Regarding civil engineering, the knowledge and understanding of climate change is important because, if there are changes in the variables related to hydrological systems, it could imply changes in design criteria, as these are frequently based upon the assumption of the hydrological series stationary. Not doing so, could mean the under or over design of hydraulic infrastructures, thus creating performance deficiencies or over expensive solutions.

The IDF (Intensity Duration Frequency) relationship constitutes an objective tool to quantify precipitation uncertainty, especially in circumstances when a design rainfall event must be determined for a particular water resources project. To perform the analysis, long-term precipitation data from a recording rain gage must be available. The prediction of uncertain environmental variables is often a hydrologic problem of significance in water resources management and water resources design projects. The Gumbel distribution, named after one of the pioneer scientists in practical applications of the Extreme Value Theory (EVT), the German mathematician Emil Gumbel (1891-1966), has been extensively used in various fields including hydrology for modeling extreme events [1] -[3] . Gumbel applied EVT on real world problems in engineering and in meteorological phenomena such as annual flood flows [4] .

Figure 1 shows that the temperature increases significantly since 1980. The objective of this present work is to study the impact of this increase on the intensity of the rainfall at Toronto for several return periods and durations.

The Gumbel distribution is very suitable for modeling extreme event [5] [6] . The cumulative distribution function (CDF) is given by Equation (1):

where X is a random variable. In our case, X is the rainfall intensity or the rainfall depth for a given duration.

The Gumbel variable is defined by Equation (2)

The parameters a and b are defined by:

where σ is the standard deviation and μ is the mean of the variable.

The empirical distribution of Hazen is used:

where i is the rank of a given data and n is the total number of data.

The rainfall data of Toronto (Canada) has been used for computing the IDF curves before and after 1980.

The rainfall data are from 1940 to 2007. The rainfall station is located at latitude 43.67˚N and longitude 79.4˚W. Its elevation is 112 m. The duration of rainfall are 5 min, 10 min, 15 min, 30 min, 1 h, 2 h, 6 h, 12 h and 24 h. Equation (2) shows that if the Gumbel distribution is valid, it has to a linear relationship between the empirical intensity x and the Gumbel variable u.

Starting from Equation (4), the Gumbel variable is computed by:

where ln is the natural logarithm, i is the rank of a given data and n is the total number of data.

Figure 2 shows the experimental rainfall depth versus the Gumble variable. The fit of the data by the Gumbel distribution is suitable.

The IDF curves

The IDF curves are computed for five return periods T (2, 5, 10, 20 and 50 years). For these return periods, the probability associated with the not exceedance is computed by:

The Gumbel variable are computed by:

Table 1 gives the results of Equations (6) and (7).

For each rainfall duration, there are a specific standard deviation σ and a specific mean μ. Therefore, there are a specific parameters a and b defined by Equation (3).

Table 2 and Table 3 give the different values of these parameters.

Equation (2) enable to compute the rainfall depth x for the different durations and return periods. Finally, the rainfall intensity is calculated by dividing the rainfall depth by the duration. Table 4 and Table 5 give the computed intensity before and after 1980 and Figures 3-7 shows the IDF curves.

Examination of Table 4 and Table 5, and Figures 3-7, it appears that the impact of global warming on the IDF curves is not very clear, however, their analysis enables to note that the rainfall intensities after 1980 are lower than those from before this date.

This is especially clear for those of short duration. Their intensity decreased, particularly for the return period of 5, 10, 20 and 50 years.

Examination of Table 4 and Table 5, and Figures 3-7, it appears that the rainfall intensities after 1980 are lower than those from before this date. This is especially clear for those of short duration.

Fallot and Hertig [7] carried out Gumbel analysis of rainfall depth at 429 locations in Switzerland. They computed rainfall depth for a return period of 500 years and concluded that rainfall depth obtained for the period 1961 to 2010 are overall higher than 15% than estimated from the rainfall series from 1901 to 1970 for all stations in Switzerland. Vaz [8] studied annual maximum daily rainfall series from 23 rain gages in Portugal.

The research carried out showed that the samples of intensive rainfalls do not exhibit trends, as to affirm or contradict the effects often attributed to the climate change phenomenon (i.e. heavier rainfalls with smaller duration). The study found out that all kinds of behaviors can occur: some samples denote the trends often considered as resulting from the climate change, while exhibit the exact opposite, not allowing the identification of any of the consequences attributed to such phenomenon.

Comparing our results with those of other authors, it appears that, for the moment, no general law on the impact of global warming on the intensity duration frequency relationships can be made. It appears that the impact of global warming on rainfall varies with geographic location and that it is not possible to draw some general conclusions across the planet

ErickCarlier,Jamal ElKhattabi, (2016) Impact of Global Warming on Intensity-Duration-Frequency (IDF) Relationship of Precipitation: A Case Study of Toronto, Canada. Open Journal of Modern Hydrology,06,1-7. doi: 10.4236/ojmh.2016.61001