Wind-speed data from four sites in Denmark have been analyzed in order to o
btain estimates of the basic wind velocity, defined as the 50 yr wind speed
(10 min averages) under standard conditions, i.e., 10 m over a homogeneous
terrain with the roughness length 0.05 m, The sites are Skjern (15 yr), Ke
gnaes (7 yr), Sprogo (20 yr), and Tystofte (16 yr). The measured data are w
ind speed, wind direction, temperature and pressure. The wind records are c
leaned for terrain effects by means of WASP (Mortensew ct al., Technical Re
port I-666 (EN), Riso National Laboratory, 1993. Vol. 2. User's Guide): ass
uming geostrophic balance, all the wind-velocity data are transformed to fr
iction velocity u(*) and direction at standard conditions by means of the g
eostrophic drag law for neutral stratification. The basic wind velocity in
30 degrees sectors are obtained through ranking of the largest values of th
e friction velocity pressure pu(*)(2)/2 taken once every two months. The ma
in conclusion is that the basic wind velocity is significantly larger at th
e west coast of Jutland (25 +/- 1 m/s) than at any of the other sites (22 /- 1 m/s). These results are in agreement with those obtained by Jensen and
Franck (Technical Report, Danish Technical press, 1970) and by Abild (Tech
nical Report R-522 (EN), Riso National Laboratory, 1994). A short discussio
n of the wind storm on the 3rd of December 1999 is included. It is demonstr
ated how the data can be applied to non-standard situations where the rough
ness length depends on the direction. (C) 2000 Elsevier Science Ltd. All ri
ghts reserved.