| 1 |
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Is the World's Ice Disappearing? |
2 |
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Quite Simply:
YES
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| 3 |
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Last Glacial Maximum vs Present |
4 |
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Human / Ice Dependency |
| 5 |
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So WHERE is Earth's ice? |
6 |
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Types of Ice |
| 7 |
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An Idealized Cryosphere System |
8 |
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Accumulation and Depletion |
| 9 |
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Mass Balance |
10 |
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Mass Balance & Warning Temperatures? |
| 11 |
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Mass Balance: Retreat |
12 |
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Mass Balance: Retreat |
| 13 |
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Meltwater Runoff |
14 |
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Meltwater Runoff |
| 15 |
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Atmospheric Feedbacks |
16 |
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Biological Impact |
| 17 |
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Cryosphere Systems are IMPORTANT |
18 |
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Short and Long Term Melting Cycles |
| 19 |
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the Melting Evolution of Glaciers |
20 |
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Seasonal Evolution of Melt, Early Spring |
| 21 |
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Seasonal Evolution of Melt, Late Summer |
22 |
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Implications of volume and time spent of water in subglacial system? |
| 23 |
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Meltwater Chemistry |
24 |
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How fast does water flow through the system? |
| 25 |
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How is ice loss assessed? |
26 |
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Can asses ice loss using remote sensing of ice masses |
| 27 |
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Remote Sensing: Instrumentation |
28 |
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Elevation Change: Greenland Ice Sheet |
| 29 |
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Rates of Ice Loss: Greenland Ice Sheet |
30 |
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Melting Extent: Greenland Ice Sheet |
| 31 |
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Remote Sensing Allows For Physical Approximation of Ice Loss |
32 |
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Besides Glaciers and Ice Sheets, There's Also Permafrost |
| 33 |
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How is permafrost impacted? |
34 |
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How is permafrost impacted? |
| 35 |
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Different Types of Permafrost |
36 |
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Polygonal Permafrost: Barrow, AK |
| 37 |
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Melt Evolution of Polygonal Permafrost |
38 |
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Peat Plateaus and Solifluction Lobes: Seward Peninsula, AK |
| 39 |
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Melt Evolution of Intrasedimental Permafrost |
40 |
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Assessing Permafrost Melt: Remote Sensing |
| 41 |
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Assessing Permafrost Melt: Water Chemistry |
42 |
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Degradation of Permafrost Results |
| 43 |
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In Summary |
44 |
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In Summary |