This study documents significant atmospheric effects over the U.S. central
plains caused by human modification of the landscape. Using observations an
d an atmospheric model, it is shown here that diurnal, thermally induced ci
rculations occur during summer over a 250 x 250 km region in Oklahoma and K
ansas. Furthermore, it is shown that the driving force behind these circula
tions is the landscape heterogeneity resulting from differential land use p
atterns, that such atmospheric phenomena are characteristic of surfaces wit
h this type of heterogeneity and not limited to infrequent days when unusua
l wind or other meteorological conditions prevail, and that the net effect
of these motions is significant, not only locally, but also at the regional
and global scales.