Week 4 references Flashcards

1
Q

Equation for water-depth calving model

A

Brown 1982

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2
Q

Crevasse-depth calving model

A

Benn et al 2007

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3
Q

Ice discharge increases with water depth b/c greater space for ice to flow through and claving/flotation rate higher

A

Weertman 1973

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4
Q

If bed deepens inland, catastrophic ‘unstable’ retreat can potentially occur

A

Thomas 1979 and others

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5
Q

Theoretical (mathematical) analysis of MISI

A

Schoof 2007

Joughin and Alley 2011

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6
Q

Once one lake drains it forms a chain reaction

A

Banwell et al 2013

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7
Q

Larsen B ice shelf, Antarctica: Loss of back stress causes acceleration and thinning of tributaries

A

Rignot et al 2004

Hulbe et al 2008

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8
Q

Larsen B ice shelf, Antarctica: pre-collapse, rapid thinning of ice shelf in previous decade 30cm/yr

A

Shepherd et al 2003

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9
Q

Larsen B ice shelf, Antarctica: post collapse instantaneous speed up of glaciers inland

A

de Rydt et al 2015

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10
Q

Outlet changes in Greenland; Jakoshavn Isbrae

Arrival of warm ocean water coincides with beginning of acceleration

A

Holland et al 2008

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11
Q

Outlet changes in Greenland; Jakoshavn Isbrae

warm water makes contact with ice and changes Fjord circulation

A

Straneo 2010

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12
Q

Pine Island Glacier: basal melting has been confirmed by satellite altimetry observations = primary control of Antarctic ice-sheet loss

A

Pritchard et al 2012

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