Using the climate data below create a line graph for temperature and a bar graph for precipitation by month for each location. If you don’t have access to graph paper, you may use an online tool such as Physics Aviary Graphing, Google Sheets or Desmos. Copy and paste your graph into each graph box. Average Precipitation for Trondheim, Norway (inches) Jan Feb Mar Apr May Jun Jul Aug Sep Oct Nov Dec 2.1 1.6 2.8 2.0 1.8 2.7 3.0 3.5 3.5 2.5 3.0 5.5
Inverse Normal Distribution
The method used for finding the corresponding z-critical value in a normal distribution using the known probability is said to be an inverse normal distribution. The inverse normal distribution is a continuous probability distribution with a family of two parameters.
Mean, Median, Mode
It is a descriptive summary of a data set. It can be defined by using some of the measures. The central tendencies do not provide information regarding individual data from the dataset. However, they give a summary of the data set. The central tendency or measure of central tendency is a central or typical value for a probability distribution.
Z-Scores
A z-score is a unit of measurement used in statistics to describe the position of a raw score in terms of its distance from the mean, measured with reference to standard deviation from the mean. Z-scores are useful in statistics because they allow comparison between two scores that belong to different normal distributions.
Graph Construction
Using the climate data below create a line graph for temperature and a bar graph for precipitation by month for each location.
If you don’t have access to graph paper, you may use an online tool such as Physics Aviary Graphing, Google Sheets or Desmos. Copy and paste your graph into each graph box.
Average Precipitation for Trondheim, Norway (inches)
|
Jan |
Feb |
Mar |
Apr |
May |
Jun |
Jul |
Aug |
Sep |
Oct |
Nov |
Dec |
|
2.1 |
1.6 |
2.8 |
2.0 |
1.8 |
2.7 |
3.0 |
3.5 |
3.5 |
2.5 |
3.0 |
5.5 |
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