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| Boilerpipe Text | Exponential Smoothing
In this method the next period's forecast is a weighted average of all previous observations that gives progressively less weight to older observations. Forecasts using exponential smoothing are simple to compute; thus, it is a very popular forecasting method that can be made as sensitive as required. This approach is called
exponential smoothing
because the forecast that is generated is made up of an exponentially weighted average of all previous observations. The averaging techniques discussed earlier are known as "smoothing" processes as they attempt to remove the random fluctuations from the time series so that the underlying trend can be seen more clearly and can thus be used for making a forecast that is not subject to random swings. Exponential smoothing was invented by R. G. Brown in the 1950s to make short term forecasts, primarily for the time period following the latest observation. The exponential smoothing formula is given by:
, where
is a smoothing factor, a fraction between 0 and 1.
The weights attached to each observed value in the series of values that make up any
"forecast", F
t+1
form an exponential series with the greatest weight being attached to the most recent observation. The weight for each of the preceding observation decreases exponentially by a fixed fraction (1-
).
The sensitivity of the forecast to changes in the most recently observed data is controlled by the factor
. If
is set to 1 the new forecast (smoothed value) will be equal to the latest observation and there will be no smoothing. The implication in this case is that the new forecast should respond immediately to changes in the actual observation seen in the most recent period. On the other hand, if
is set to 0, then all variations in the actual value from the initial forecast is ignored and the new forecast remains the same as the previous forecast value. This implies that the actual value in the most recent period is purely a random occurrence and hence should be ignored. In practice, however, the value chosen for
is
between 0.1 and 0.3.
In order to initialize exponential smoothing, a forecaster needs two pieces of information--an initial forecast and a value for
. The value of
is left to the judgment of the forecaster. An initial forecast can be obtained using the naïve approach by assuming that it is equal to the actual value from the previous period. We will now go through a simple example of generating forecasts using exponential smoothing. |
| Markdown | 
MANGT 515: Cost and Value Management
[previous](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_10.html) \| [contents](https://courses.worldcampus.psu.edu/welcome/mangt515/toc.html) \| [next](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_12.html)
MANGT 515 Prospective Students
| |
|---|
| [Sample Syllabus](https://courses.worldcampus.psu.edu/welcome/mangt515/index.html "Sample Syllabus") |
| [Sample Lesson](https://courses.worldcampus.psu.edu/welcome/mangt515/toc.html "Sample Lesson") |
| [Introduction](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_01.html) |
| [2\.1 Reasons for Forecasting in Project Management](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_02.html) |
| [2\.2 Forecasting Methods for Projects](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_03.html) |
| [2\.2.1 Qualitative Forecasting Methods](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_04.html) |
| [2\.2.2 Quantitative Forecasting Methods](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_05.html) |
| [Time Series Analysis](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_06.html) |
| [Short Term Forecasting Methods](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_07.html) |
| [Naïve Approach](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_08.html) |
| [Simple Averages](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_09.html) |
| [Moving Averages](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_10.html) |
| [Exponential Smoothing](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_11.html) |
| [Example of Exponential Smoothing](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_12.html) |
| [Trend-Adjusted Exponential Smoothing](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_13.html) |
| [Example of Trend-Adjusted Exponential Smoothing](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_14.html) |
| [2\.3 Intermediate Term Forecasting](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_15.html) |
| [Example of Linear Regression](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_16.html) |
| [Evaluating the "Fit" of the Regression Line](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_17.html) |
| [2\.3.2 The Correlation Coefficient (r)](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_18.html) |
| [2\.3.3. The Standard Error of the Estimate (syx)](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_19.html) |
| [2\.3.4 Limitations in Forecasting Using Linear Regression](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_20.html) |
| [2\.3.4 Limitations in Forecasting Using Linear Regression (continued)](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_21.html) |
| [2\.4 Forecasting the Project End Conditions](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_22.html) |
| [2\.5 S-curve Forecasting](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_23.html) |
| [2\.6 Technological Forecasting\*](https://courses.worldcampus.psu.edu/welcome/mangt515/lesson02_24.html) |
### **Exponential Smoothing**
In this method the next period's forecast is a weighted average of all previous observations that gives progressively less weight to older observations. Forecasts using exponential smoothing are simple to compute; thus, it is a very popular forecasting method that can be made as sensitive as required. This approach is called **exponential smoothing** because the forecast that is generated is made up of an exponentially weighted average of all previous observations. The averaging techniques discussed earlier are known as "smoothing" processes as they attempt to remove the random fluctuations from the time series so that the underlying trend can be seen more clearly and can thus be used for making a forecast that is not subject to random swings. Exponential smoothing was invented by R. G. Brown in the 1950s to make short term forecasts, primarily for the time period following the latest observation. The exponential smoothing formula is given by:
> , where  is a smoothing factor, a fraction between 0 and 1.
The weights attached to each observed value in the series of values that make up any
"forecast", Ft+1 form an exponential series with the greatest weight being attached to the most recent observation. The weight for each of the preceding observation decreases exponentially by a fixed fraction (1-).
The sensitivity of the forecast to changes in the most recently observed data is controlled by the factor . If  is set to 1 the new forecast (smoothed value) will be equal to the latest observation and there will be no smoothing. The implication in this case is that the new forecast should respond immediately to changes in the actual observation seen in the most recent period. On the other hand, if  is set to 0, then all variations in the actual value from the initial forecast is ignored and the new forecast remains the same as the previous forecast value. This implies that the actual value in the most recent period is purely a random occurrence and hence should be ignored. In practice, however, the value chosen for  is between 0.1 and 0.3.
In order to initialize exponential smoothing, a forecaster needs two pieces of information--an initial forecast and a value for . The value of  is left to the judgment of the forecaster. An initial forecast can be obtained using the naïve approach by assuming that it is equal to the actual value from the previous period. We will now go through a simple example of generating forecasts using exponential smoothing.
page 11 of 24
Pennsylvania State University �2007
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| Readable Markdown | ### **Exponential Smoothing**
In this method the next period's forecast is a weighted average of all previous observations that gives progressively less weight to older observations. Forecasts using exponential smoothing are simple to compute; thus, it is a very popular forecasting method that can be made as sensitive as required. This approach is called **exponential smoothing** because the forecast that is generated is made up of an exponentially weighted average of all previous observations. The averaging techniques discussed earlier are known as "smoothing" processes as they attempt to remove the random fluctuations from the time series so that the underlying trend can be seen more clearly and can thus be used for making a forecast that is not subject to random swings. Exponential smoothing was invented by R. G. Brown in the 1950s to make short term forecasts, primarily for the time period following the latest observation. The exponential smoothing formula is given by:
> , where  is a smoothing factor, a fraction between 0 and 1.
The weights attached to each observed value in the series of values that make up any
"forecast", Ft+1 form an exponential series with the greatest weight being attached to the most recent observation. The weight for each of the preceding observation decreases exponentially by a fixed fraction (1-).
The sensitivity of the forecast to changes in the most recently observed data is controlled by the factor . If  is set to 1 the new forecast (smoothed value) will be equal to the latest observation and there will be no smoothing. The implication in this case is that the new forecast should respond immediately to changes in the actual observation seen in the most recent period. On the other hand, if  is set to 0, then all variations in the actual value from the initial forecast is ignored and the new forecast remains the same as the previous forecast value. This implies that the actual value in the most recent period is purely a random occurrence and hence should be ignored. In practice, however, the value chosen for  is between 0.1 and 0.3.
In order to initialize exponential smoothing, a forecaster needs two pieces of information--an initial forecast and a value for . The value of  is left to the judgment of the forecaster. An initial forecast can be obtained using the naïve approach by assuming that it is equal to the actual value from the previous period. We will now go through a simple example of generating forecasts using exponential smoothing. |
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