84
. ‘
. . \
--.
- 001
2 1 :
-000
JOOST A. BUSINOER A N D S. P. S. ARYA
- .--I ri
( ug-J 1 / U*
Fio. 6. The longitudinal velocity defect proah for different rtabilities.
earlier by Zilitinkevich (1972) relating the boundary layer thickness to the
stability parameter.
The geostrophic drag relations for the stratified boundary layer are
usually expressed as (see, e.&. Zilitinkevich and Chalikov, 1968; Clarke,
1970)