During precipitation events usually a high proportion of the altitude
column will show a high total reflectivity DBZH
(which includes biology +
meteorology), because precipitation usually falls from several kilometers high
to the ground surface. Precipitation events are often obvious in profile plots
of quantity DBZH
as reflectivity signals extending from ground level to high
altitudes far above the typical altitudes where biology is expected. This filter
identifies and removes these cases.
The posthoc precipitation filter examines the total reflectivity factor DBZH
and calculates the altitude range at which DBZH
is larger than parameter
dbz
. Whenever this altitude range is larger than parameter range
(and drop
is FALSE
), the biology is removed by setting profile quantities dens
and eta
to zero and profile quantity dbz
to -Inf
. When parameter drop
is TRUE
, the profile is removed from the time series altogether.
This posthoc precipitation filter is likely to remove biological scatterers
that co-occur with precipitation, for example biological movements during isolated
convective thunderstorms. It is more aggressive than precipitation filters
applied during vertical profile generation with calculate_vp()
that attempt to
remove precipitation and retain biology. The posthoc precipitation filter is especially
useful for analyses where you want to minimize the risk of precipitation contamination,
at the cost of filtering out some biology during precipitation events.
Lowering the default minimum reflectivity (dbz
) for precipitation
below 7 dBZ is not recommended, as most precipitation has a reflectivity above 7 dBZ.
Parameter range
should be chosen carefully, and should be higher than the
typical altitude where biological scatterers still reach a reflectivity factor equal to dbz
.
Note that at S-band wavelengths bird migration occurs much more frequently in the reflectivity
regime for precipitation than at C-band. Therefore, at C-band lower settings for parameter dbz
are appropriate than at S-band.