This relative frequency histogram shows the distribution of daily rainfall (in centimeters) for a mountainous area over the last 50 days. 20 Complete the table for each rainfall interval with the proportion of days over the 50 days years whose rainfall amount fell in that interval. 18 15 J4
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.
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This relative frequency histogram shows the distribution of daily rainfall (in centimeters) for a mountainous area over the last 50 days.
20
Complete the table for each rainfall interval with the
proportion of days over the 50 days years whose rainfall
amount fell in that interval.
.18
15
14
12
10
Rainfall Interval
Proportion of Days
.08
0G
C to I centimeter
04
.02
2 to 3 pentimetera
1
2
5
9 10
rainfall amount (cm)
3 to 5 centimeters
5 to 7 centinetors
7 to 10 centimeters
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