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2. semi-arid areas in the eea area

2. Semi-Arid Areas in the EEA Area

A climatic zoning, which is based on the moisture index Ih -, (also known as the UNESCO index), has been established with a view to obtaining insight into the problems associated with water resources in the semi-arid areas of the European Environment Agency (EEA). This index, Ih, is obtained as P/PET, where P is the average annual precipitation, and PET is the potential evapotranspiration according to Penman's formula.

In 1979, UNESCO prepared the World Map of Arid Zones (UNESCO, 1979). Four classes or degrees of aridity were considered, these corresponding to the great geographical categories that are generally accepted. These were:

  • Hyper-arid zones (P/PET < 0.03). Deserts in the strict sense of the term.

  • Arid zones (0.03 £ P/PET < 0.20). Sub-deserts or semi-deserts.

  • Semi-arid zones (0.20 £ P/PET < 0.5). Steppes, prairies, certain types of savannah and a large part of the Mediterranean vegetation. These are zones whose precipitation varies greatly from year to year.

  • Sub-humid zones (0.5 £ P/PET < 0.75). The limits between these zones and the wet and semi-arid zones, are highly changeable and subject to fluctuations.

The precipitation (Figure 2.1-1) and average annual potential evapotranspiration maps (Figure 2.1-2), have been taken from the UNESCO publication entitled "Atlas of World

Water Balance" (UNESCO, 1977).

Figure 2.1-3 shows a map of Europe after the four classifications mentioned above have been applied, and it can be seen that the following EEA regions fall into the semi-arid category: South of Portugal, South East Spain and parts of the central area, South East Italy plus Sardinia and Sicily and South East Greece.

Sections 2.1 and 2.2. are focused on the hydrological characteristics: precipitation, evapotranspiration, and runoff, in semi-arid EEA areas. The information has mainly been taken from the UNESCO publication "Comparative Hydrology" by Falkenmark and Chapman (1989), and has been supplemented with more detailed information concerning the semi-arid regions of Spain and Portugal.

2.1. Precipitation and Evapotranspiration

The average annual precipitation in semi-arid regions is well below the annual potential evapotranspiration (P < 0.5 PET). The values are generally very low, and the completely dry season usually lasts several months.

A basic feature of precipitation is the spatial distribution of storms. The surface area covered by storms in semi-arid zones, especially in the Mediterranean, is often small, and the rainfall decreases sharply within a short distance of the epicentre of the storm. The intensity of the precipitation is another relevant factor in flow generation and also in soil erosion. For instance, at different locations in the Spanish Mediterranean area, over 500 mm have been recorded in one single day.

The maximum theoretical evapotranspiration is determined by the potential evapotranspiration, PET. However, in semi-arid zones, the actual evapotranspiration E is considerably lower than the PET, on account of the lack of water most of the year. As specific potential evapotranspiration conditions are absent, it is difficult to estimate E, because a series of other factors come into play, such as the pattern and magnitude of the precipitation, soil-type and vegetation cover, etc.

The actual evapotranspiration is close to zero in the driest regions of the semi-arid zones, where maximal PET values and negligible rainfall is recorded. The value can be estimated from the water balance. Several different methods can be used for calculating the potential evapotranspiration, including the Penman Monteith method, recommended by the FAO in the "Report on the Expert Consultation on Revision of FAO Methodologies of Crop Water Requirements". (FAO, 1991).

Figure 2.1.-1 - Precipitation map

 

 

Figure 2.1.-2. - Potential evapotranspiration map

 

Figure 2.1.-3 - Moisture index map.

 

2.1.1. Spain

The rainfall distribution is extremely uneven, and an approach to the problem by using average statistical values, could give rise to serious errors. Therefore, although the national average annual precipitation is about 670 mm (equivalent to 340,000*106 m3/year), the average is 1,315 mm, in Northern Spain, and 380 mm in the Segura Basin. The average annual precipitation does not exceed 200 mm in some areas, like Almería in the Sur Basin (MOPTMA, 1993). There is also a marked annual unevenness in each basin, which brings water shortages and drought after several consecutive dry years.

The national mean annual PET is about 800 mm and the actual evapotranspiration 445 mm/year, which amounts to approximately 226,000*106 m3/year.

The Segura Basin is the area whose mean annual precipitation is considerably lower than it is in the rest of the semi-arid areas in Spain. This area must face the problems related to water availability for irrigation year after year. Water supply problems also appear during dry seasons in most of the areas of the Guadiana, Guadalquivir and Sur Basins. Those basins register an annual mean precipitation lower than the national average.

Table 2.1- 1 shows the basins considered, in global terms, as semi-arid regions in Spain (Estrela, T. 1995). A region has been considered as a semi-arid one when a high percentage of its surface area complies with the UNESCO moisture index criterion for semi-arid areas (P/PET £ 0.5).

 

2.1.2. Portugal

The mean annual precipitation (P) in Portugal is 889 mm (OECD, 93). There is an imbalance between the northern and southern basins: whilst P=1,800 mm or even more (2,373 mm/year in Cavado basin) in the north; while in the south, the Sado and Mira Basins have P values around 700 mm or even less in the Guadiana Basin.

In Portugal, there are 5 regions with semi-arid or scarcity issues (INAG, 1995b), as Table 2.1-1 shows. Region 1 is the part of the Douro catchment with Mediterranean climate (located in the North). Regions 3 and 4 are the must problematic zones in terms of scarcity, both in surface and groundwater. In these regions there are problems of domestic water supply. The figures corresponding to P/PET are slightly greater or equal to 0.5 in the Alto Douro (01), Soul Tejo (02) and Sado e Mira (03) , yet they are less than 0.5 in the Guadiana basin and in the Algarve region. Although in the Guadiana basin the PET is equal to 1,304 mm/year, the precipitation is the lowest in the Portuguese catchment areas. In Algarve, the mean annual precipitation is equal to 653 mm, but the PET is the highest (equal to 1689 mm/year).

The PET figures quoted here seem to have been estimated in a different way from those in Spain.

 

2.1.3. Italy

The mean annual precipitation in Italy is P=982 mm (OECD 93). The island of Sardinia (24,000 km2) in Italy has a climate characterised by a water deficit at most altitudes. The mean annual precipitation is 752.8 mm and the mean annual potential evapotranspiration is roughly 1,500 mm (Environment Department, 1995)

 

2.1.4. Greece

Greece is divided into fourteen hydrologic departments. Two of them, Attiki and the Aegean Islands, are areas with water scarcity problems, due to the unfavourable hydrogeology and the low precipitation. The high population density in Attiki is another particularly remarkable factor (almost 35% of the total population in Greece is concentrated in Athens). There are also water scarcity problems in East Peloponnisos and in some particular areas of Central Macedonia, as Table 2.1-1 shows. The Aegean Islands region is the driest in Greece, having a mean annual precipitation of 500 mm and the potential evapotranspiration is equal to 1250 mm/year.

 

Table 2.1. -1 Semi-arid regions in the EEA area.

Country

Region name

Region number

P (mm/year)

PET (mm/year)

P/PET

Greece

Aegean Islands

Attiki

North Peloponnisos

East Peloponnisos

Central Macedonia

Kriti

14

06

02

03

10

13

500

900

800

600

600

900

1250

1250

1250

1250

1250

1250

0.40

0.72

0.64

0.48

0.48

0.72

Portugal(*)

Alto Douro (18,710a )

Sul Tejo (24,860 b)

Guadiana (11,700)

Sado e Mira (9,236)

Algarve (4,048)

01

02

03

04

05

683

687

564

659

653

1293

1381

1304

1327

1689

0.53

0.50

0.43

0.50

0.39

Italy (+*)

Sardinia (24,000)

753

1500

0.50

Spain (*)

Guadiana (60,000)

Guadalquivir (63,500)

Sur (18,000)

Segura (18.800)

Jucar (42,200)

04

05

06

07

08

557

617

539

381

520

933

951

985

912

802

0.60

0.65

0.55

0.42

0.65

Notes:

P (mm/year) is the mean annual precipitation.
PET (mm/year) is the mean annual evapotranspiration.
(*) Figures in brackets state the catchment surface (km2)
(+) Only information from Sardinia.
(a) Total surface area of Portuguese Douro basin.
(b) Total surface area of Portuguese Tejo basin.

The value of mean annual potential evapotranspiration in Spanish semi-arid areas is PET= 950 mm/year on average, whilst, those are greater than or equal to 1500 mm/year in Portugal (Algarve), Greece and Sardinia. However, Figure 2.1-4 shows a comparison of the values of the registered evapotranspiration, which are similar in the semi-arid countries. Studies at a European scale would be necessary in order to establish commonalities between the semi-arid regions in the EEA area.

 

fig214.gif (16208 bytes)

Figure 2.1.-4 Precipitation and evapotranspiration in semi-arid countries.


2.2. Runoff

The discharge hydrograph is closely related to the temporal precipitation distribution. The precipitation characteristics mentioned in Section 2.1 make flash floods be a common feature in semi-arid zones.

Droughts are a consequence of the variability in river runoff from year to year. Although they tend to affect large parts of Europe at the same time, they are particularly damaging in semi-arid areas, like the one which has affected southern Spain during these last years.

Aquifer recharge in semi-arid zones is lower than in wet areas, not only because the precipitation is lower, but also as a result of the uneven temporal distribution of this precipitation. During most of the year, the soil is not saturated, and this makes aquifer recharge difficult not only in summer months, but sometimes even in winter. The use of groundwater, either in conjunction with surface water or independently, is of vital importance in these zones when attempting to alleviate the effects of drought.

Part of the water that recharges the aquifers eventually reaches the surface drainage network, and is one of the basic constituents of the total yield. It is of paramount importance to have in-depth knowledge of the processes and laws of exchange which govern the river-aquifer relationship in such zones. An awareness of this information would serve to evaluate, for example, the effects of aquifer extraction on the discharges of the rivers.

 

2.2.1. Spain

The total average annual yield (surface water and groundwater) is 114,000*106 m3, which amounts to specific runoff figures of 230 mm/year. The European average is approximately 300 mm/year. However, only a small amount of the natural resources are directly useable, roughly 9,200*106 m3 per year, which is a mere 8 % of the total on the Spanish peninsular. This figure contrasts sharply with the European average, where the percentage is 40% of the natural resource (MOPTMA, 1993).

From a comparative viewpoint, this situation is even less satisfactory when the uneven space/time distribution is taken into account. The basins in Galicia and in the North, which have a surface area of 53,800 km2 (10.6 % of the national territory), provide an average annual figure of 42,000*106 m3 (36.3 % of the national average). Two basins in the South, the Segura and the Júcar, with a total surface area of 79,830 km2 (15.8 %) yield an annual average of 7,600*106 m3 (6.6 % of the total). That is to say, there is an 8:1 relationship in the yields per unit of surface area.

 

2.2.2. Portugal

The total surface of the Portuguese catchment areas is 89,300 km2 . Five rivers are transboundary and the total surface of the shared basins between Spain and Portugal is 268,529 km2. The total specific runoff (Spain and Portugal) is 295 mm/year, and the figures for Portugal are 313 mm/year and 287 mm/year for the runoff coming from Spain. (LNEC, 1992).

There is also an imbalance between the northern and the southern basins. The Minho catchment area is 17,081 km2 (5% of the surface is Portuguese) and its average total runoff is 750 mm/year; whilst in the Guadiana basin (71,573 km2 , 16.3% of this surface is Portuguese) the total runoff is only 90 mm/year (188 mm/year yield in Portugal), (LNEC, 1992).

 

2.2.3. Italy and Greece

The average specific runoff in Italy is 554 mm/year, which is a much higher figure than the European average, and it represents a total quantity of internal resources of 167,000 *106 m3 (OECD 1993). Despite these figures, Sardinia and Sicily are stated as semi-arid regions, which demonstrate once more the imbalance between basins in Italy.

The internal resources of Greece are 45,000*106 m3 (OECD,1992), which are equivalent to an average runoff of 341 mm/year. The areas having scarcity problems are located mainly in the southern regions of the country.

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