Greater understanding of the details of the how fields around bluff bodies
and the separated regions associated with these hows is necessary to advanc
e the knowledge of fluid-structure interactions. These mechanisms are parti
cularly important in wind engineering in determining design pressures on st
ructures. In almost all instances the maximum design pressure occurs in reg
ions of separated flow. The details of the how in these separated regions a
nd the criteria for physical or numerical modeling of the flows in these re
gions are not well understood. Measurements have been conducted using a las
er Doppler velocimeter (LDV) to examine the structure of separated shear la
yers and the associated regions of separated flow. a LDV is an important to
ol for this application. A LDV system is capable of measuring reversing flo
ws and consequently high local turbulent intensities. Thermal anemometry do
es not allow measurements under these conditions. When making measurements
with a LDV in air, it is necessary to seed the how with particles. Seeding
is a challenge in applying these measurement techniques to flows in boundar
y-layer wind tunnels. Efforts to understand the basic mechanisms affecting
pressure fluctuations and associated extreme pressures on a bluff body will
be advanced by the ability to measure the flow in separated shear layers a
nd within separated regions associated with these shear layers. The use of
a LDV system provides an additional tool to explore this complex region. (C
) 1998 Elsevier Science Ltd. All rights reserved.