Aerosol Observing System (AOS) Purge: initiated flow reversal for aerosol stack dependent on CO level (b0-level)
Aerosol Observing System (AOS) Purge: initiated flow reversal for aerosol stack dependent on CO level
Engineering topics
Publications and source records attributed to Ermold, Brian.
Aerosol Observing System (AOS) Purge: initiated flow reversal for aerosol stack dependent on CO level
Ceilometer (CEIL): cloud-base heights and polarimetric variables
AOS: Single Particle Soot Photometer, extended range
Auxiliary data for the AOS Single Particle Soot Photometer, extended range
AOS: Single Particle Soot Photometer, extended range, particle-by-particle
MAGIC 250 Water-Based Condensation Particle Counter
MAGIC 250 Water-Based Condensation Particle Counter
ARM Aerial Facility (AAF) Fiber Optic Temperature Sensor
The condensation particle counter (CPC) measures sub-micron aerosol particle number concentration by condensing fluid onto particles and causing them to grow to sizes that are easily detectable by optical scattering. The condensing liquid is typically an alcohol (e.g., butanol) or water. Depending on the CPC type, typical CPC instruments can count particles with sizes that range from 3 to 3000 nanometers (ultrafine CPC) or from 10 to 3000 nanometers (fine CPC).
The micropulse lidar (MPL) is a ground-based, optical, remote-sensing system designed primarily to determine the altitude of clouds; however, it is also used for detection of atmospheric aerosols. The physical principle is the same as for radar. Pulses of energy are transmitted into the atmosphere; the energy scattered back to the transceiver is collected and measured as a time-resolved signal, thereby detecting clouds and aerosols in real time. From the time delay between each outgoing pulse and the backscattered signal, the distance to the scatterer is inferred. Post-processing of the lidar return characterizes the extent and properties of aerosols or other particles in a region.