snow 
- avalanches and rock fall
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2
Q

Components

A
  • Depositional landforms and landscapes
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3
Q

are Glacial environments open systems?

A

yes

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4
Q

flows/transfers

A
  • ice movement
  • erosional processes
  • ice and meltwater transport
  • melting
  • sublimation
  • calving
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5
Q

positive feedback in a cold environment

A

arctic ice melts - land and water surfaces are exposed - these darker and dull surfaces have low albedo - exposed land and sea reflects less solar radiation than ice - more solar radiation is absorbed causing the surfaces to warm - arctic ice melts.

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6
Q

Permafrost

A

Permanently frozen ground, found in polar and tundra regions.

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7
Q

Polar

A

The regions of Earth surrounding the North and South Poles. These regions are dominated by Earth’s polar ice caps, the northern resting on the Arctic Ocean and the southern on the continent of Antarctica.

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8
Q

tundra

A

The flat, treeless Arctic regions of Europe, Asia and North America, where the ground is permanently frozen. Lichen, moss, grasses and dwarf shrubs can grow here.

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9
Q

25%

A

The amount of the World’s land surface that are Cold environments cover.

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10
Q

latitude

A

One of the main controlling factors of how cold a place is and what cold features an area has is. At extreme latitudes, there are Ice sheets in areas of extreme cold such as Antarctica

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11
Q

Arctic

A

Northern polar region composed largely of sea ice, which changes in thickness and extent from month to month and year to year.

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12
Q

66.5°N

A

The Arctic circle

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13
Q

66.5°S

A

The antarctic circle

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14
Q

Nuntaks

A

ice-free areas in polar environments

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15
Q

tundar

A

from sami (northern finland) and the original word means “uplands” and “treeless mountain tract”

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16
Q

tundra areas

A

cover approximately 1/5 of the world’s land surface, including parts of Northern Canada and Russia.

17
Q

Active layer

A

The layer that thaws at the surface of the permafrost in the Tundra.

18
Q

Tundra climates

A

very harsh in winter, the precipitation falls as snow and although the average temperatures are -25°C in some months the daily minimum can be much lower, dropping below -40°C. Soils also freeze during these months, making life for most plants during this time impossible.

19
Q

polar climates

A

classed as a cold desert, there is very little precipitation as the air cannot hold much water vapour as it is so cold. The precipitation that does fall does so as snow and ice. Average temperatures are always below freezing point, but daytime summer temperatures can exceed 0°C.