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Cloudiness in Breslau. In the paper "Cloudiness: Note on a Novel Case of Frequency" (Proceedirgs of the Royal Society of London, Vol. 62. pp. 287-290), K. Pearson examined data on daily degree of cloudiness, on a scale of 0 to 10 , at Breslau (Wroclaw), Poland, during the decade 1876-1885. A frequency distribution of the data is presented in the following table. From the table, we find that the mean degree of cloudiness is 6.83 with a standard deviation of 4.28.

a. Consider simple random samples of 100 days during the decade in question. Approximately what percentage of such samples have a mean degree of cloudiness exceeding 7.5 ?

b. Would it be reasonable to use a normal distribution to obtain the percentage required in part (a) for samples of size 5 ? Explain your answer.

Short Answer

Expert verified

Part (a)P(X¯>7.5)=5.82%

Part (b) No.

Step by step solution

01

Part (a) Step 1: Given information

The frequency distribution of the data is depicted in the table below based on the information provided.

DegreeFrequencyDegreeFrequency
0751621
1179771
21078194
3699117
446102089
59

Given the mean degree of cloudiness is 6.83with a standard deviation of 4.28

That is μx=6.83and σx=4.28

Let Xdenotes the number of degree of cloudiness.

A population variable x has a normal distribution with a mean μ and standard deviation σ The variable x¯ is then normally distributed for samples of size n, with a mean $mu$ and standard deviation σ/n

02

Part (a) Step 2: Concept

The formula used: Standard deviationσx¯=σxn

03

Part (a) Step 3: Calculation

We need to figure out what percentage of 100-day simple random samples have a mean degree of cloudiness greater than 7.5

Sample size n=100

Sampling distribution of the sample mean

μx=μx=6.83

Sampling distribution of the sample standard deviation

σx¯=σxn=4.28100=0.428

We need to figure out what proportion of the sample mean degree of cloudiness is greater than 7.5

That is P(X¯>7.5)

=P(z>1.57)=1-P(Z1.57)=1-0.9418=0.0582=5.82%

04

Part (b) Step 1: Explanation

The sample size is 5; the assumption for addressing this problem is that the degree of cloudiness distribution is not normally distributed, as shown in part (A).

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