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Question 2
The partially completed box plot in Figure 1 shows the distribution of daily mean air temperatures using the data from the large data set for Beijing in 2015. An ou... show full transcript
Step 1
Answer
To identify any outliers based on the provided definition, we first need to calculate the Interquartile Range (IQR). The IQR is calculated as follows:
Given that and (from the data), we find:
Next, we calculate 1.5 times the IQR:
Now, we determine the lower and upper bounds for outliers:
After analyzing the data, the values of temperature below -19.65°C or above 54.35°C can be considered outliers. In the context of the provided data, the significant outlier is the highest temperature, which is 32.5°C. We plot this alongside the calculated quartiles and whiskers to complete the box plot.
Step 2
Answer
The significant outlier temperatures are typically expected during extreme weather conditions. Given the temperatures provided for Beijing and historical weather patterns, we can suggest that the outlier temperatures likely come from the months of October or January, as these are historically colder months in the region.
Step 3
Answer
To find the standard deviation, we use the relationship:
S_x = rac{ au_s}{ au}
where and . The variance can be expressed as:
Calculating this gives:
Now adjusting for standard deviation based on the size of the sample:
S_x ≈ rac{70.4}{ ext{sqrt}(n)} = rac{70.4}{ ext{sqrt}(184)}
Finally, calculating gives us the value close to 5.19°C when rounded to three significant figures.
Step 4
Answer
To calculate the 10th to 90th interpercentile range for , we find the corresponding z-scores for the 10th and 90th percentiles:
Using the z-score formula:
Calculating these values gives:
Thus, the interpercentile range is:
Step 5
Answer
Rainfall: Rainfall data is often skewed with many days receiving no rain at all, leading to a non-normal distribution.
Daily wind speed: Wind speeds can be affected by extreme weather events and are typically not symmetrically distributed, which deviates from the assumption of normality.
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