Snow and Ice Glaciers Reasons to study glaciers
- Slides: 47
Snow and Ice: Glaciers
Reasons to study glaciers • Because they are there. . … and in the course outline • Impact on river temperature • Water supply for hydro power • Water supply to agriculture • Hazards e. g. outburst floods • The ‘canary’ of climate change • They last longer than snow • Can also be used to milk those who can’t turn on a tap ->
ENSC 454 Snow and Ice: Glaciers Glacier formation Types of Glaciers Distribution of glaciers Glacier movement and change Glacier tour web resources (Not a glacier)
Non-formation of glaciers: Late summer snow patches
Snow must safely survive through the year And not just one year
Mt. St. Helens 2002
What is a glacier ? A glacier is a long-lasting body of ice that is formed on land moves in response to gravity and undergoes internal deformation A glacier is a body of ice, consisting of recrystallized snow, that shows evidence of downslope or outward movement due to the pull of gravity. A general measure of downhill movement is 1 metre per day in summer • How small can a glacier be ? • Minimum. 01 -. 05 sq km ?
How glaciers form • Snowflakes collect or accumulate • More snow falls, compressing it, increasing the density, until after years snow becomes compact and rounded to form firn. • With more snowfalls, the weight compresses the firn into solid ice of a much greater density. • If the ice does not melt and snow continues to fall, the ice mass will increase. Gravity causes the ice mass to move downhill. • As the glacier moves it erodes the landscape on either side and below • Cirque glacier: : / http: //www. fettes. com/Cairngorms/corrie%20 formation. htmp /www. fettes. com/Cairngorms/corrie%20 formation. htm
Snow to ice: Density of snow and ice - kg / m 3 (Patterson, 1994) Pure Ice: 917 Glacier ice: 830 -910 Firn: 400 -830 Fresh snow: 50 -200 http: //www. sciencelearn. org. nz/contexts/icy_ecosystems/sci _media/animations_and_interactives/snow_to_ice_animation
2. Distribution of glaciers
Distribution of Mountain Glaciers on Earth Zuo and Oerlemans (1997)
Kilimanjaro: 1993 and 2000 ice predicted in 2004 to disappear by 2010 (recalculated to 2020) Glacier status depends on: a. (winter) Precipitation b. (summer) Temperature
Glaciers in Canada …. When Ice was King 15, 000 years ago Christopherson (2006)
Antarctica Dry Valley
Distribution of glaciers There is ice on Mars
National Atlas of Canada (online) archives, 5 th edition
http: //atlas. nrcan. gc. ca/site/english/maps/freshwater/distribution/glaciers/1
BC parks with glaciers [Total 83 parks: 7000 sq km- 1987] Number Glaciers Tatshenshini-Alsek Park Ice area (sq. km) Park area (sq. km) % ice 446 3527. 02 9473. 24 37. 23 43 621. 94 2070. 27 30. 04 Huchsduwachsdu Nuyem Jees / Kitlope 318 410. 38 3211. 36 12. 78 Ts'yl-Os (Ts'il? os) Park 212 315. 42 2358. 80 13. 37 86 297. 41 1887. 06 15. 76 128 201. 69 5407. 08 3. 73 Atlin Recreation Area 44 127. 76 403. 89 31. 63 Kakwa Park 56 124. 77 1708. 93 7. 30 Cariboo Mountains Park 66 115. 05 1133. 63 10. 15 Mount Robson Park 61 114. 24 2253. 14 5. 07 Kwadacha Wilderness Park 32 107. 39 1303. 35 8. 24 Mount Edziza Park 15 75. 79 2659. 18 2. 85 Tweedsmuir Park (South) 32 70. 84 5418. 00 1. 31 Northern Rocky Mountains Park 79 70. 64 6663. 83 1. 06 Clendinning Park 34 69. 39 303. 52 22. 86 Tweedsmuir Park (North) 58 53. 48 4460. 96 1. 20 Redfern-Keily Park 24 43. 31 808. 00 5. 36 Gitnadoiks River Park 28 41. 66 577. 44 7. 22 Purcell Wilderness Conservancy Park 27 37. 18 2009. 20 1. 85 Monkman Park 17 35. 38 628. 96 5. 62 Atlin Park Garibaldi Park Wells Gray Park
BC parks with glaciers (. . remaining parks with > 10 sq km glaciers) Park name # Glaciers Ice area (1987) Park area % ice K'ootz//khutze Conservancy 29 34. 73 341. 94 10. 16 Foch-Gilttoyees Park 38 33. 20 612. 16 5. 42 Bishop River Park 18 30. 65 198. 39 15. 45 Hamber Park 20 30. 37 251. 55 12. 07 Bugaboo Park 15 29. 01 138. 17 21. 00 Stein Valley Nlaka'pamux Heritage Park 24 26. 55 1084. 35 2. 45 Fiordland Conservancy 45 23. 89 844. 76 2. 83 2 23. 34 93. 14 25. 06 Lava Forks Park 13 23. 07 73. 88 31. 22 Khutzeymateen Park 14 22. 23 450. 80 4. 93 Smokehouse Creek Conservancy 14 20. 38 379. 02 5. 38 Strathcona Park 50 18. 97 2470. 28 0. 77 Upper Lillooet Park 14 18. 66 199. 96 9. 33 Seven Sisters Park 7 18. 35 271. 40 6. 76 Goat Range Park 22 16. 57 787. 72 2. 10 Height of the Rockies Park 22 10. 94 541. 90 2. 02 Bowron Lakes Park 14 10. 74 1397. 70 0. 77 Tantalus Park 10 10. 70 113. 60 9. 42 Spruce Lake Protected Area 33 10. 32 712. 74 1. 45 Golden Ears Park 18 10. 17 616. 34 1. 65 Great Glacier Park
BC parks with glaciers (3) Glaciers Glacier area Total Area % (1987) Stagoo 8 9. 63 114. 33 8. 42 Gladys Lake Ecological Reserve 8 9. 39 430. 67 2. 18 Upper Seymour River Park 6 8. 91 106. 76 8. 35 Elk Lakes Park 14 8. 40 180. 13 4. 66 Ningunsaw Park 12 8. 25 157. 19 5. 25 Tatlatui Park 12 6. 40 1032. 36 0. 62 Goosegrass Creek Ecological Reserve 1 6. 12 27. 01 22. 67 Small River Caves Park 2 5. 91 18. 10 32. 66 Finlay Russel Park 6 4. 89 1092. 27 0. 45 Spatsizi Plateau Wilderness Park 7 4. 85 7000. 75 0. 07 Swan Lake Kispiox River Park 6 3. 88 623. 03 0. 62 Joffre Lakes Park 3 3. 81 14. 88 25. 60 Pinecone Burke Park 5 3. 78 372. 53 1. 02 Kokanee Glacier Park 3 3. 78 319. 05 1. 19 Woss Lake Park 3 3. 73 65. 27 5. 72 Cummins Lakes Park 5 3. 46 218. 27 1. 59 Crab Lake Conservancy 4 2. 83 127. 99 2. 21 Dune Za Keyih Park 7 2. 78 3317. 30 0. 08 Anhluut'ukwsim Laxmihl Angwinga'Asanskwhl Nisgaa 4 2. 75 178. 80 1. 54 Q'altanaas/Aaltanhash Conservancy 6 2. 56 187. 84 1. 36 Hunwadi/Ainuhhati-Bald Peak Conservancy 4 2. 46 345. 28 0. 71 Big Creek Park 6 2. 08 679. 62 0. 31
BC parks with glaciers (4) Glaciers Glacier area Total Area % (1987) Gingietl Creek Ecological Reserve 3 1. 75 29. 00 6. 05 Bear Glacier Park 1 1. 52 5. 81 26. 12 Mehatl Creek Park 6 1. 11 238. 93 0. 46 Wapiti Lake Park 2 1. 09 168. 37 0. 64 Ptarmigan Creek Park 2 1. 01 33. 06 3. 07 Valhalla Park 2 0. 92 500. 32 0. 18 Upper Raush Protected Area 3 0. 91 55. 80 1. 63 West Twin Park 1 0. 89 223. 20 0. 40 Schoen Lake Park 1 0. 65 87. 79 0. 74 Callaghan Lake Park 2 0. 65 26. 93 2. 40 Blackcomb Glacier Park 2 0. 60 2. 44 24. 38 Denetiah Park 1 0. 59 904. 63 0. 07 Dunn Peak Park 3 0. 41 195. 67 0. 21 Skagit Valley Park 1 0. 39 279. 71 0. 14 Babine Mountains Park 1 0. 38 314. 77 0. 12 Monashee Park 2 0. 38 226. 63 0. 17 Sikanni Chief River Ecological Reserve 1 0. 34 21. 76 1. 54 Strathcona-Westmin Park 1 0. 25 30. 86 0. 81 Birkenhead Lake Park 1 0. 15 97. 77 0. 15 Duffey Lake Park 1 0. 08 20. 97 0. 36 Sustut Park 1 0. 03 756. 87 0. 00
Mountain glaciers in the cryosphere • Small area and volume compared to ice sheets • Total sea level rise equivalent: “only” 0. 5 m • + close to human activities Surface (106 km 2) Volume (106 km 3) Sea level equivalent (m) Antarctica 12. 1 29 68 Greenland 1. 71 2. 95 7. 4 Mountain Glaciers 0. 68 0. 18 0. 5 Sea Ice 16 to 25 Permafrost 22. 7 ? ? Continental Snow 1 to 50 x x 4 km 0 Surface and volume of different components of the cryosphere (IPCC, 2001) 0. 3 km (E. Berthier)
Types of glaciers • • • Ice sheets – Greenland, Antarctica Mountain (Icefields) Valley (Alpine) Piedmont Cirque Hanging Tidewater Niche Glacierets http: //www. solcomhouse. com/icecap. htm
How small can a glacier be ? Minimum. 01 -. 05 sq km ? Niche glaciers
Valley and hanging glaciers
Separated glaciers
Change and movement: Pleistocene maximum ice extent
… somewhere between PG and Vancouver
Nigardsbreen, Norway
Crevasses and surge moraine
Glacier energy and budget: Corrie (cirque) formation
Organisation of a mountain glacier Zones Mass balance accumulation Equilibrium line ablation moraine Longitudinal profile of a mountain glacier Accumulation zone ~ (winter) Precipitation Ablation zone ~ (summer) Temperature (E. Berthier)
Amethyst Lakes, Jasper Nat Park Cirque glaciers will be more common on NE aspects
Tropical glaciers: Venezuela: cirque glaciers >4500 metres ASL
New Guinea, 1936
New Guinea, 1972
Hardanger jokull, Norway Landsat image 1997 snow is in the way!
Hardangerjokull and Finse 3 hours ago
Some Glacier websites http: //ebeltz. net/glaciers. html http: //www. solcomhouse. com/icecap. htm http: //gallery. backcountry. net/papabear_torngats_maps http: //www. pbs. org/wgbh/nova/sciencenow/3210/03 -spac-nf. html http: //www. hi. is/~oi/icelandic_glaciers. htm
Kristie Glacier, near Mc. Bride
Castle Glacier, near Mc. Bride
Castle Glacier
- Rock roll snowman
- Snow teresa jennings
- Few snow or little snow
- Snow and ice cover map
- What is the simple subject of the sentence snow and ice
- Glaciers cause erosion by abrasion and
- Chapter 7 glaciers deserts and wind
- Chapter 8 mass movements wind and glaciers
- Metamorphic rock
- Moraine
- Icing
- Clear ice vs rime ice
- Minnesota glaciers map
- Continetal glaciers
- Glacial drift vs till
- Continental glacier
- Nsidc glaciers
- Bolivia glaciers
- Reasons to study physics
- What is work study in management
- Objectives of work study
- Differentiate between time study and motion study
- Holtmc
- Geometry statements and reasons
- Three g's of spain
- Mathematical proof
- Geometry statements and reasons
- Why did singapore want to merge with malaysia
- Segment and angle proof reasons scavenger hunt
- Angles reasons
- Triangle statements and reasons
- Statements and reasons
- Why does jem openly defy atticus and refuse to leave?
- Snow white different versions
- Once upon a time seven dwarfs
- Good morning snow
- Ashes and snow mexico
- Miles and snow's adaptive strategies
- Cold in the earth
- Mountains and sea
- Low-lying clouds that produce rain and snow
- Case series
- Retrospective cohort study vs prospective cohort study
- Marty lobdell
- Phytogeography region of india
- Do you find zinn’s argument convincing?
- What is your favourite tv show and why
- Reasons for manifest destiny