It is well known that turbulent transfer models can sometimes produce
results that cannot be realised in nature. In this paper we develop si
mple rules to check the physical robustness of parameterisations of la
nd-surface turbulent transfer for heterogeneous surfaces. The methodol
ogy draws upon areal-averaging by parameter aggregation and by flux ag
gregation. Both techniques have been demonstrated to be valid. Combini
ng the two techniques enables one to determine the surface potential t
emperature and specific humidity, averaged over the grid-box. When thi
s is done the implied turbulent transfer is sometimes counter-gradient
. The implications of this result are discussed. The methodology prese
nted is general and provides a complementary way of evaluating the rol
e of coupling land-surface schemes to atmospheric host models to that
presented by Polcher et al. [Polcher, J., McAvaney, B., Gaertner, M.-A
., Hahmann, A., Noilhan, J., Phillips, T., Pitman, A., Schlosser, A.,
Schulz, J.-P., Timbal, B., Verseghy, D., Viterbo, P., Xue, Y., 1998. A
proposal for a general interface between land-surface schemes and gen
eral circulation models. Global Planet. Change, this issue.]. (C) 1998
Elsevier Science B.V. All rights reserved.