Term 2 - Theme 3 (1) Flashcards

1
Q

Observed sea level has increased around

A

10cm since 1970s.

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2
Q

Glaciers are driven by climate

A

Snow and ice accumulation, ablation through radiative forcing.

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3
Q

IPCC, 2001 + 2007

A

glaciers re the clearest indicators of what is currently happening to the climate of the earth… the fact that they are thinning and retreating at historically unprecedented rates should be a concern to us all.

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4
Q

Mass balance equation

A

MB = accumulation - ablation (-iceberg calving)

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5
Q

The cryosphere consists of

A

Northern hemisphere - Greenland, Arctic glaciers, Alaska, alps, himalayas (7m potential SLR).
Southern hemisphere - Antarctica - 57m potential SLR and the andes.

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6
Q

Change in glacier length

A

indirect, delayed sign of change in climate

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7
Q

Air temperature role

A

Related to radiation balance and solid/liquid precipitation ratio.

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8
Q

Climatic sensitivity of a glacier depends on

A

local topographic effects.

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9
Q

Response/lag time

A

Occur because the signal must be transferred from accumulation area to the snout of the glacier.

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10
Q

Response/lag time controlled by

A

glacier size, gradient and flow velocity. Lay, low gradient, slow glaciers will have a long lag time. Short, steep and fast glaciers will have a short lag time.

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11
Q

Monitoring frontal variations of glaciers

A

Direct measurement, image comparison.

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12
Q

Mass balance measurement of glaciers

A

Direct measurements of accumulation and ablation, remote sensing methods.

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13
Q

Global glacier changes (length)

A

General glacier recession shown in Little Ice Age. Intermittent readvances on decadal timescales. Strong glacier retreat in the 1920s and 1940s.

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14
Q

Glacier frontal variations

A

Most visible component of glacier response to climate change. May be studied over long time scales. All related to changes in total glacier mass balance.

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15
Q

global glacier change (mass balance)

A

mass balance is the different between mass gained and mass lost. Mountain glaciers are losing mass all the time + this has increased in the last decade.

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16
Q

Glacier fluctuation - Africa

A

occur on Rwenzari, Mount Kenya and Kilimanjaro In 1906 Rwenzari had 43 glaciers with a total area of 7.5km2. By 2005, this was about 1.5km2.

17
Q

Glacier fluctuations - New Zealand

A

Most glaciers located along the Southern Alps . Overall retreat over the past 150 years, with intermittent Alpine radius in the 1890s, 19202, 70/80s and 1985. Ice cover estimated to have diminished by about 35% from 1850 to 1970s and another 22% by 2000.

18
Q

Glacier fluctuations - Antarctica

A

Majority of glaciers and ice caps located on the Antarctic Peninsula. Cook et al (2005) showed that 87% of the glaciers have retreated over the last 6 decades. Glaciers on S Georgia receded overall since 9th Century.

19
Q

Antarctic glacier change

A

Increasing atmospheric + oceanic temp. Air temps rose by 2.5 degrees in the northern antarctic peninsula. 1950-2000. Collapse of ice shelves. Acceleration of ice streams + outlet glaciers.

20
Q

Glacier surface lowering

A

More surface lowering in the north related to greater temp increases. The thinning is likely to be related to glacier acceleration and increasing calving rates.

21
Q

Prediction of future glacier changes are important for

A

understanding contribution to SLR, Managing water resources, mitigation against hazards such as GLOFs.

22
Q

Prediction of future changes difficult due to

A

Uncertainty of future climate scenarios. Uncertainty as to how glaciers will retreat in future changes in climate. Local factors such as aspect and sliding.

23
Q

Equilibrium line altitude (ELA) increased

A

in a warmer climate.

24
Q

Prediction: topography

A

Steeper glaciers more likely to survive longer into a period of continental warming. Rise in eLA translated to a smaller zone of ice transferring from the accumulation to ablation zone.

25
Q

The WAIS: marine ice sheet instablility

A

Major concern about the West Antarctic ice sheet size -much of the sheet is below sea level.

26
Q

Nesje, A + Dahl, S, O (2000) the equilibrium line altitude marks

A

the area or zone on the glacier where accumulation is balanced by ablation.

27
Q

Kieffer et al, 1994

A

The EOS has been developed to build uniform database of most glaciers in the world and monitor changes in glaciers on a periodical basis.

28
Q

Paterson, 1994

A

The response time is defined as the time a glacier takes to adjust to a change in mass balance.

29
Q

Johannesson et al, 1989

A

The response time is defined as the time a glacier takes to adjust to a change in mass balance.

30
Q

During the Quarternary glacial periods, ice sheets were extensive, covering bout

A

30% of the Earth’s land area.