Names and topic Flashcards

1
Q

Benn and Lehmkuhl

A

2000

glacier systems and mass balance
- ELAs, MBs and debris

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2
Q

Hock

A

2005

glacier systems and mass balance
- modelling, snow melt and the atmosphere, albedo

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3
Q

Jacob et al

A

2012

glacier systems and mass balance
-1.5mm/yr total contribution to SL rise, GRACE

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4
Q

Nakawo and Young

A

1982

glacier systems and mass balance
- albedo and debris

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5
Q

Braithwaite

A

2002

glacier systems and mass balance
- MB and hydrology, contribution to mean SL

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6
Q

Radic and Hock

A

2011

glacier systems and mass balance
- contributions of SL rise

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7
Q

Bjornsson

A

1992

water in glaciers
- jokulhaulps

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8
Q

Holmlund

A

1988

water in glaciers
- moulins and crevasses

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9
Q

Gulley and Benn

A

2009

water in glaciers
- conduit formation and heat dissipation

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10
Q

Zwalley et al

A

2002

water in glaciers
- coupling of surface melting and ice sheet flow

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11
Q

Sorg et al

A

2012

Water in glaciers
- G run off, Tien Shan

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12
Q

Nienow

A

1998

Water in glaciers
- d’Arolla, development of efficient channel system by end of melt season

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13
Q

Menzies

A

2002

water in glaciers
- meltwater origins and causes

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14
Q

Fountain and Walder

A

1998

water in glaciers
- water flux and storage

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15
Q

Alley et al

A

1986

glacier flow
- WAIS till deformation beneath ice stream

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16
Q

Bamber et al

A

2000

glacier flow
- complex flow of interior antarctic ice sheet

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17
Q

Engelhardt and Kamb

A

1998

glacier flow
- basal sliding, WAIS

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18
Q

Harrison and post

A

2003

glacier flow
-surging

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19
Q

Kamb et al

A

1985

glacier flow
- Variegated glacier, surging

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20
Q

Benner

A

2003

glacier flow
- ice streams

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21
Q

Stokes et al

A

2007

glacier flow
- sticky spots

22
Q

Joughin and Alley

A

2011

marine terminating glaciers
- WAIS retreat

23
Q

Alley et al

A

2005

marine terminating glaciers
- Greenland and Antarctica loss

24
Q

Howat et al

A

2007

marine terminating glaciers
- Greenland calving and tidewater glaciers

25
Q

Shepherd et al

A

2001

marine terminating glaciers
- PIG retreat

26
Q

Van der Veen

A

2002

marine terminating glaciers
- calving

27
Q

Benn et al

A

2007

marine terminating glaciers
- calving rates

28
Q

Favier et al

A

2014

glacier and ice sheet modeling
- PIG instability

29
Q

Gladstone et al

A

2012

glacier and ice sheet modelling
- PIG prediction using flow line and box model

30
Q

Nick et al

A

2009

glacier and ice sheet modelling
- Greenland thinning

31
Q

Vaughan and Arthern

A

2007

glacier and ice sheet modelling
- difficulty of predicting ice sheets

32
Q

Alley et al

A

2003

glacier erosion processes
- effect of water, slope and till on erosion

33
Q

Benn and Evans

A

2010

glacier erosion processes
- different scales of erosional landforms, models of friction

34
Q

Bennet and Glasser

A

2009

glacier erosion processes
- glacial abrasion (Boulton model, Hallet model), G plucking and G MW erosion

35
Q

Bennett and Glasser

A

2009

landforms and landscapes of G erosion
-each feature in lecture

36
Q

sudden and John

A

1976

landforms and landscapes of G erosion
-general

37
Q

Greenwood et al

A

2007

landforms and landscapes of G erosion
-MW channels in British ice sheet

38
Q

Boulton

A

1979

landforms and landscapes of G erosion
-deformable or resistant substratum

39
Q

Boulton and Hindmarsh

A

1987

landforms and landscapes of G erosion
-horizon A and B

40
Q

Benn and Evans

A

1998

Land forms and landscapes
- 4 types of small scale erosional forms: striae, rat tails, gouges/fractures/chattermarks, P forms

41
Q

Dreimanis

A

1953

Land forms and landscapes
- gouges/fratucres/and chatter makes fracture plans can be used to infer ice direction

42
Q

Dahl

A

1965

Land forms and landscapes
- P forms originally thought to be produced by abrasion of plastically deforming ice (debris rich?)

43
Q

Kor et al

A

1991

Land forms and landscapes
- non-generic term ‘s-form preferred’ (than p form as ‘sculptured’), meltwater movement through bed

44
Q

Shaw

A

1988

Land forms and landscapes
- fluvial explanation of S (/P) bedforms !!
morphological similarity to scour marks eroded by water, due to overall appearance from a distance
- tortuous appearance: ice doesn’t flow like that, must be MW
- scour mark appearance: analogues to fluvial bedrooms
- striated surface: ice erosion occurred afterwards

45
Q

Goldthwaite

A

1979

Land forms and landscapes
- striae were created after the p-forms

46
Q

Boulton

A

1974

Land forms and landscapes
- ice erosion explanation for P/(S) forms!!
P forms observed with debris rich basal ice in situ
- scour mark appearance: fluvial erosion occurred afterwards
- striated surface: can not be formed by MW
- tortuous appearance: evidence of ice flowing like that in situ

47
Q

Rea and Whalley

A

1994

Land forms and landscapes
- P forms associated with ice turning corners

48
Q

Sugden et al

A

1992

Land forms and landscapes

  • RMs tend to form under thin ice with fluctuating water pressures
  • Bed rock structure important
49
Q

Roberts et al

A

2005

Land forms and landscapes
- bedrock structure importantt to RMs

50
Q

Lane et al

A

2014

Land forms and landscapes
- bedrock structure important to RMs