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168 T. Weidinger et al.<br />

2<br />

3 4<br />

1<br />

5<br />

6<br />

7<br />

8<br />

9<br />

3<br />

3.5<br />

3.0<br />

2.5<br />

2.0<br />

< 1<br />

1 - 1.5<br />

1.5 - 2<br />

2 - 2.5<br />

2.5 - 3<br />

3 - 3.5<br />

3.5 - 4<br />

4 - 4.5<br />

4.5 - 5<br />

5 - 5.5<br />

5.5 - 6<br />

> 6 m/s<br />

Fig. 30.1. Annual wind speed in Hungary based on 55 automated meteorological<br />

stations for the period 1997–2003 [4] (left panel); wind map of Hungary based on<br />

wind measurements from 1997 till 2002 [3] (right panel)<br />

Table 30.1. Average wind speed (m s −1 ) for the period 1970–1987, relative deviation<br />

of the maximum and minimum annual mean wind speed from the average<br />

(rel. min and rel. max, respectively) and that for wind energy (proportional to the<br />

cube of wind speed), estimated from monthly wind roses (cub. min and cub. max,<br />

respectively)<br />

Station Average rel. min rel. max cub. min cub. max<br />

Győr 2.70 (m s −1 ) −11.8% 14.3% −40.3% 31.5%<br />

Sopron 4.38 − 8.9 6.7 −21.6 13.1<br />

Szombathely 3.39 −14.1 14.4 −33.9 82.3<br />

Pápa 2.56 −11.1 8.0 −30.6 26.3<br />

Siófok 3.17 −21.0 23.4 −42.8 58.8<br />

Budaörs 2.88 −14.7 16.5 −34.8 58.9<br />

Budapest 2.87 −15.9 19.9 −46.9 72.7<br />

Szeged 3.32 −6.5 9.6 −14.7 23.5<br />

Kékestető 4.40 −23.1 12.8 −55.2 35.5<br />

Relocation of a weather station also causes significant changes. For example<br />

in Sopron (2) 1 the new location of the station is a former wind mill’s location;<br />

here the annual average wind speed increased by more than 1 m s −1 .<br />

The inter-annual variability of annual mean wind speed is an additional<br />

source of uncertainty. In Table 30.1 this uncertainty is demonstrated. The<br />

calculation is based on Annals of the Hungarian Meteorological Service. The<br />

largest values were recorded at the western boundary in Sopron (2) and at the<br />

“top” of Hungary, Kékestető (1,010 m elevation). This inter-annual variability<br />

is the nature of the wind climate. The deviation of the annual mean from<br />

the long term average is around 10%. In the wind tunnel of the Buda hills at<br />

Budaörs (6), this type of deviation is about 15%, at Siófok (5) near Lake Balaton<br />

or at Kékestető (9) this value is above 20%. For the period of 2001–2004<br />

we got even larger deviations. Annual average wind speed for the latter period<br />

1 Numbers in parenthesis after station names refer to their location in Fig. 30.1.<br />

2.0<br />

2.0<br />

2.5<br />

2.5<br />

2.5<br />

2.0<br />

2.5<br />

2.0<br />

2.0<br />

3.0 3.0<br />

2.0<br />

2.5

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