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9-60. Cloud seeding has been studied for weather modification procedure (for an intere subject, see the article in Technometr

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Answer #1

a) to support the claim, we need to do 1 sample t testing (one tail test)

Null hypothesis (Ho) : There is no significant difference between the mean rainfall and the average of 30*10^3 m^3

Alternate hypothesis (Ho) : The mean rainfall is greater than the average of 30*10^3 m^3

Running the test, we get the values

One-Sample T: C13

Descriptive Statistics

N Mean StDev SE Mean 99% Lower Bound
for μ
20 32105 5901 1320 28754

μ: mean of C13

Test

Null hypothesis H₀: μ = 30000
Alternative hypothesis H₁: μ > 30000
T-Value P-Value
1.60 0.064

Since p-value is greater than the level of significance (0.01), we fail to reject the null hypothesis and conclude that the mean rainfall is not greater than 30 * 10^3 m^3

b) Checking for normality

Summary Report for Mean rainfall (*10л3) Anderson-Darling Normality Test A-Squared p-Value 0.22 0.820 32.105 5.901 34.823 0.0

The result from Anderson darling normality test shows that the p value is more than the level of significance of 0.05 (for this test only), we conclude that the data is normal. also the histogram shows data follows normality

c) If the true mean rainfall is 33 * 10^3 and the average we need to check for is 30*10^3 m^3

we find the difference of 3000 m^3 to be meaningful

Sample size = 20

Power and Sample Size

1-Sample t Test

Testing mean = null (versus > null)

Calculating power for mean = null + difference

α = 0.01 Assumed standard deviation = 5901

Results

Difference Sample
Size
Power
3000 20 0.415298

The power of the test is 0.41

d) To get the power of 0.9

sample size is

Power and Sample Size

1-Sample t Test

Testing mean = null (versus > null)

Calculating power for mean = null + difference

α = 0.01 Assumed standard deviation = 5901

Results

Difference Sample
Size
Target
Power
Actual Power
3000 54 0.9 0.905446

Sample size should be 54

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