15.2: Assignment- Changes in Extent of Sea Ice at the Poles
- Page ID
- 12947
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\(\newcommand{\avec}{\mathbf a}\) \(\newcommand{\bvec}{\mathbf b}\) \(\newcommand{\cvec}{\mathbf c}\) \(\newcommand{\dvec}{\mathbf d}\) \(\newcommand{\dtil}{\widetilde{\mathbf d}}\) \(\newcommand{\evec}{\mathbf e}\) \(\newcommand{\fvec}{\mathbf f}\) \(\newcommand{\nvec}{\mathbf n}\) \(\newcommand{\pvec}{\mathbf p}\) \(\newcommand{\qvec}{\mathbf q}\) \(\newcommand{\svec}{\mathbf s}\) \(\newcommand{\tvec}{\mathbf t}\) \(\newcommand{\uvec}{\mathbf u}\) \(\newcommand{\vvec}{\mathbf v}\) \(\newcommand{\wvec}{\mathbf w}\) \(\newcommand{\xvec}{\mathbf x}\) \(\newcommand{\yvec}{\mathbf y}\) \(\newcommand{\zvec}{\mathbf z}\) \(\newcommand{\rvec}{\mathbf r}\) \(\newcommand{\mvec}{\mathbf m}\) \(\newcommand{\zerovec}{\mathbf 0}\) \(\newcommand{\onevec}{\mathbf 1}\) \(\newcommand{\real}{\mathbb R}\) \(\newcommand{\twovec}[2]{\left[\begin{array}{r}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\ctwovec}[2]{\left[\begin{array}{c}#1 \\ #2 \end{array}\right]}\) \(\newcommand{\threevec}[3]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\cthreevec}[3]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \end{array}\right]}\) \(\newcommand{\fourvec}[4]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\cfourvec}[4]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \end{array}\right]}\) \(\newcommand{\fivevec}[5]{\left[\begin{array}{r}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\cfivevec}[5]{\left[\begin{array}{c}#1 \\ #2 \\ #3 \\ #4 \\ #5 \\ \end{array}\right]}\) \(\newcommand{\mattwo}[4]{\left[\begin{array}{rr}#1 \amp #2 \\ #3 \amp #4 \\ \end{array}\right]}\) \(\newcommand{\laspan}[1]{\text{Span}\{#1\}}\) \(\newcommand{\bcal}{\cal B}\) \(\newcommand{\ccal}{\cal C}\) \(\newcommand{\scal}{\cal S}\) \(\newcommand{\wcal}{\cal W}\) \(\newcommand{\ecal}{\cal E}\) \(\newcommand{\coords}[2]{\left\{#1\right\}_{#2}}\) \(\newcommand{\gray}[1]{\color{gray}{#1}}\) \(\newcommand{\lgray}[1]{\color{lightgray}{#1}}\) \(\newcommand{\rank}{\operatorname{rank}}\) \(\newcommand{\row}{\text{Row}}\) \(\newcommand{\col}{\text{Col}}\) \(\renewcommand{\row}{\text{Row}}\) \(\newcommand{\nul}{\text{Nul}}\) \(\newcommand{\var}{\text{Var}}\) \(\newcommand{\corr}{\text{corr}}\) \(\newcommand{\len}[1]{\left|#1\right|}\) \(\newcommand{\bbar}{\overline{\bvec}}\) \(\newcommand{\bhat}{\widehat{\bvec}}\) \(\newcommand{\bperp}{\bvec^\perp}\) \(\newcommand{\xhat}{\widehat{\xvec}}\) \(\newcommand{\vhat}{\widehat{\vvec}}\) \(\newcommand{\uhat}{\widehat{\uvec}}\) \(\newcommand{\what}{\widehat{\wvec}}\) \(\newcommand{\Sighat}{\widehat{\Sigma}}\) \(\newcommand{\lt}{<}\) \(\newcommand{\gt}{>}\) \(\newcommand{\amp}{&}\) \(\definecolor{fillinmathshade}{gray}{0.9}\)Module 15 Assignment
Changes in Extent of Sea Ice at the Poles
Overview
With regard to arguments supporting (or not supporting) climate change, climate scientists agree that climate change is happening and that it is indeed exacerbated by human activity. However, there are still a few skeptics and whole organizations outside of the field of climate science that are dedicated to debunking climate change. They might use real data to support their argument, but important data are often omitted or presented in such a way as to paint a very different or skewed picture of the evidence for or against climate change. In this lab activity, you will have an opportunity to explore and compare data presented from different points of view, including data presented in a widely circulated (but unattributed) article entitled “Antarctic Sea Ice for March 2010 Significantly Greater Than 1980,” which was published in April 2010 by a website called “Global Warming Hoax”. Feel free to visit the website and read the article before completing this lab, although it is not required.
How to Draw a Best Fit Line
All of the data provided in this lab originally come from the National Snow and Ice Data Center (NSIDC), housed at the University of Colorado, and can be freely downloaded at nsidc.org. You will be graphing these data and drawing a “best fit line” through the points in order to calculate the slope of line and examine trends in the data. An example of this process is shown below.
![Example of creating a best fit line](https://geo.libretexts.org/@api/deki/files/11379/a15_plot_full.png?revision=1)
Instructions
Part A – Original Data
The two data points on sea ice extent that are included in the Figure 2 were obtained from the article “Antarctic Sea Ice for March 2010 Signicantly Greater Than 1980,” which was published on a website called “Global Warming Hoax.” The data, which is included to the left of the graph below, is the extent of Antarctic sea ice in millions of square kilometers as measured in March of 1980 and 2010. This data is accurate and is consistent with data that can be downloaded from NSIDC. To do this, follow the instructions on how to draw a best-fit line (above). In this case, steps two and three are the same and you can easily calculate slope using the original data.
- Based exclusively on the data provided and the graph, what conclusion would one make regarding climate change? Explain.
- Using the method illustrated in Figure 1, what is slope of the line of best fit for these two data points? Show all your work.
- Even though the above data are accurate, give and explain two reasons why this dataset might lead you to an incorrect conclusion regarding global climate change.
- Reason #1:
- Reason #2:
![template for plotting a best fit line for sea ice extent in the southern hemisphere](https://geo.libretexts.org/@api/deki/files/11435/a16_seaice_full.png?revision=1)
Part B – South Pole Sea Extent
![a15_antartica_full.png](https://geo.libretexts.org/@api/deki/files/11300/a15_antartica_full.png?revision=1)
In part B, you will explore an expanded dataset of Antarctic sea ice extent measured during March 1980 through 2018, downloaded from NSIDC. Only the even-numbered years are presented, but the addition of odd years does not alter the trend in the data. Following the instructions for how to draw a best-fit line (above), graph the data, draw a line of best fit, and calculate the slope of the line.
Year | Ice Extent, million square kilometeres |
---|---|
1980 | 3.29 |
1982 | 4.29 |
1984 | 3.61 |
1986 | 3.7 |
1988 | 3.97 |
1990 | 3.97 |
1992 | 3.57 |
1994 | 4.55 |
1996 | 4.18 |
1998 | 4.11 |
2000 | 4.09 |
2002 | 3.75 |
2004 | 4.53 |
2006 | 3.21 |
2008 | 5.28 |
2010 | 3.85 |
2012 | 4.55 |
2014 | 4.9 |
2016 | 4.07 |
2018 | 3.53 |
![template for plotting a best fir line for sea ice extent in the northern hemisphere](https://geo.libretexts.org/@api/deki/files/11421/a15_seaicesouth_full.png?revision=1)
- What is the slope of the line of best fit you estimated for this data set? Show all your work.
- What do these data tell you about how sea ice extent is changing in the southern hemisphere? How does your result for the extended dataset compare to the results from the data presented from the article presented in Part A?
- What can you say about the data variability, or how wide of a range the data points cover, between the earlier years and the later years on the graph?
- Please offer one suggestion for why the variability in sea ice extent has been changing between 1980 and 2018.
Part C – North Pole Sea Ice Extent
![a15_greenland_full.png](https://geo.libretexts.org/@api/deki/files/11329/a15_greenland_full.png?revision=1)
Next, we will examine the ice-extent patterns of the northern Arctic polar ice sheet that is located on Greenland. The ice-extent data are from March 1980 through 2018 for even-numbered years, also downloaded from NSIDC. Again, here you will graph the data, draw a line of best fit, and calculate the slope of the line.
Year | Ice Extent, million square kilometeres |
---|---|
1980 | 16.04 |
1982 | 16.04 |
1984 | 15.58 |
1986 | 15.91 |
1988 | 15.96 |
1990 | 15.87 |
1992 | 15.48 |
1994 | 15.55 |
1996 | 15.12 |
1998 | 15.6 |
2000 | 15.22 |
2002 | 15.35 |
2004 | 14.99 |
2006 | 14.42 |
2008 | 15.18 |
2010 | 15.14 |
2012 | 15.2 |
2014 | 14.76 |
2016 | 14.4 |
2018 | 14.3 |
![a15_iceextentnorth_full.png](https://geo.libretexts.org/@api/deki/files/11356/a15_iceextentnorth_full.png?revision=1)
- What is the slope of the line of best fit you estimated for this data set? Show all your work.
- What do these data tell you about how sea ice extent is changing in the northern hemisphere? How does your result for the North Pole compare to that of the South Pole (Part B)?
- Explain why you might see a different trend, or slope of the best-fit line, when comparing the sea-ice extent data between the northern and southern hemispheres.
- Module 15 Assignment: Changes in Extent of Sea Ice at the Poles. Authored by: Anne Huth. Provided by: Pima Community College. Located at: http://cc.pima.edu/~lumen/glg101/module%20parts%20-%20LUMEN/Module15/L_Assign15.html. License: CC BY: Attribution
- Physical Geology, Adapted by Anne Huth, Pima Community College. Authored by: Steven Earle. Located at: https://opentextbc.ca/geology/. License: CC BY: Attribution
- Laboratory Manual for Introductory Geology, Adapted by Anne Huth, Pima Community College. Authored by: Bradley Deline, Randa Harris, and Karen Defend. Located at: https://open.umn.edu/opentextbooks/BookDetail.aspx?bookId=506. License: CC BY: Attribution
- Figure 1: Scientists work putting trackers on the ice in the Marginal Ice Zone of Antarctica. Authored by: Katrine Claassens. Provided by: Wikimedia Commons. Located at: https://commons.wikimedia.org/wiki/File:Scientists_work_putting_trackers_on_the_ice_in_the_Marginal_Ice_Zone_of_Antarctica.jpg. License: CC BY-SA: Attribution-ShareAlike
- Figure 2: How to draw a Best Fit Line from Laboratory Manual for Introductory Geology. Authored by: Bradley Deline, Randa Harris, and Karen Defend. Located at: https://open.umn.edu/opentextbooks/BookDetail.aspx?bookId=506. License: CC BY: Attribution
- Figure 3: Sea Ice Extent Southern Hemisphere from Laboratory Manual for Introductory Geology. Authored by: Bradley Deline, Randa Harris, and Karen Defend. Located at: https://open.umn.edu/opentextbooks/BookDetail.aspx?bookId=506. License: CC BY: Attribution
- Figure 5: Sea Ice Extent Southern Hemisphere from Laboratory Manual for introductory Geology. Authored by: Bradley Deline, Randa Harris, and Karen Defend. Located at: https://open.umn.edu/opentextbooks/BookDetail.aspx?bookId=506. License: CC BY: Attribution
- Figure 6: Greenland Ice Sheets. Authored by: Eric Gaba. Provided by: Wikimedia Commons. Located at: https://commons.wikimedia.org/wiki/File:Greenland_ice_sheet_AMSL_thickness_map-en.svg. License: CC BY-SA: Attribution-ShareAlike
- Figure 7: Sea Ice Extent Northern Hemisphere from Laboratory Manual for Introduction Geology. Authored by: Bradley Deline, Randa Harris, and Karen Defend. Located at: https://open.umn.edu/opentextbooks/BookDetail.aspx?bookId=506. License: CC BY: Attribution
- Figure 4: Antartica Ice Shelves. Authored by: USGS. Provided by: Wikimedia Commons. Located at: https://commons.wikimedia.org/wiki/File:Antarctica_ice_shelves.png. License: Public Domain: No Known Copyright