The environmental impact of the urban drainage in Barcelona is mainly provoked by the combined sewer overflows (CSOs) in the sea and in the rivers. In order to properly analyze the effect of the plan’s measures on the CSO, a standard hydrological year was defined as having more than 50 rainfall events.
3.1. Rainfall Time Series Reanalysis and Storm Design
To date, studies into Barcelona’s rainfall have been calculated using rainfall data from the Fabra Observatory rain gauge station. The time series includes almost 100 years of data, but the location of the observatory in the mountains above the city cannot ensure, a priori, that it is representative of the whole city. Moreover, the temporal resolution of the data is less accurate than the new rain gauges’ time step. Since 1994, the city has developed a management plan to control the sewer system, installing a total of 25 new rain gauges that cover its entire surface. Hence, a long time series of rainfall data is available (approximately 24 years recorded by 25 rainfall graphs achieved by tipping bucket rain gauges), which permits the development of the entire statistical methodology based on real data.
The starting hypothesis is that the existing data do not yet suffer significant CC trends. Subsequently, the influence of the impact of climate change can be considered explicitly after the rainfall analysis, in accordance with the future scenarios obtained in recent studies of the Barcelona City Council and various climate models.
It is possible to directly estimate the empirical exceedance probability of the rainfall data recorded in the rain gauges during the years considered. This method is a good estimation of the maximum rainfall intensity for return periods shorter than the recorded years. For this case, this method was assumed to be valid for return periods of up to 10 years, using 24 years of data. The annual maximum intensity curves for each return period between years 1 and 10 were completed by interpolation of the available data from the empirical intensity–duration–frequency (IDF) table.
For return periods above or equal to the number of available data, an extrapolation must be performed. The maximum annual intensities for the return periods of 20, 25, 30, 50, 75, 100, and 500 years were calculated by extrapolating the parameters according to the Gumbel or extreme type I probability distribution. With the curves corresponding to the 95th percentile for each return period, joint IDF curves for the city of Barcelona were constructed for both the empirical curves and the curves extrapolated by Gumbel.
Figure 2 compares the IDF curves obtained using the Fabra Observatory dataset and the new dataset developed in the PDISBA using the new rain gauges’ data. The plot shows the 10-year return period plots.
As has been stated, the selected intensity of the IDF curves corresponds to the 95% confidence interval of the data. The blue line in the plot shows the maximum observed intensity and the cyan line corresponds to the minimum. The dispersion corresponds to the 25 available rain gauges. It can be observed that, for short durations, the Fabra Observatory IDF curves overestimated the rainfall intensity, but for long durations, they underestimated the precipitation.
Figure 3 shows the IDF curves obtained by the empirical method for return periods equal to or less than 10 years, as well as the IDF curves obtained by extrapolation using the Gumbel distribution. The former exhibits a smoother shape, due to the mathematical extrapolation.
Hyetographs, designed using synthetic rainfall scenarios, were constructed using the alternating block method [
22] and the S-curves method [
23]. Analysis of the temporal pattern of the rainfall was conducted on a selection of the extreme rainfall events recorded in the last 24 years. According to the study of the temporal distribution of the rain, the average duration varied between 160 and 230 min for the different curves. In the alternating blocks hyetographs, the tails corresponding to the difference between 160 and 230 min were analyzed and finally discarded; therefore, a rainfall duration of 160 min was finally selected. The precipitation duration for the previous plans was approximately 60 min [
24].
The second parameter to be established was the intensity peak position in the hyetograph, for which the alternating block method permitted to translate the central intensity peak in order to advance or delay it. The analysis was performed using the S-curves S1, S2, and S3 fitted to the rain gauge data. It was observed that for shorter return periods, the rain showed a centered peak. For rains corresponding to return periods greater than T = 10 years, there was a similar probability of finding the three types of curve (S1, S2, and S3). To conclude which was the most harmful, several model runs were performed using three prototypes of rainfall temporal distribution. For the 10-year return period, it was observed that a delayed peak resulted in higher discharge.
Figure 4 shows the final hyetograph for the selected 10-year return period under the actual conditions. The effect of CC was applied to these values, and the peak intensity was 177.2 mm/h.
3.3. Effects of Climate Change on Extreme and Moderate Rainfall Events in Barcelona
The effects of climate change on the urban hydrological cycle due to a potential increase in extreme rainfall episodes should be considered in order to prevent future problems in urban drainage systems. IDF curves are commonly used to design different types of hydraulic structures in the field of urban drainage. IDF curves could be altered due to a presumed increase in extreme intense rainfall caused by climate change. A general overview about this issue was presented by Willems et al. [
7].
Contrary to what happens in the high-or mid-latitude regions of the world, in which an increase in total precipitation has been reported [
26], several studies have shown a decreasing dominant trend during the last decades in the Mediterranean area. Indeed, the regional climate change assessment report prepared by researchers from the CLIVAR-Spain network [
27] concluded that the annual rainfall in the Iberian Peninsula in the last three decades has decreased significantly compared to the 1960s and 1970s. Despite this decrease in total precipitation, an increase in extreme precipitation has been observed. Simulations for the 21st century typically use climate models to predict significant decreases in total precipitation in the Mediterranean area [
28], although some projections of regional models have shown a possible increase in torrential rainfall [
28,
29], with shorter and more intense precipitation episodes.
According to the V report on climate change of the Intergovernmental Panel on Climate Change (IPCC), known as AR5 in English, in some areas of the world, the frequency, intensity, and/or amount of strong precipitation will increase, but, due to high uncertainty, local detailed studies are required [
28,
30].
The assessment of the potential influence of climate change on the intensity of extreme rainfall is very interesting in the Mediterranean area, especially in densely populated urban areas with complex sewer systems, vulnerable infrastructures, and urban services in the case of extreme rainfall episodes.
In Barcelona, the first evaluation of the possible influence of climate change on extreme precipitation was carried out by Rodríguez et al. [
21]. The authors analyzed future series of daily precipitation for the period of 2000–2099, obtained through five general circulation models under four future special reports on emissions scenarios (SRES) climate scenarios of greenhouse gas emissions (A1B, A2, B1, and B2) and applying the statistical downscaling method for six rainfall stations located in the metropolitan area of Barcelona.
From these series, the future changes to be expected in the IDF curves of Barcelona, for each climatic scenario considered, were calculated. To achieve this, two different time reduction (or downscaling) methods were used. In the first, it was assumed that the relative variations of precipitation between the present and the future are the same for any duration less than 24 h. Meanwhile, for the second, which was based on the scale properties of precipitation, the estimates of these variations depend on the duration.
In particular, in this study, the climate change factors
cf were defined by hourly intensity for different temporal horizons, such as the ratio between the rainfall intensity with a return period
T and for a certain duration
t and the corresponding rainfall intensity for the future with the same
T and t [
31,
32]:
These types of values can be applied directly to the intensities of the design project storm, obtaining a new rainfall hyetograph for future scenarios.
The temporal downscaling technique, based on the fractal properties of rain, was applied up to a duration of 1 h, although climatic change factors were applied to the 5 min intensities as a better approximation available on the date of the study. For the period of 2066–2099, under scenarios A1B, A2, B1, and B2, the climate change factors varied from 1.02 to 1.20 for return periods between 1 and 500 years, those for scenario B2 generally being the greatest [
21].
Representative concentration pathway (RCP) scenarios are the new set of scenarios developed by the IPCC for the Fifth Assessment Report (AR5) [
26,
33]. The pathways describe four possible climate futures based on radiative forcing SRES.
Recently, in the context of the H2020 RESCCUE project (Resilience to Cope with Climate Change in Urban Areas–A Multi-Sectorial Approach Focusing on Water) (
www.resccue.es), new climatic projections concerning several climate variables (temperature, precipitation, sea level rise, heat wave, drought, etc.) were developed for several European cities (Barcelona, Bristol, and Lisbon) [
34].
For the case of Barcelona and the precipitation variable, the historical series of 20 tipping bucket pluviometers of the BCASA rain gauge network with a resolution of 5 min were used, such as the data from the ERA-Interim reanalysis and the of 10 climatic CMIP5 models proposed by the V report of the ICPP [
34]. The projections concerning 20 rainfall time series corresponding to the rainfall gauge stations in Barcelona were achieved through a statistical two-step analogue/regression downscaling method successfully implemented in other recent studies in Spain [
35,
36]. The general atmospheric circulation models were forced by RCPs 4.5 and 8.5, and previously, they were validated for the historical control period of 1976–2005.
The analysis of extreme rainfall episodes on the pluviometric rainfall series (for the period of 2071–2100) of the most representative pluviometer of the BCASA rain gauge network (the Faculty of Physics Station) allowed to achieve new maximum rainfall intensities and new values of climate change coefficients in the range between 1.07 and 1.26, depending on the frequency and duration of each maximum rainfall intensity (
Table 1) [
37,
38]. These values represent the 50th percentile of the results obtained by an ensemble strategy considering all of the outputs provided by the 10 general atmospheric circulation models forced by RCPs 4.5 and 8.5 in order to take into account the uncertainty related to model/run selection and the RCP scenario considered. The new range of climate change coefficients achieved in this study is quite similar to the range achieved by Rodriguez et al. [
21], confirming the same trend of the projections about extreme rainfall events in Barcelona, notwithstanding the use of different general atmospheric circulation models and different climate change scenarios (SRES and RCPs) related to the IV and V reports of ICCP.
The climatic change coefficients obtained for the future time period of 2071–2100 and the return periods of T1, T10, T50, T100, and T500 were applied directly to the project storms proposed in the PDISBA, in order to take into account the effects of climate change on the IDF curves, and consequently, on the drainage capacity of the city and the socioeconomic impacts potentially generated from other services.
The RESCCUE project also provided historical and future rainfall time series to be used as input in the urban drainage and sea water quality models. Ten different climate models were used to provide 5 min downscaled rainfall time series in Barcelona, based on historical (1976–2005) and future (2071–2100) period simulations forced by both RCPs 8.5 and 4.5. The achieved results show that the simulated annual rainfall volume of the historical 1997–2005 period and the number of annual rainfall events were similar to the observed mean values, while the future simulated annual rainfall volumes and annual number of events slightly decreased compared to the historical simulation period.
With these analyses, it can be concluded that the future rainfall scenarios relevant for the analysis of the impacts of CSOs on the sea water quality of Barcelona are unlikely to get worse. Therefore, future continuous rainfall time series with environmental design purposes were considered to be the same as the historical rainfalls [
38]. The available climate change factors were for durations of 5–60 min. In order to be able to apply this transformation to durations above 60 min, the trend was propagated for each of the return periods.
While the available climate change factors did not correspond exactly to the period calculated by the IDF (1994–2018), they were used as a reference to obtain the forecast of the IDF curves, including the influence of climate change. The future rainfall for the return periods of T1, T5, T10, T25, T100, and T500 was also calculated.
Figure 6 shows a comparison between the design rainfall for a 10-year return period calculated with rainfall data up to 2018 and the forecast for the period 2071–2100 according to the climate change coefficients. The blue is the current rain, while red indicates the future increase in rainfall.