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How does mean winter temperature affect length of season for lake ice?  To investigate this question we obtained seasonal ice observation data for a single gauge station (#9004) on Lake Superior.  Data were reported in the form of "first date of observed ice" and "last date of observed ice" -- from these dates we computed the number of days of ice for each year at this station.  We found temperature data from a nearby National Climate Data Center weather station (#205816 in Michigan).  The temperature data is compiled by the United States Historic Climate Network (USHCN) a division of NOAA, but can be downloaded most easily through QELP data set #050.

The scatter in the data suggests that mean winter (December through April) temperature is not a very strong predictor of the length of the ice season.  There is some correlation in the data (we computed a linear regression r value of -.42), but why not more?  What other factors could affect the length of the ice season?  Could the mean December and mean April temperatures be a better predictor?  Is there a different weather station whose temperature data would correlate better with the ice data?  Are there other climate factors (such as wind, clouds, or solar radiation) that also play a part in the duartion of ice?  What information can be gleaned from the outliers on this scatterplot? These are all excellent questions that students might investigate, if only at a rudimentary level.

Variables:

"season"

"mean_temp"

"ice_days"

Link To Google Sheets:

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Columns:

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References/Notes/Attributions:

Ice Data Source:  National Snow and Ice Data Center:  http://www.nsidc.org

https://seattlecentral.edu/qelp/sets/053/053.htm

R Dataset Upload:

Use the following R code to directly access this dataset in R.

d <- read.csv("https://www.key2stats.com/Lake_Superior__Ice_v.csv")

R Coding Interface:


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