Based on both in-flight measurements and a fluid dynamics model, airflow in
the National Center for Atmospheric Research (NCAR) Community Aerosol Inle
t (CAI) is similar to fully developed pipe flow. Distortions of the velocit
y field were pronounced when suction to inlet tubes was shut off, but condi
tions were otherwise insensitive to all flight parameters but airspeed. The
principal value of the multiuser CAI system for NCAR's C-130 is that it de
celerates air with no curves until the velocity has been reduced to 10 m s(
-1). It then supplies uniformly modified air (after turbulent losses) to al
l users, enabling valid closure experiments.
Chemical data from both the First Aerosol Characterization Experiment (ACE-
1) and the Second Community Aerosol Inlet Evaluation Program (CAINE-II) cle
arly indicate that while passing efficiency for submicron aerosol is accept
able, very little of the sea salt mode mass is transmitted by the CAI to in
struments inside the aircraft. Comparisons between chemical samples from an
external total aerosol sampler and samplers behind the CAI indicate that 7
0%-90% of the sea salt mass is unable to pass the CAI. The 50% cut size is
about 3 mum, but the precise details of the efficiency curve are obscured b
y the difficulty of measuring a reference ambient aerosol distribution. The
loss of particle mass becomes very significant above 3 mum, but the size c
ut is not sharp. These conclusions are supported by calculated particle tra
nsmission efficiencies for the CAI.