1 / 47

Organization of this Lab

“Going, going … gone? Analyzing glacier change” Detailed instructions for completing the laboratory. Organization of this Lab. Activity 1: Analyze media stories on the effect of global warming on glacial retreat in terms of glacial processes Activity 2: Develop your hypothesis

doane
Download Presentation

Organization of this Lab

An Image/Link below is provided (as is) to download presentation Download Policy: Content on the Website is provided to you AS IS for your information and personal use and may not be sold / licensed / shared on other websites without getting consent from its author. Content is provided to you AS IS for your information and personal use only. Download presentation by click this link. While downloading, if for some reason you are not able to download a presentation, the publisher may have deleted the file from their server. During download, if you can't get a presentation, the file might be deleted by the publisher.

E N D

Presentation Transcript


  1. “Going, going … gone? Analyzing glacier change”Detailed instructions for completing the laboratory

  2. Organization of this Lab • Activity 1: Analyze media stories on the effect of global warming on glacial retreat in terms of glacial processes • Activity 2: Develop your hypothesis • Activity 3: Test your hypothesis by gathering data on the Nisqually Glacier • Activity 4: Compare Nisqually behavior with other glaciers • Activity 5: Predict future change to glaciers

  3. Activity 1: Analyze media stories on the effect of global warming on glacial retreat in terms of glacial processes • Many videos you can watch on YouTube: http://youtube.com/watch?v=UGclsV3JuAQ http://youtube.com/watch?v=Pem4fpMwkSQ http://youtube.com/watch?v=7MXazI568Bs Just search “glacier retreat” • Media loves the visuals of glacial retreat…

  4. Activity 1: Analyze media stories on the effect of climate change on glacial retreat in terms of glacial processes • You will read media stories

  5. Activity 2: Develop your hypothesis Entire Book, The Scientific Nature of Geomorphology ed. by Rhoads & Thorn SODA

  6. Activity 2: Develop your hypothesis • Read Hecht & Pelto; what are their hypotheses?

  7. Activity 2: Develop your hypothesis

  8. Activity 2: Develop your hypothesis

  9. Activity 3: Test your hypothesis by gathering data on the Nisqually Glacier • Background information on the study area • Methods used to study glacier change… • Task 1. You measure how the length of the Nisqually Glacier changes over time • Task 2. Analyzing uncertainty • Task 3. Plot your data • Task 4. Comparison with atmospheric temperature • Task 5. Comparison with other glacier length records

  10. Activity 3: Background on study area

  11. Activity 3: Background on study area Fly around and two QTVRs

  12. Activity 3: Background on study area Glacier in various positions “above” bridge Bridge marking previous glacier advance

  13. Activity 3: Background on study area

  14. Mt. Rainer through time (courtesy of NPS)

  15. Activity 3: Methods Lots of techniques… field methods mapping terminus historical photos ground photos maps From a Master’s thesis…

  16. Activity 3: Task 1. Measure length of Nisqually Glacier & how changes 1971

  17. Activity 3: Task 1. Measure length of Nisqually Glacier & how changes

  18. Take a string (or ruler). Measure length from the top of Rainier. Then, compare with scale. Then convert km to miles. Activity 3: Task 1. Measure length of Nisqually Glacier & how changes

  19. Ground Photos require that you look for features on the topographic map that can help you identify location of terminus

  20. Working with ground photos can bedifficult and can have low confidence From Mt. Rainer website (photoshopped) Ground photo 1912

  21. Trees…Cliff

  22. Activity 3: Task 2. Analyze Uncertainty

  23. Activity 3: Task 3. Plot your data Already given in data table Need to be graphed

  24. Only connect lines between 4 (high) and 3 (medium confidence) – and leave 2 & 1 unconnected

  25. Example from Glacier X at Mount Rainier

  26. Example from Glacier X at Mount Rainier High confidence ~0.1 km (100 m) range Med. confidence ~0.2-0.3 km (200-300 m) range Low/VL confidence ~0.5-1 km range (guess) Inform reader: where we’re sure of the data and why…here’s our estimate…we need more research…

  27. Activity 3: Task 4. Compare with temperature records

  28. Example from Glacier X at Mount Rainier

  29. Activity 3: Task 4. Example Glacier length increasing… Global temp record shows temp increasing too… Why? Does this make sense? Low confidence for 3 years of data… Note in writing

  30. Activity 3: Task 4. Compare with temperature records—lots of noise & lots of uncertainty Blue dots = avg. annual temp Trend line

  31. Example from Glacier X at Mount Rainier What do the two graphs tell us? Write-up, noting speculative-ness and low/very low confidence levels, but possibilty…

  32. Activity 3: Task 5. Compare with other glacier length records from Oerlemans

  33. Example from Glacier X at Mount Rainier Different is OK…Glaciers have personalities…may not do what “everyone” else does Use fieldwork & maps & other datasets to help us interpret glacier’s personality

  34. Activity 4: Comparing Nisqually to other Glaciers • After scientists conduct research at their study site, most compare results with other locations to discover if their site is an anomaly or reflects a broader trend • Sometimes, scientists do this themselves and make a career studying glaciers • Sometimes, compare with other published studies

  35. Activity 4: Comparing Nisqually to other glaciers

  36. Activity 4: Comparing Nisqually to other glaciers

  37. Activity 4: Comparing Nisqually to other Glaciers

  38. Activity 5: Predict the future (~1850) 10,000 100,000 1,000,000

  39. Activity 5: Predict the future WITHOUT anthropogenic influence…

  40. Activity 5: Predict the future Die-out completely, like Kilimanjaro? Advance in another little ice age?

  41. Activity 5: Predict the future

More Related