Variable Transformations |
This example illustrates how to define a custom transformation by using the Variable Transformation Wizard.
Note: This example is intended for SAS programmers who are comfortable writing DATA step code.
Kimball and Mulekar (2004) analyze the intensification tendency of Atlantic cyclones. This example is based on their analysis and graphics.
In this example, you use the Variable Transformation Wizard to write DATA step code that creates a character variable, Tendency, that encodes whether a storm is strengthening or weakening. The Tendency variable is computed by transforming a numeric variable for wind speed. For each observation of each storm, the Tendency variable has the value "Intensifying" when the wind speed is stronger than it was for the previous observation, "Steady" when the wind speed stays the same, and "Weakening" when the wind speed is less than it was for the previous observation.
Open the Hurricanes data set. |
The wind speed is contained in the wind_kts variable. Note that the values of the wind_kts variable are rounded to the nearest 5 knots. The name of each storm is contained in the name variable.
The data are grouped according to storm name, so an algorithm for creating the Tendency variable is as follows.
For each named storm: Compute the difference between the current wind speed and the previous wind speed by using the DIF function in Base SAS. Specify a value for the tendency variable according to whether the difference in wind speed is less than zero, exactly zero, or greater than zero.
If you were to write a DATA step to create the Tendency variable in a data set, you might write code like the following. The DATA step creates two new variables: a numeric variable called dif_wind_kts and a character variable of length 12 called Tendency. The BY statement is used to loop through the names of cyclones; the NOTSORTED option specifies that the Name variable in the input data set is not sorted in alphabetic order.
data WindTendency; set Hurricanes; by name notsorted; length Tendency $12; dif_wind_kts = dif(wind_kts); if first.name then do; Tendency = "Intensifying"; dif_wind_kts = .; end; else do; if dif_wind_kts < 0 then Tendency = "Weakening"; else if dif_wind_kts > 0 then Tendency = "Intensifying"; else Tendency = "Steady"; end; run;
The Tendency variable is assigned to "Intensifying" for the first observation of each storm because the storm system was weaker six hours earlier. The dif_wind_kts variable is assigned a missing value for the first observation of each storm because the previous wind speed is unknown.
For subsequent storm observations, the dif_wind_kts variable is assigned the results of the DIF function, which computes the difference between the current and previous values of wind_kts.
Submitting this DATA step in the Variable Transformation Wizard is easy. No changes are required.
Select Analysis Variable Transformation from the main menu. |
Select Custom from the Family list on the left side of the page, as shown in Figure 32.21. |
Click Next. |
The wizard displays the page shown in Figure 32.22.
Type the DATA step into the Variable Transformation Wizard, as shown in Figure 32.23. |
Figure 32.23: A Custom Transformation
Click Finish. |
Stat Studio scans the contents of the window and determines that the name and wind_kts variables are needed by the DATA step. The input data set, Hurricanes, is created in the work library. The input data set contains the name and wind_kts variables.
Next, the DATA step executes on the SAS server. The DATA step creates the output data set, WindTendency, which contains the dif_wind_kts and Tendency variables. The dif_wind_kts and Tendency variables are copied from the output data set to the Stat Studio data table.
Scroll the data table to the extreme right to see the newly created variables. |
You can now investigate the relationship between the Tendency variable and other variables of interest.
Create a box plot of latitude versus Tendency. |
The box plot in Figure 32.24 shows the distribution of
latitudes for intensifying, steady, and weakening storms.
Intensifying storms tend to occur at more southerly latitudes, whereas
weakening storms tend to occur at more northerly latitudes.
Figure 32.24: Latitude Stratified by Intensification Tendency
Copyright © 2008 by SAS Institute Inc., Cary, NC, USA. All rights reserved.