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Lecture 19: Orbital Variations in Ice Sheets

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Presentation on theme: "Lecture 19: Orbital Variations in Ice Sheets"— Presentation transcript:

1 Lecture 19: Orbital Variations in Ice Sheets
Chapter 9 (p ) This lecture was prepared on 1/23/2005 (Sunday). Took me 5 hours (from 8:00pm to 1:00am)

2 Orbital-Scale Control of Ice Sheets
Ch. 10, p 18000 yrs ago, ice sheets surrounded much of the Arctic Ocean. Today, ice sheets exist only on Greenland. Tectonic-scale cooling caused ice sheets to appear, but why did they grow and melt over (the shorter) orbital-scales?

3 What Controls the Size of Ice Sheets
Ice sheets exist because ice accumulates more than melts. Both depend on temperature  insolation  season Summer insolation controls the size of ice sheets.

4 Ice Growth and Decay: Force and Response
Delayed bedrock sinking  + feedback to ice growth Ice sheets lags behind summer insolation forcing - - Delayed bedrock rebounding  + feedback to ice decay


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