At the Department of Physical Geography, Goteborg University, the Cour's po
llen filter was used to calculate the aerial mass flow and concentration of
marine salts in coastal and inland locations. During this work, it became
apparent that a correction formula for obtaining the how through the filter
was required. This was obtained by acquiring correct concentration values
from the flow through an undisturbed, equally-sized cross section beside th
e filter. Cour (1974) suggests that concentration values should be multipli
ed by a factor of five but also adds that the relation is wind speed depend
ant. Hence, an aerodynamic investigation was performed in a wind tunnel at
five different reference wind speeds. The air flow through the filter was t
hus found to depend on reference wind speed as a 4th grade polynomial. The
airflow through the filter is insignificantly affected by applied contamina
tion of wheat flour or pollen grains to the filter surface up to approximat
ely 500 mg. Above is an increasing risk for reduced flow. The reduction can
be estimated using the results of this work. Applying the correction to ex
isting data showed that the correction effect decreases with increasing ref
erence wind speed. Due to the form of the polynomial, a correction is not r
ecommended outside the approximate interval 2 < u(ref) > 27 m s(-1).