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An extension of the equations 2 is proposed in this study by analyzing the
inclusion of the population pressure (for residents and tourist) as an additional exogenous
determinant. This variable can be easily obtained in isolated territories where a higher
level of forecasting accuracy is specially appreciated. Thus, analytically, equation 1 can
be extended, to:
lnCt= pt+st+CSDt+CWEAt+Pt+ut (3)
where Pt denotes the population pressure. In a similar way equation 2 can be
rewritten as
tttt
εuqθXb
Cp
)(')(ln)( (4)
where X' includes the variables p, s, CSD, CWEA and Pt.
3. Data and forecasting evaluation strategy
3.1. Data
The dataset used in this study concerns daily time series for electricity consumption for
Majorca, Minorca and Pitiüses (Ibiza and Formentera). The Balearics are considered
jointly from January 1995 until September 2007. This is 4655 daily observations for each
one of the four utility systems considered. The dataset was compiled by the Spanish
System Operator Red Electrica de España and no missing observations were present.
Charts of the time series. in Figure 1. show a clear trend along the whole sample, and
depict different seasonal cycles. In this case, it should be highlighted that for many
coastal areas in the Mediterranean Sea, high season is characterized with high
temperatures and an important presence of tourists. Therefore, it is important to be aware
that the seasonal movement of electricity load is not originated exclusively by weather
pattern but also from differences in the population that is on the islands during the year.
Meteorological variables were provided by the Instituto Nacional de
Meteorologia, the Spanish official meteorological bureau, and are referred to the airport
stations. From the experience of previous literature, the weather-related factors that can
influence the electricity demand are temperature, humidity, wind and precipitation in
decreasing order of importance [9]. However, the non-linear influence of temperature on
the electricity demand suggests the use of two temperature derived functions: heating
degree-days (HDD) and cooling degree-days (CDD)[30]. When dealing with the non-
linearity of the temperature effect, the most frequent approach is to segment temperature
into HDD and CDD, defined as shown below:
HDDt = Max (Tref - Tt, 0) (5)
CDDt = Max (Tt-Tref, 0) (6)
M.BakhatandJ.RosselloNadal / ImprovingDailyElectricityLoadsForecasting 69
Intelligent Environments 2019
Workshop Proceedings of the 15th International Conference on Intelligent Environments
- Title
- Intelligent Environments 2019
- Subtitle
- Workshop Proceedings of the 15th International Conference on Intelligent Environments
- Authors
- Andrés Muñoz
- Sofia Ouhbi
- Wolfgang Minker
- Loubna Echabbi
- Miguel Navarro-Cía
- Publisher
- IOS Press BV
- Date
- 2019
- Language
- German
- License
- CC BY-NC 4.0
- ISBN
- 978-1-61499-983-6
- Size
- 16.0 x 24.0 cm
- Pages
- 416
- Category
- Tagungsbände