The complexity of wind loading arises from their variations in space a
nd time. The paper discusses three key spatial functions which control
the magnitude of responses: the influence lines, the mode shapes and
pressure distributions. The last can be efficiently described in terms
of orthonormal expansions. The paper describes how the different time
dependent loadings the mean, the background and resonant responses -
are related to the spatial functions. These tools provide a promising
route for generalization and simplification of wind loading.