414
t . K . WIPI'KRMANN
4 -!
1- -
I
!
I
I
.
. .
~.
.a-.
a
Fic;. 5. The turbulent flux of sensihle heat at the ground as chosen for the input into thc
tirnc-tlcpndent houndary laycr nidel. Comparisons with observations. (After Wipperniann t'r
o/.. lW3,)
tic;. 6. 'The variation of the vertical Km* protile during a ckar day. obtained with it
tinieilependent houndary layer model. (After Wipprmann el a/.. 1973.)
t . K . WIPI'KRMANN
4 -!
1- -
I
!
I
I
.
. .
~.
.a-.
a
Fic;. 5. The turbulent flux of sensihle heat at the ground as chosen for the input into thc
tirnc-tlcpndent houndary laycr nidel. Comparisons with observations. (After Wipperniann t'r
o/.. lW3,)
tic;. 6. 'The variation of the vertical Km* protile during a ckar day. obtained with it
tinieilependent houndary layer model. (After Wipprmann el a/.. 1973.)